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Sample records for 137cs iz organizma

  1. 137Cs metabolism during pregnancy

    Data from two pregnant women contaminated with 137 Cs, body burdens of 0.2 and 300 MBq, respectively, at the time of the Goiania accident, were compared. The first one, with lower 137 Cs body burden was exposed during the fourth month of pregnancy, while the second became pregnant three years and eight months after 137 Cs intake. For the first woman 137 Cs concentrations were similar for the mother, infant and placenta, indicating an easy and homogeneous transport of 137 Cs from mother to fetus. The whole-body monitoring data from the second woman, who became pregnant four years after intake, did not show a reduction in biological half-life during the pregnancy. Cs concentration in the mother was found to be 13 times higher than in the infant. One possible reason for this result is that four after intake. Cs is supposed to be concentrated mainly in skeletal muscle tissue. During the pregnancy the blood flux becomes higher in most of organs and tissues except brain, liver and skeletal muscle tissue. In this case, the physiological changes due to pregnancy did not modify the cesium retention. (author)

  2. 137Cs in freshwater fish in Finland

    The paper deals with an evaluation of the importance of Finnish freshwater fish as a source of 137Cs in the diet. Freshwater fish were analysed for 137Cs in 1982. The 137Cs concentration factors from water to edible fish were determined for the same year. The evaluation is based on an extensive surface water investigation performed from 1965 to 1967. Along with the continuous fallout monitoring since the beginning of the 1960'es, this material makes it possible to valuate the 137Cs levels in surface water right up to the 1980'es. In 1982 the Finns received an average of 90 Bq 137Cs from freshwater fish. This dose constitutes a quarter of the 137Cs uptake from the total food consumtion in Finland in 1982

  3. 137Cs in northern Adriatic sediments

    The activity of 137Cs in shallow northern Adriatic sediments was obtained on the basis of measurement results from 25 sediment box cores, sampled during the Adriatic Scientific COoperation Program (ASCOP) 16 cruise in the summer 1990. 137Cs was determined in surface sediments (0-3 cm) and 12-15 cm-deep sediment. It was found that the lowest caesium concentrations correspond to sands, which are spread along the Croatian coast. Parallel to the Italian coast, 137Cs concentrations in pelites are the highest. It seems that the influence of Po River is significant for 137Cs activities in recent marine sediments along Italian coast south of Po River delta. Significantly higher 137Cs activities in 0-3 cm sediment layer can be attributed to the deposition caused by Chernobyl accident. (author)

  4. Desorption of 137Cs+ from mosses

    OLGICA NEDIC

    2002-09-01

    Full Text Available Mosses are biomonitors that accumulate large amounts of various pollutants, including radionuclides. In this work we investigated the possibility of 137Cs extraction from mosses, as well as the significance of species specificity on the efficiency of 137Cs desorption. Salt and acid solutions were used as extraction media. It was shown that a 5 % solution of both ammonium oxalate and phosphoric acid was able to desorb 81.8 % of 137Cs+ from Homalothecium sericeum, which was 39.9 % more than desorption from water. At the same time, most of the desorbed 137Cs+ was incorporated in crystals that precipitated from the solution. An interspecies difference in respect to 137Cs+ desorption was noticed.

  5. Biokinetic model for 137 Cs

    The main objective of this work was to provide a realistic biokinetic model for 137 Cs metabolism. This model was based on the retention of cesium in 57 people contaminated in the Goiania accident, ages 1 to 73 y old, complemented by data obtained in an experiment with beagle dogs, and data taken from the open literature. Cesium is distributed among all tissues and organs of the body. Its main retention site is the skeletal muscle tissue. Mathematically, cesium retention in the body may be described by a sum of three terms exponential equation. The first term represents the fraction which is rapidly eliminated in urine. This fraction is weight dependent (negative correlation). The second term represents the retention of cesium in tissues and organs of the body. For children and adolescents, the second term biological half-life is a function of the weight. For adults, it is correlated with sex. Men present a higher retention of cesium than women. The third term correspond to a retention fraction of the order of 0,1% of the initial body burden. It is characterized by a very long half-life and represents a subcellular retention of cesium in the skeletal muscle tissue. During pregnancy the transfer factor from the mother to the fetus is correlated to the amount of cesium in the blood and it is equal to 1, if the intake of cesium occurs pregnancy. (author)

  6. 137Cs concentration in stingray (Dasyatis akajei)

    137Cs, which is of great interest and importance as an indicator of radioactive pollution in marine environments, is one of the long-lived artificial radio-nuclides introduced by the atmospheric deposition of debris from nuclear explosions mainly before 1962. For the estimation of effects of the effluents from nuclear facilities, it is necessary to know the natural variations in the concentration of 137Cs and factors affecting variations in marine organisms. We observed positive correlation between growth and 137Cs in 4 species among 14 major teleost species from fishing grounds along the coast of Japan. No increase in 137Cs concentration with increase of growth was observed in 2 species. In the remaining species no specific correlation is observed. These differences in the patterns were dependent on a change of feed habits with growth. As little is known of the 137Cs concentration in selachian we have investigated the natural variations of 137Cs in stingray. The correlation between growth and the concentration of 137Cs in stingray will be discussed. (author)

  7. Transfer of 137Cs into mother's milk

    The concern of nursing mothers about the contamination of foodstuffs after Chernobyl prompted this investigation of radiocaesium transfer to mother's milk. Between May 1987 and December 1988, duplicates of daily food intakes, as well as the corresponding mothers' milk samples, were collected from 12 nursing mothers for two to four weeks in order to measure the 137Cs activity. Once during the collection period, the total-body activity of each of the mothers involved was measured. Based on our results, 137Cs is transferred into mother's milk not only directly from food intake but also from the accumulated body burden. Approximately 19% of the 137Cs activity from the daily food intake and about 13% of the specific 137Cs body activity of the mother are transferred into 1 litre of mother's milk. (author)

  8. Radiochemical determination of 137Cs in foods

    A determination of radionuclides in food samples is important in commodities in order to attend to regulatory requirements for international trade. As a long-lived radioisotope of cesium, 137Cs is produced as a result of human nuclear activities and than its contamination level evaluation among others radionuclides in foods is necessary. A methodology for the determination of 137Cs in foods, pork and fish, is described. The procedures covered homogenization and freeze-drying of the samples. The 137Cs was measured by gamma spectrometry using Canberra 50% HPGe detector. The counting was carried out with Monte Carlo software for detection conditions optimization including geometry and chemical data information. A certified sample, SRM IAEA-375, was analyzed in order to evaluate the reliability of the method, and the results showed good agreement between the measured and certified values. (author)

  9. Spatial 137Cs distribution in forest soil

    This work presents the distribution of radioactive caesium in several types of forest soil originating from the Lesisko reserve (Opole Province, Poland). Vertical distribution of 137Cs isotope was determined in the profiles related to physicochemical properties of different types of soils and their location. Thickness of emerging genetic horizons, structure and morphology of soil profiles were determined. The highest 137Cs activities were found in Of and A horizons. At the same time, there was a sudden drop of 137Cs activity in mineral horizons of soil profiles. By analysis of caesium radioisotope content and its distribution in soil profiles significant correlations were observed between certain physicochemical properties (e.g. pH value, hydrolytic acidity, granulometric composition) of soils in selected forest habitats. (author)

  10. 137Cs metabolism in pregnant women

    Data from two pregnant women contaminated with 137Cs, body burdens of 0.2 and 300 MBq, respectively at the time of the Goiania accident, were compared. The first one, with lower body burden was exposed during the fourth month of pregnancy, while the second became pregnant three years and eight months after 137Cs intake. For the first woman 137Cs concentrations were equal for the mother, infant and placenta, indicating an easy and homogeneous transport of 137Cs from mother to foetus. The whole body monitoring data from the second woman, who became pregnant four years after intake, did not show a reduction in biological half-life during the pregnancy. Cs concentration in the mother was found to be 13 times higher than in the infant. One possible reason for this result is that four years after intake, Cs is supposed to be concentrated mainly in skeletal muscle tissue. During the pregnancy the blood flux becomes higher in most of the organs and tissues except brain, liver and skeletal muscle tissue. (author)

  11. 137Cs in forest ecosystems in Estonia

    Full text: In the recently published 'Europe's Environment' (1995) one can find the map on 137Cs cumulative deposition in Europe after the Chernobyl accident (source: De Corte et al., 1990). On this map most of the Eastern Europe including Baltic Sea region is practically uncovered. In this reason we decided to present data on accumulation of 137Cs in the forest ecosystems in Estonia. Field sampling for current study has been conducted in 1986 - 1994. 137Cs concentrations were measured in different compartments of model trees, ground vegetation layers, debris and topsoil. The amount of 137Cs varied from 1.9 kBq/m2 in continental Estonia to 28.8 kBq/m2 in north-eastern Ne part of Estonia. The results obtained correspond to data presented in Wahlstroem et al., (1992) for Finland. According to the 'Europe's Environment' criteria northeastern Estonia belongs to the third cumulative deposition zone (10 to 32 kBq/m2). In Estonia the total deposition of 137Cs varies in the range from practically zero to 3.9 kBq/m2 . The calculations of Realo et al. (1994) back to May 1, 1986 gave figures from 0 to 21 kBq/m2. In macro lichens Cetraria, Cladina, Cladonia the rapid changes in 137Cs concentrations were observed: 0.06 - 0.18 kBq/kg in 1982-85, 0.93 - 6.23 kBq/kg in 1986-87, 0.27 -4.26 kBq/kg in 1988-89, 0.05 - 1.46 kBq/kg in 1990-91 and, finally, 0.03 - 0.46 kBq/kg in 1993-94. At the end of the observation period average value of the 137Cs concentrations was the same as maximum before the CRA and decline of the concentrations was 4 times during six years. Average concentrations of 137Cs in two common forest mosses Pleurozium shreberi and Hylocomium splendens was 0.43 kBq/kg of dry matter and in forest debris 0.38 kBq/kg. In 1986 the highest concentration in mushrooms - 16.6 kBq/kg was found in Lactarius sp. (Martin, L., et al., 1991). In 1991 samples of 41 different mushroom species from 63 sample sites mostly in Scots pine stands were analyzed. The highest concentration of

  12. Biological effects of 137Cs, incorporated into organism of rats

    Results of investigating mutagenous and hemotoxic effects of 137Cs on blood lymphocytes of rats are presented. 137Cs was orally administrated into organism of rats as 270 kBq/g chloride solution. 137Cs mutagenous effect was studied on metaphase plates of rat blood lymphocytes in course of rats lifetime experiment. It is stated that 137Cs inducing severe disturbances of genetic material in a great quantity of blood lymphocytes, causes their total killing

  13. Quantitative Model for Estimating Soil Erosion Rates Using 137Cs

    YANGHAO; GHANGQING; 等

    1998-01-01

    A quantitative model was developed to relate the amount of 137Cs loss from the soil profile to the rate of soil erosion,According th mass balance model,the depth distribution pattern of 137Cs in the soil profile ,the radioactive decay of 137Cs,sampling year and the difference of 137Cs fallout amount among years were taken into consideration.By introducing typical depth distribution functions of 137Cs into the model ,detailed equations for the model were got for different soil,The model shows that the rate of soil erosion is mainly controlled by the depth distrbution pattern of 137Cs ,the year of sampling,and the percentage reduction in total 137Cs,The relationship between the rate of soil loss and 137Cs depletion i neither linear nor logarithmic,The depth distribution pattern of 137Cs is a major factor for estimating the rate of soil loss,Soil erosion rate is directly related with the fraction of 137Cs content near the soil surface. The influences of the radioactive decay of 137Cs,sampling year and 137Cs input fraction are not large compared with others.

  14. Reactive barriers for 137Cs retention

    137Cs was dispersed globally by cold war activities and, more recently, by the Chernobyl accident. Engineered extraction of 137Cs from soils and groundwaters is exceedingly difficult. Because the half life of 137Cs is only 30.2 years, remediation might be more effective (and less costly) if 137Cs bioavailability could be demonstrably limited for even a few decades by use of a reactive barrier. Essentially permanent isolation must be demonstrated in those few settings where high nuclear level wastes contaminated the environment with 135Cs (half life 2.3x106 years) in addition to 137Cs. Clays are potentially a low-cost barrier to Cs movement, though their long-term effectiveness remains untested. To identify optimal clays for Cs retention Cs resorption was measured for five common clays: Wyoming Montmorillonite (SWy-1), Georgia Kaolinites (KGa-1 and KGa-2), Fithian Illite (F-Ill), and K-Metabentonite (K-Mbt). Exchange sites were pre-saturated with 0.16 M CsCl for 14 days and readily exchangeable Cs was removed by a series of LiNO3 and LiCl washes. Washed clay were then placed into dialysis bags and the Cs release to the deionized water outside the bags measured. Release rates from 75 to 139 days for SWy-1, K-Mbt and F- 111 were similar; 0.017 to 0.021% sorbed Cs released per day. Both kaolinites released Cs more rapidly (0.12 to 0.05% of the sorbed Cs per day). In a second set of experiments, clays were doped for 110 days and subjected to an extreme and prolonged rinsing process. All the clays exhibited some capacity for irreversible Cs uptake so most soils have some limited ability to act as a natural barrier to Cs migration. However, the residual loading was greatest on K-Mbt (∼ 0.33 wt% Cs). Thus, this clay would be the optimal material for constructing artificial reactive barriers

  15. Separation of 137Cs from nuclear waste

    Sodium zirconate is one member of a family of new inorganic ion exchange materials which have high affinity for all actinides and fission product cations except for Cs+. A combination of cold, tracer and high level liquid waste experiments with sodium zirconate has shown that 70 to 80 and 80 to 100% of the Cs+ in high level liquid waste remains in solution following batch or column equilibration, respectively. The fact that 137Cs can be obtained in relatively pure form permits subsequent conversion directly to an insoluble radiation source. This is of prime importance in areas such as sewage sludge sterilization via γ-ray irradiation. (author)

  16. Fallout 137Cs in soils from North Western Libya

    Fallout levels of 137Cs in surface soil from North Western Libya have been measured using gamma-ray spectrometry. The activity concentrations of 137Cs in soil ranged from 975 to 1720 mBq x kg-1. The areal activity concentrations ranged from 1300 to 2250 mBq x m-2, and were highly correlated with annual precipitation. The effective dose from external exposure to 137Cs is found to be 3 nSv x y-1. (author)

  17. Putative bioindicator of 137Cs in Perna viridis

    Green lipid mussels (Perna viridis L.) are utilized as bioindicators and bioconcentrators not only for marine radionuclide contamination but also for heavy metal bioaccumulation. Depurated P. viridis were incubated in 137Cs-spiked aquarium for 4 days. Soluble protein fractions of soft tissue obtained were electrophoresed (SDS-PAGE) to determine the exposure effects of 137Cs on P. viridis. Results showed the presence of a 154-kDa protein in 137Cs-spiked samples which could be a potential bioindicator of 137Cs in P. viridis. Other differences involving two more proteins (∼94-kDa and∼61 KDa) are reported. (Author)

  18. Speciation of 137Cs in the Baltic sea water

    A possibility of application of Filtrac 391 and Nuclepore filters, Ky-2-8-C exchanger and the Mtilon-T fiber impregnated with Fe, Co, Ni ferrocyanides for separation of particulate and ionic 137Cs in the sea water was investigated. Physico-chemical forms of 137Cs were investigated in the Baltic Sea water during 1995-1997. It was determined that 137Cs was mainly present in ionic form (62-93 %) both in the near-shore and open waters. Concentration of particulate 137Cs ranged from 255 to 625 Bq/kg (dry weight).The distribution coefficient (Kd) of radiocaesium reached values of 2100-9700. (author)

  19. Mechanisms of 137Cs migration in coniferous forest soils

    Field and laboratory studies demonstrate two processes involved in 137Cs migration in coniferous forest soil. The data illustrate that the effects of leaching and litter accumulation combine, over the time interval since deposition, to achieve the observed distribution of 137Cs in the soil profile. Today, under normal field conditions the rate of 137Cs leaching from forest humus is low and even extreme environmental conditions do not increase greatly the extent of 137Cs mobilisation by leaching. A three-phase model of 137Cs migration in the organic horizons of coniferous forest soils is proposed. The phases are discrete but at any point in time the behaviour of some portion of deposited 137Cs will be characteristic of one of the three phases. In the first phase 137Cs intercepted by the canopy is washed to the forest floor where a proportion (20-40% is reported) rapidly percolates through the organic horizons reaching the underlying soil; the remainder is retained in the organic horizons. In the second phase, which our study estimates to last about 5 years, the 137Cs contained within the Ol and Of horizons moves to the Oh horizon. Accumulation of relatively uncontaminated litter on top of the Ol horizon contributes to this migration, while 137Cs mobilised from the Ol and Of horizons by decomposition is leached to the Oh horizon. The 137Cs which reaches the Oh horizon, either by leaching or by decomposition and burial, enters the third phase in which the pace of migration is greatly reduced. Decomposition is slowest in the Oh horizon and the accumulation and turnover of Oh material is also very slow. At the site investigated in this study the bulk of the deposited 137Cs is in this third phase and we suggest that this phase will persist for many years to come

  20. Cumulative deposition of 137Cs in the soil of Korea

    The cumulative deposition of 137Cs in the soil of Korea has been studied. Using γ-ray spectrometry, the concentrations of 137Cs were determined for the soil samples collected to a depth of 20 cm. The average accumulated depositions of 137Cs were estimated roughly to be 2,501 ±499 Bq m-2 in the forest and 1,058 ±322 Bq m-2 in the hill. The inventory value of 137Cs in the forest is about two times higher than that in the hill. Except for some cases, the concentrations of 137Cs in the undisturbed soils decreased exponentially with increasing the soil depth. The influences of rainfall, organic matter content, clay content and pH on the deposition of 137Cs were studied using the field method. Among these factors, the organic matter content played the most important role in the retention and relative mobility of 137Cs in the soil. The other factors such as rainfall, clay content and pH showed weak correlation with the deposition of 137Cs in the soil

  1. Sediment environmental capacity of 137Cs in Daya Bay

    ZHANG Junli; CHEN Jiajun; XU Jialin; LI Yuanxin; HUANG Naiming

    2007-01-01

    Sediment environmental capacity of pollutants is very important for marine environmental management.Based on the methodology of a study on water,soil environmental capacity,and mass conservation theory in a system,the concept and model on sediment environmental capacity for 137Cs in Daya Bay were developed.The static capacity for 137Cs in the upper sediment near the shore at a shallow area was calculated,and the annual dynamic capacity and total dynamic capacity were also calculated through determination of the typical biomass in the sediment.The results showed that the estimated environmental capacity for 137Cs in sediments was approximately equal to the current input of 137Cs into the sediments.Controlling the input of 137Cs in the sediments within the environmental capacity guarantees the sustainability of the current situation of the Daya Bay ecosystem and avoidance of a significant degradation of the system.

  2. {sup 137}Cs accumulation in coastal sediments in Sweden

    Pettersson, H.B.L.; Salih, I. [Linkoeping Univ. (Sweden). Dept. of Radiation Physics; Herrmann, J. [Federal Maritime and Hydrographic Agency, Hamburg (Germany)

    2005-09-15

    Seabed sediment samples were collected in 1998, 2000 and 2001 at 20 sites located in the Baltic Sea and 4 sites in the Skagerrak. The objectives of the sampling campaigns were (i) to establish the coastal sediment distribution of {sup 137}Cs, (ii) to evaluate the vertical core distribution of {sup 137}Cs, (iii) to study the sediment accumulation rates, and (iv) to assess the sediment inventories of {sup 137}Cs. The results show a very high variation in {sup 137}Cs concentrations and an almost 100-fold difference in inventories, showing predominance of Chernobyl derived {sup 137}Cs in the Baltic Proper compared to the western Baltic and the Skagerrak areas. Sediment accumulation rates were highly dependent on sediment types and ranged from 0.05 to 1.8 cm/y.

  3. Evaluating gully erosion using 137Cs and 210Pb/137Cs ratio in a reservoir catchment

    Water erosion in the hilly areas of west China is the main process contributing to the overall sediment of the Yellow River and the Yangtze River. The impact of gully erosion in total sediment output has been mostly neglected. Our objective was to assess the sediment production and sediment sources at both the hillslope and catchment scales in the Yangjuangou reservoir catchment of the Chinese Loess Plateau, northwest China. Distribution patterns in sediment production caused by water erosion on hills and gully slopes under different land use types were assessed using the fallout 137Cs technique. The total sediment production from the catchment was estimated by using the sediment record in a reservoir. Sediment sources and dominant water erosion processes were determined by comparing 137Cs activities and 210Pb/137Cs ratios in surface soils and sub-surface soils with those of sediment deposits from the reservoir at the outlet of the catchment. Results indicated that landscape location had the most significant impact on sediment production for cultivated hillslopes, followed by the terraced hillslope, and the least for the vegetated hillslope. Sediment production increased in the following order: top>upper>lower>middle for the cultivated hillslope, and top>lower>upper>middle for the terraced hillslope. The mean value of sediment production declined by 49% for the terraced hillslope and by 80% for the vegetated hillslope compared with the cultivated hillslope. Vegetated gully slope reduced the sediment production by 38% compared with the cultivated gully slope. These data demonstrate the effectiveness of terracing and perennial vegetation cover in controlling sediment delivery at a hillslope scale. Averaged 137Cs activities and 210Pb/137Cs ratios in the 0-5 cm surface soil (2.22-4.70 Bq kg-1 and 20.70-22.07, respectively) and in the 5-30 cm subsoil (2.60 Bq kg-1 and 28.57, respectively) on the cultivated hills and gully slopes were close to those of the deposited

  4. 137Cs in the western South Pacific Ocean

    The 137Cs activities were determined for seawater samples from the East Caroline, Coral Sea, New Hebrides, South Fiji and Tasman Sea (two stations) Basins of the western South Pacific Ocean by γ spectrometry using a low background Ge detector. The 137Cs activities ranged from 1.4 to 2.3 Bq m-3 over the depth interval 0-250 m and decreased exponentially from the subsurface to 1000 m depth. The distribution profiles of 137Cs activity at these six western South Pacific Ocean stations did not differ from each other significantly. There was a remarkable difference for the vertical profiles of 137Cs activity between the East Caroline Basin station in this study and the GEOSECS (Geochemical Ocean Sections Study) station at the same latitude in the Equatorial Pacific Ocean; the 137Cs inventory over the depth interval 100-1000 m increased from 400 ± 30 Bq m-2 to 560 ± 30 Bq m-2 during the period from 1973 to 1992. The total 137Cs inventories in the western South Pacific Ocean ranged from 850 ± 70 Bq m-2 in the Coral Sea Basin to 1270 ± 90 Bq m-2 in the South Fiji Basin. Higher 137Cs inventories were observed at middle latitude stations in the subtropical gyre than at low latitude stations. The 137Cs inventories were 1.9-4.5 times (2.9 ± 0.7 on average) and 1.7-4.3 times (3.1 ± 0.7 on average) higher than that of the expected deposition density of atmospheric global fallout at the same latitude and that of the estimated 137Cs deposition density in 10o latitude by 10 deg. longitude grid data obtained by Aoyama et al. [Aoyama M, Hirose K, Igarashi Y. Re-construction and updating our understanding on the global weapons tests 137Cs fallout. J Environ Monit 2006;8:431-438], respectively. The possible processes for higher 137Cs inventories in the western South Pacific Ocean than that of the expected deposition density of atmospheric global fallout may be attributable to the inter-hemisphere dispersion of the atmospheric nuclear weapons testing 137Cs from the northern

  5. 137Cs contaminated waste disposal in cement factory: Environmental problems

    In the course of utilization (May-June '91) of aluminum slags polluted by 137Cs at the cement factory Presacementi in Robilante (Cuneo, Italy) and during the following months, samples were taken in particular points of the plant, at fixed frequencies. Samples were analyzed to determine 137Cs concentration. Collected data were used to study the behaviour of the element throughout the process. Emissions and ground level air concentrations were estimated from the available data. Contamination of the manufactured cement were monitored until negligible values of 137Cs concentration were attained

  6. Long-term behaviour of 137Cs in Finnish lakes

    Deposition of 137Cs from Chernobyl accident was unevenly distributed in Finland. This caused large variation to contents of 137Cs in freshwater fish in Finnish lakes. In the course of time environmental processes like runoff, water flow, hydrological cycling, sedimentation and chemical parameters as e.g., K of lake water, topography of the catchment affect the transfer of 137Cs in water sheds. Most of the Finnish lakes are deficient in nutrients and hence the accumulation of 137Cs into fishes is high. High amount of humic substances is also typical of Finnish lakes. About 6000 freshwater fish samples from 350 Finnish lakes have been analysed for 137Cs in 1986-2003. Sampling was focused on the central parts of Finland with highest deposition of 137Cs, but samples from other areas were also analysed. Large lakes, most important for freshwater fishing in Finland, and small oligotrophic lakes, in which the highest contents of 137Cs were expected to be found, were included in the study. Variation range of 137Cs in fish was still in 2003 large, from 5 Bq/kg to 5000 Bq/kg (fresh weight). Water samples from about 30 lakes were taken in 1998 and 2002 and analysed for 137Cs. Contents of 137Cs in lake waters varied then from 4 to 330 Bq/m3. During the first years after the deposition in 1986, the amount of the deposited 137Cs in the lake was the dominant factor on the distribution of 137Cs in fish and surface water. Later study on regional behaviour of 137Cs in fish revealed differences in decrease rates in the large drainage areas [2]. Temporal changes of 137Cs in water and especially in fish in individual lakes of various types, even in those located close to each other, differ still much. Transfer coefficients of 137Cs from the deposition to water, TFw (Bq/m3 in water/kBq/m2 deposited) of the lakes included in this study varied from 0,40 to 8,7 in 1998. Transfer factors from the deposition to various species of fish from various lakes, TFf (Bq/kg in fish / Bq/m2), varied

  7. Accumulation of 137Cs in puddle sediments within urban ecosystem

    The role of puddle sediments as a final depot of 137Cs horizontal migration within the urban landscape is studied using the example of Ekaterinburg city, Russia. Radioactive contamination in the city appeared due to fallout after atmospheric testing of nuclear weapons and nuclear accidents. Contamination density of 137Cs in the region was assessed from archive data to be about 5.1 kBq/m2, of which the maximum activity concentration (137Cs activity concentration in puddle sediments of 80 Bq/kg, with a maximum value of 540 Bq/kg. It is estimated that horizontal migration has led to about a fourfold concentration of 137Cs in puddle sediments.

  8. Migratory capacity of 137Cs in water-containing rocks

    The effects of a number of physicochemical and hydrogeologic factors (sorption capacity of rocks, mechanisms of cesium absorption by these, chemical composition of underground waters) on 137 Cs migration in the case of radioactive contamination of underground water in areas of location of atomic power stations have been studied. Approximate equations of ion-exchange sorption may be applied for predicting 137 Cs migration in rocks within the aeration zone and in water-bearing horizons

  9. /sup 137/Cs radioactive dating of Lake Ontario sediment cores

    Ward, T.E.; Breeden, J.; Komisarcik, K.; Porter, R.; Czuczwa, J.; Kaminski, R.; McVeety, B.D.

    1987-12-01

    The distribution of /sup 137/Cs in sediment cores from Lake Ontario provides estimates of the sediment accumulation rates. Geochronology with /sup 210/Pb dating and distribution of Ambrosia (ragweed) pollen compare well with /sup 137/Cs dating. These methods can determine with precision, changes in sedimentation occurring over the past 100 years or so. Typical sedimentation rates of 0.18-0.36 cm/yr were measured. 16 refs., 3 figs., 2 tabs.

  10. 137Cs radioactive dating of Lake Ontario sediment cores

    The distribution of 137Cs in sediment cores from Lake Ontario provides estimates of the sediment accumulation rates. Geochronology with 210Pb dating and distribution of Ambrosia (ragweed) pollen compare well with 137Cs dating. These methods can determine with precision, changes in sedimentation occurring over the past 100 years or so. Typical sedimentation rates of 0.18-0.36 cm/yr were measured. 16 refs., 3 figs., 2 tabs

  11. Distribution of 137Cs in water leachates of forest humus

    The distribution of 137Cs in water extracts of organic layers of forest soils was investigated using an ultrafiltration method. Samples were taken from two sites in the Bavarian Alps. The different horizons of the organic layers were extracted by column elution with water and 50 mmol/litre CsCl solution. Water extracts were fractionated using membranes with the molecular weight cutoff of 500, 1000 and 3000 Dalton to determine the molecular weight distribution of dissolved organic carbon (DOC). The activity of 137Cs associated with the different DOC-fractions was measured by direct gammaspectrometry. Cesium-137 in the fraction smaller than 500 Dalton was defined as 'ionic'. The results indicated a change of the binding sites depending on the degree of decomposition and humification in the profile. Organic bound 137Cs was identified in all extracts. High mobilities of DOC and 137Cs were observed in the same horizons, fractionation showed then low-molecular-weight DOC and 137Cs mainly in ionic form. In horizons with high-molecular-weight DOC the portion of organic bound 137Cs ranged up to 40%. (author)

  12. Estimation of erosion rate using natural isotop 137Cs

    The investigation of erosion rate using natural isotope 137Cs had been done in hilliness area at GOULBURN-NWS-Australia. The presentation of 137Cs in natural was as a result of nuclear weapon testing in the middle of 1950's. Fallout of 137Cs input, when it reached the ground, it rapidly adsorbed at the soil. 137Cs bind very strong at the fine soil, so it can be used as tracer in the study of soil movement. Soil samples were taken using coring device (di=10 cm, h=20 cm), and were brought to laboratorium for short commun analysis. The preparation are drying, weighing, crushing and sieving. The 137Cs content of fine samples that pass the 1 mm sieve were analyzed using gamma-spectrometer. The total erosion rate was calculate by ploting the 137Cs values in the topography map of study area. The result showed that erosion was very low, and total erosion rate is 130 kg/ha.y. (authors)

  13. Transfer of 137Cs through the food chain to man

    Deposition, concentrations in diet, and body burdens of 137Cs have been measured since 1954 at various sites throughout the world. This report is a compilation and updating of various fallout 137Cs measurements and an interpretation of transfer properties of 137Cs from deposition to diet and from diet to man. An empirical model is used to correlate deposition and diet data. Direct foliar contamination, stored food supplies, and uptake from soil contribute to the dietary levels of 137Cs. The accumulation of 137Cs by man is described by a single exponential model. The inferred biological half-times, 200 to 400 days, are somewhat greater than the half-time of about 100 days obtained from shorter term studies. Differences in body burdens due to sex, age, and weight are discussed. During the period 1954 to 1974, the internal dose from fallout 137Cs, based on average body burdens, is estimated to be 4 to 5 percent of the 21 year radiation dose from 40K

  14. Specific activity 137Cs at fishes of Ukraine current state

    Specific activity of 137Cs at fishes of reservoirs of 30 kilometers ChNPP zone (Pripyat river and its bays, lakes, cool-ing-pond of ChNPP, etc.), water basins of Dneprovsky cascade, Shatsky lakes and Black sea near town Sudak is investigated during 2010 - 2012. Levels of specific activity of 137Cs at fishes in many respects are defined by flowage of the reservoir. Normally, the flowage of the reservoir is more, the levels of specific activity of 137Cs at fishes are less. The greatest specific activity of 137Cs at fishes was registered in the north of Ukraine in closed and half-closed reservoirs of 30 kilometers ChNPP zone - to 32000 Bqk/kg. In the southern direction activity of 137Cs at fishes decreases from 4,8 to 78,5 Bq/kg in Kyiv water basin to 1 - 6 Bq/kg, in the Kahovsky water basin and to 0,6 - 1,9 Bq/kg in the Black sea. In large reservoirs the greatest specific activity of 137Cs, as a rule, is registered in fishes of the higher trophic levels

  15. Plant remediation of soil contaminated with 137Cs

    A pot experiment was conducted to evaluate the bio-remediation of soils contaminated with 137Cs. The selected plants are Cucurbita moschata Duchesne, Brassica chinensis L, Chloris virgata, Beta oulgaris L. Hongye, Beta oulgaris L. Dongshengye and Beta oulgaris L. The soils samples were taken from the paddy field, 2 km from the Dayawan nuclear power plant and Qinshan nuclear power plant, respectively, and cinnamon soil from the cultivated land in Beijing. The results show that all the employed species of plant have a higher accumulation to 137Cs with the increased grade of the radioactivity of 137Cs. A good correlation exist with the coefficient (r2) of 0.9989. When the contaminated radioactivity of 137Cs is in the same level the uptake of Cucurbita moschata Duchesne, Brassica chinensis L. and Chloris virgata increased with the decrease of pH value ranged 5.22-7.69. The ability of bioremediation in the orders were Chloris virgata, Brassica chinensis L., Beta oulgaris L. Hongye, Cucurbita moschata Duchesne, Beta oulgaris L. and Beta oulgaris L. Dongshengye, according to the comprehensive evaluation of transfer factor, specific activity of plant in dry weight of biomass and total absorption of 137Cs by the individual plant in the same area. (authors)

  16. Sorption of 137Cs from Aqueous Waste Solutions using Pottery

    A simple and inexpensive method for sorption of 137Cs from aqueous solutions using a highly available vase shape pottery material has been investigated. Porosity of the used pottery allowed for the penetration of the radioactive solution through its permeable body. Two routes had been investigated for cesium removal from the radioactive solutions. In the first one, pottery bodies were immersed into the radioactive solutions. In the second method; the radioactive solutions were filled the inner volumes of the pottery bodies. Vase shape pottery showed higher sorption capability for 137Cs much more than its powder forms, especially in the alkaline medium. Pottery bodies showed high potential for 137Cs removal. Adsorption isotherms revealed good lit to the Freundlich and Langumir isotherms. During sorption processes outside and inside the pottery body, 137Cs was well captured inside the amorphous microstructure of the pottery body. In this respect, micro filtration of cesium radionuclides through the used pottery could be postulated. Desorption experiments indicated higher immobilization affinity for radiocesium into pottery bodies, which indicates a high containment for 137Cs with an irreversible fixation mechanism

  17. Household methods to reduce 137Cs contents of mushrooms

    High radiocaesium contents in different species of mushrooms have been observed in areas contaminated by radiocaesium deposition after the Chernobyl accident in 1986. There has been no significant reduction in the 137Cs contents of mushrooms during the past ten years, besides via radioactive decay. The internal radiation dose received via mushrooms can be reduced by processing mushrooms before consumption. Various household methods were studied to find out their efficiency to reduce 137Cs contents of mushrooms. The methods tested were the same as normally used in cooking. The tests were made for the species of edible mushrooms widely consumed. The retention factors for the treatments tested were in most cases 0.2-0.3. The efficiency of treatments in reducing the 137Cs contents increased with larger water volumes and prolonged treatment times

  18. Radiochemical determination of {sup 137}Cs in foods

    Kastner, Geraldo F.; Ferreira, Andrea Vidal; Monteiro, Roberto P.G., E-mail: gfk@cdtn.br, E-mail: avf@cdtn.br, E-mail: rpgm@cdtn.br [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil)

    2013-07-01

    A determination of radionuclides in food samples is important in commodities in order to attend to regulatory requirements for international trade. As a long-lived radioisotope of cesium, {sup 137}Cs is produced as a result of human nuclear activities and than its contamination level evaluation among others radionuclides in foods is necessary. A methodology for the determination of {sup 137}Cs in foods, pork and fish, is described. The procedures covered homogenization and freeze-drying of the samples. The {sup 137}Cs was measured by gamma spectrometry using Canberra 50% HPGe detector. The counting was carried out with Monte Carlo software for detection conditions optimization including geometry and chemical data information. A certified sample, SRM IAEA-375, was analyzed in order to evaluate the reliability of the method, and the results showed good agreement between the measured and certified values. (author)

  19. Transfer of 137Cs into fish in small forest lakes

    The transfer of 137Cs into fish in seepage and drainage lakes from 1988 to 1992 was analysed using linear regression. Empirical results for 137Cs in lake water and fish were used to calculate concentration factors (CFs). In the drainage lakes the CF decreased during the study period by 9% per year whereas in the seepage lakes the CF increased significantly by 4.3% per year. The transfer of 137Cs into pike was significantly (1.6 times) higher than that into perch. The CF increased on average by 3.4% for each 1-cm increase in the median size of perch. The relationship between the water chemistry and the CF differed between clear-water seepage and brown-water drainage lakes.

  20. 137Cs transfer coefficients from fodder to cow milk

    The transfer of 137Cs from the components of cows' diets to milk was followed in detail on 10 farms in the north-eastern region of Italy (Friuli-Venezia Giulia) from June to July 1988. Samples of milk, grass and other components of the cows' diet were collected regularly and analysed for radiocaesium content. The transfer factors, calculated for 137Cs after a four-week feeding period with contaminated silage, were higher (0.0064) than those calculated in 1987 in the same area (0.0030). This may be attributable to the fact that the 137Cs associated to the forage administrated to cows in 1988 was completely incorporated in the plant and thus more assimilable to the cattle. (Author)

  1. Household methods to reduce {sup 137}Cs contents of mushrooms

    Kostiainen, E. [Radiation and Nuclear Safety Authority - STUK, Helsinki (Finland)

    2005-09-15

    High radiocaesium contents in different species of mushrooms have been observed in areas contaminated by radiocaesium deposition after the Chernobyl accident in 1986. There has been no significant reduction in the {sup 137}Cs contents of mushrooms during the past ten years, besides via radioactive decay. The internal radiation dose received via mushrooms can be reduced by processing mushrooms before consumption. Various household methods were studied to find out their efficiency to reduce {sup 137}Cs contents of mushrooms. The methods tested were the same as normally used in cooking. The tests were made for the species of edible mushrooms widely consumed. The retention factors for the treatments tested were in most cases 0.2-0.3. The efficiency of treatments in reducing the {sup 137}Cs contents increased with larger water volumes and prolonged treatment times.

  2. Surface activity of 137Cs, sheet 35 - Trnava

    In the predominantly geomorphologically mountainous terrain the map of surface activity of 137Cs was compiled from the results of exploration activities on scale 1:200 000 and in the Danube upland (between Povazsky Inovec and Little Carpathians) on scale 1:50 000. Surface activities of 137Cs are significantly unevenly distributed. The most widespread surface activity of 137Cs in the interval from 1000 to 2000 Bq · m-2 was mapped on mostly continuous area in the central part of map sheet and represents 68.4% of its area. The exception is only a small increase (10,225 Bq · m-2) in Banovska upland south-east from the village Zlatniky. Higher surface activities of 137Cs were registered in the north part of the map sheet. There from neighbouring map sheet (34 - Znojmo) reaches an area of increased values (3000 to 5000 Bq · m-2, max. 6550 Bq · m-2), geomorphologically falling into the western part of the White Carpathians. Relatively high surface activities of 137Cs were found in the south-east part of the map sheet in the Tribec mountains near Skycov (max. 7426 Bq.m-2), in Zitavska flood-plain south of the Zlate Moravce (max. 13962 Bq · m-2), but mainly in Vtacnik and Stiavnicke Hills, where in Nova Bana was measured the maximal surface activity 16497 Bq · m-2. Considering sizeable areal expansion of lower levels of surface activity of 137Cs, the geometric mean (1338 Bq.m-2) on this map sheet corresponds to the national average. (authors)

  3. Changes in 137Cs transfer to agricultural products

    The food production and food harvesting systems common in the areas contaminated by the Chernobyl accident in Republic of Belarus can be grouped into three major categories: collective farm produce, private farming produce and natural foods collected from natural ecosystems. The collective farm system provided the smallest contribution (8-12 %) to the intake of 137Cs. Natural food was the major contributor to the intake at one study site (73 %), and private produce was the major contributor (60 %) at the other study site. Assessment of the situation just after the accident (one year) shows that collective farming was still a minor contributor to 137CS intake (10 %) whilst private fanning would have been the major contributor wherever private milk production and consumption continued. The extent to which inhabitants consume natural foods from forests has a considerable effect on their 137CS intake. The comparative importance of food products from natural ecosystems increases with time due to the long effective ecological half lives of 137Cs in unimproved pastures and forests. Estimation of the contribution to the fluxes of 137Cs from the different production and harvesting systems showed that the contribution from private farming and food harvesting from natural ecosystems may also be significant, contributing 14-30 % to the total fluxes of 137Cs from an area even if the quantity of food produced in these systems is small. However, the major contributor to the flux exported from an area was the collective farming system, accounting for about 70-86 % of the total. Refs. 12 (author)

  4. Uptake and transfer factors of 137Cs by mushrooms

    The 137Cs content of 118 species (668 samples) of higher fungi collected in the period from August 1984 to October 1989 at three different locations in Styria, Austria, was determined by gamma-spectrometry. The Cs-content of most mushrooms has been increasing since September 1986. In order to find out which factors determine the 137Cs-contamination of mushrooms and the transfer-value soil to mushroom, the concentration of total and plant-available radiocesium in soils as well as the pH-value, the content of humus, clay, silt, sand, exchangeable cations, the composition of the clay minerals, and the particle size distribution of the soils of two different locations were examined. The higher the 137Cs contamination of the soil, the thicker the layer of humus and the higher the content of humus, the lower the pH-value, and the lower the amount of essential cations, especially of K+, the higher the amount of 137Cs plant-available will be. Therefore, the contamination of the mushrooms in the coniferous forest of Koralpenblick (1000 m) is higher than in the mixed forest at the Rosenberg around Graz at approx. 500 m height. Of 26 different species of mushrooms measured at both sites, only 61% show the highest TF-values soil to mushrooms also at the Koralpenblick. In the spruce forest at Koralpenblick there are many species of mushrooms with high 137Cs-contamination which were not found at the Rosenberg. However, the properties of the species to which a mushroom belongs are more important than environmental conditions and soil properties. The transfer values of 40K stay within narrow bounds, whereas those of 137Cs differ widely. (orig.)

  5. Declassification of 137Cs liquid wastes by reverse osmosis

    In June 1998, a 137Cs source was accidentally melted in one of the furnaces of a stainless steel production company located in Spain. As a result of this incident, the furnace and its cooling circuit were radioactively contaminated. LAINSA (Logistica y Acondicionamientos Industriales S.A.) company took charge of the plant decontamination process, in which 40 m3, approximately, of 137Cs contaminated water with a mean activity of 300 kBq/L were generated. This company contacted the Chemical and Nuclear Engineering Department of the Polytechnic University of Valencia (UPV) to develop a project for radioactive liquid wastes treatment

  6. The behaviour of 137Cs in the aquatic environment

    Through 137Cs concentration profiles in sediments from Rochedo Reservoir, it was possible to estimate the amount of this radionuclide (94 TBq) which has reached the Meia Ponte River system, as a consequence of the Goiania Radiological accident in 1987. Based on in-situ measurements as well as on laboratory studies, the influence of NH4+ concentration on the Kd value was also investigated. The results have shown that for high NH4d+ concentrations there is a clear correlation between both parameters. It was also observed the influence on the ageing effect on the 137Cs release from the sediment, as well as of the illite content on it. (author)

  7. Transfer factor values of 137 Cs from latosoils to vegetables

    Transfer Factor values for black beams, radish and carrot were obtained for soils artificially and accidentally contaminated in Goiania during 1987. Differences of 137 Cs-soil-to-plant transfer were discussed in the light of pedology and crop type. These values were about one order of magnitude higher than mean values reported by IUR for temperature climate for the same crops. These results advertising for the peculiar dynamics of 137 Cs in tropical soils and for needs to obtain regional data to be used in assessment dose models. (author)

  8. Mathematical model of 137Cs dynamics in the deciduous forest

    A mathematical model of 137Cs behaviour in the forest ecosystem is presented. The behaviour of this radionuclide is assumed to obey the same regularities as the behaviour of its stable chemical analogue, potassium. Radionuclide dynamics are considered in parallel with the dynamics of the phytomass. Radionuclides contained in the vegetation are pooled into two basic compartments: external and internal contamination, with separate analysis of each. The model was verified using the data obtained in the 30-km zone of the Chernobyl NPP in 1986-1994. The algorithm described was found to be the most efficient in terms of 137Cs behaviour in the forest environments

  9. 137Cs in the fungal compartment of Swedish forest soils

    The 137Cs activities in soil profiles and in the mycelia of four ectomycorrhizal fungi were studied in a Swedish forest in an attempt to understand the mechanisms governing the transfer and retention of 137Cs in forest soil. The biomass of four species of fungi was determined and estimated to be 16 g m-2 in a peat soil and 47-189 g m-2 in non-peat soil to the depth of 10 cm. The vertical distribution was rather homogeneous for two species (Tylospora spp. and Piloderma fallax) and very superficial for Hydnellum peckii. Most of the 137Cs activity in mycelium of non-peat soils was found in the upper 5 cm. Transfer factors were quite high even for those species producing resupinate sporocarps. In the peat soil only approximately 0.3% of the total 137Cs inventory in soil was found in the fungal mycelium. The corresponding values for non-peat soil were 1.3, 1.8 and 1.9%

  10. Transport of 137Cs to the Southern Hemisphere in an ocean general circulation model

    Tsumune, Daisuke; Aoyama, Michio; Hirose, Katsumi; Bryan, Frank O.; Lindsay, Keith; Danabasoglu, Gokhan

    2011-04-01

    137Cs originating from global fallout is transported into the ocean interior by advection and diffusion, and the 137Cs concentration is reduced by radioactive decay. 137Cs concentrations in the global ocean can be simulated by global integration of the coarse-resolution Parallel Ocean Program to understand the mechanism of material transport in the ocean. We investigated the transport mechanism of 137Cs to the Southern Hemisphere using an ocean general circulation model (OGCM) and compared the simulated results with observations of 137Cs concentrations in the Southern Hemisphere. 137Cs was deposited on the ocean surface mainly as global fallout originating from atmospheric nuclear weapons testing since 1945, and the global distribution of cumulative 137Cs deposition has been reconstructed from global measurements of 137Cs in rain, seawater, and soil. We estimated the global distribution of 137Cs deposition from 1945 to 2003 using these distribution data, 137Cs deposition data observed at the Meteorological Research Institute, Tsukuba, Japan, from 1958 to 2003, and 137Cs deposition data for 1945-1957 estimated from ice-core data. We compared the simulated results with 137Cs sections from the South Pacific, Indian, and South Atlantic Oceans obtained during the BEAGLE2003 cruise in 2003. The simulated 137Cs sections were in good agreement with the observations, except for the effects of mesoscale eddies, which not be simulated by the model because of its coarse resolution. OGCMs can simulate the general pattern of 137Cs distribution in the world’s oceans and improve our understanding of the transport mechanism leading to those 137Cs distributions on a time scale of several decades. The model simulation results suggest that the 137Cs deposited in the North Pacific advected to the South Pacific and Indian Ocean, and then to the South Atlantic over about four decades. The North Pacific is thus an important source area of 137Cs to the Southern Hemisphere.

  11. Contribution of Asian dust to atmospheric deposition of radioactive cesium (137Cs)

    Both Asian dust (kosa) transported from the East Asian continent and locally suspended dust near monitoring sites contribute to the observed atmospheric deposition of 137Cs in Japan. To estimate the relative contribution of these dust phenomena to the total 137Cs deposition, we monitored weekly deposition of mineral particles and 137Cs in spring. Deposition of 137Cs from a single Asian dust event was 62.3 mBq m-2 and accounted for 67% of the total 137Cs deposition during the entire monitoring period. Furthermore, we found high 137Cs specific activity in the Asian dust deposition sample. Although local dust events contributed to 137Cs deposition, their contribution was considerably smaller than that of Asian dust. We conclude that the primary source of atmospheric 137Cs in Japan is dust transported from the East Asian continent

  12. Distribution of 137Cs radionuclide in industrial wastes effluents of Gresik, East Java, Indonesia

    The distribution of anthropogenic radionuclides 137Cs was measured from industrial waste effluent of Gresik to Gresik Sea in east Java, Indonesia. The activity of 37Cs detected at all stations was much lower than in northeast Japan both before and after NPP Fukushima accident. This indicated that in Gresik industrials waste did not consist of 137Cs. The lowest activity 137Cs occurred at the station nearest to the industrial waste effluent that contained some particle ions that were able to scavenge 137Cs and then precipate this radionuclide. Furthermore, the greatest 137Cs occurred at the station that has high current speeds that stirred up sediment to release 137Cs in seawater as a secondary source. The lowest salinity did not effect on the activity of 137Cs even though the lowest salinity and activity 137Cs occurred at the same station. (author)

  13. Distribution of 137Cs Radionuclide in Industrial Wastes Effluents of Gresik, East Java, Indonesia

    Muslim

    2015-04-01

    Full Text Available The distribution of anthropogenic radionuclides 137Cs was measured from industrial waste effluent of Gresik to Gresik Sea in east Java, Indonesia. The activity of 37Cs detected at all stations was much lower than in northeast Japan both before and after NPP Fukushima accident. This indicated that in Gresik industrials waste did not consist of 137Cs. The lowest activity 137Cs occurred at the station nearest to the industrial waste effluent that contained some particle ions that were able to scavenge 137Cs and then precipate this radionuclide. Furthermore, the greatest 137Cs occured at the station that has high current speeds that stirred up sediment to release 137Cs in seawater as a secondary source. The lowest salinity did not effect on the activity of 137Cs even though the lowest salinity and activity 137Cs occured at the same station

  14. Geographic zones with increased migration of 137Cs from environment into food stuffs

    Increased 137Cs migration from the environment into the human organism through the biological lichen-deer-man chain in the arctic region is considered. Levels of 137Cs content in lichen and deer meat are presented. The degree of 137Cs migration in the wooded district on food stuffs of local production (milk, mushrooms, meat) is presented. The increased 137Cs content is found in food stuffs of animal and vegetable origin in the wooded district due to peculiarities of natural conditions

  15. Behaviour of 137Cs in the Boreal forest ecosystem of central Sweden

    Behaviour of Chernobyl fallout 137Cs in a coniferous forest ecosystem in central Sweden was investigated between 1990 and 1994. Results demonstrated that forest soil belongs to nutrient deficient type, and deposited fallout 137Cs from Chernobyl nuclear accident (CNA) was retained (85%) in the upper 5 cm of humic forest soil layer, with a venial migration deeper into soil profile. No correlation between forest soil exchangeable and total potassium (K+) and 137Cs transfer parameters was observed. However, addition of K+, found to efficiently reduce 137Cs uptake by sheep's fescue and the addition of stable caesium (133Cs+) enhanced it. The addition of ammonium (NH4+) was slightly stimulating the uptake of 137Cs by sheep's fescue in the first cut only. Field plants showed a considerably reduction in their 137Cs activity concentrations. Relative to their 137Cs levels of 1986-89, a little reduction in heather (16%) occurred eight years after CNA. In contrast the reductions in lingonberry and bilberry were 87% and 68%, respectively. Three fractions of forest soil bound 137Cs were observed due to sequential extraction procedure (SEP). The first, is easily extractable 137Cs fraction (F1+F2), it comprises 22% of total forest soil 137Cs inventory in the upper 5 cm layer. The second, is soil organically and biologically bound 137Cs (F3+F4) comprises about 30% of soil bound 137Cs. This fraction might be accounted for long-term soil available 137Cs for plant uptake after bio-degradation processes by soil microorganisms. The third, is the residual fraction (F5), it comprises more than 35% of total forest soil 137Cs inventory, and may be associated with soil components which are probably of organic nature. Sorption of 137Cs by zeolite (Mordenite) revealed that soil bound 137Cs is to some extent more mobile in forest soils with high OM% and low pH than those with low OM%. 99 refs

  16. Fractionation of caesium (137Cs) in coniferous forest soil in central Sweden

    Sequential extraction procedure (SEP) was applied for fractionation of Chernobyl fallout 137Cs bound onto soils of a coniferous forest ecosystem located in central Sweden. Results of sequentially extracted 137Cs fractions demonstrated that 8% (mean value) of the total deposited 137Cs was water soluble (F1) and 13% was NH4OAc extractable (F2). Oxidation of F2 residuals by H2O2 led to a release of 15% of soil-bound 137Cs (F3). Acid digestion of F3 residuals showed a possibility of releasing an extra amount of soil-bound 137Cs, 22% of the total soil 137Cs inventory (F4). These two fractions (F3 and F4) include strongly bound 137Cs that seems to require longer biodegradation processes by soil microflora and microfauna before becoming available for uptake by plants and fungi. More than 37% of the total soil 137Cs inventory was bound onto soil residuals in a non-extractable form that includes slowly degradable organic matter and other soil residual compartments. The distribution coefficient (Kd) was rather low and shows an inverse relation with the increase of percentage of soil organic matter, which indicates a week binding of 137Cs onto forest soil. In contrast, chemical fractionation of soil bound 137Cs showed a substantial fraction of 137Cs was strongly bound onto soil as organically bound 137Cs. Apparently, the binding processes of radiocaesium onto forest soil seems to be time dependent

  17. Standardization of 137 Cs+137m Ba by Liquid Scintillation

    A procedure for the preparation of a stable, homogeneous solution of ''137 Cs+''137m Ba, for use in liquid scintillation measurements, is described. Its count rate stability and spectral time evolution has been followed for several weeks. The solution has been standardised by the CIEMAT/NIST method in both Ultima-Gold and Insta-Gel, to a combined uncertainty lower than 0,51% (k=1)

  18. Uncertainty in the modelling of 137Cs turnover in lakes

    In the context of the IAEA-CEC co-ordinated research programme on Validation of Environmental Model Predictions (VAMP), a generic model for lake ecosystems has been tested under a variety of environmental conditions. The main emphasis has been placed on predicting the levels of 137Cs in water and predatory fish, which are of most concern from a radiological point of view. 2 figs

  19. Activity of 137Cs in mushrooms from Slovak Republic

    In this paper, activity concentrations of radiocesium in mushrooms from various locations in the Slovak Republic during the year 2001 are presented. The highest activity concentration of 137Cs measured was 966 Bq/kg, for Suillus luteus from Senica. Mushrooms belonging to Boletaceae which grow in Central Europe are not only bio-indicators of the environmental contamination with radiocesium, but might also represent depending on their actual radiocesium contamination - some risk factor if consumed too extensively. (authors)

  20. Distribution of 137Cs in soil samples of Goa environment

    Systematic studies on distribution of 137Cs in soil samples of Goa region have been carried out using gamma spectrometric technique. Soil samples were collected from different places of Goa region and studied their depth profile and seasonal variation of the activity. Efforts have been to find the correlation between this radionuclide concentration and the soil organic matter content and possible inferences were drawn. (author)

  1. Leaching of /sup 137/Cs from an epoxide resin

    Leaching of /sup 137/Cs has been found to be independent of surface-area-to-volume ratio and leachant renewal frequency. Short-term leaching can be satisfactorily described by a simple diffusion model. Longer-term data are better explained by including a first-order reaction combined with diffusion. γ-irradiation to 10/sup 7/ Gy has little effect on leaching behaviour of samples containing IX resin

  2. 137Cs and 210Pb distribution in Manila Bay sediment

    Two radionuclides were measured in surface sediment samples taken from geographically distributed sections of Manila Bay, namely cesium-137 (137Cs) and lead-210 (210Pb). Results indicated a noticeable change in the radioactivity concentration levels in sediments collected in 2005 and 2010, with a median concentration of 1.0 and 2.64 Bq kg-1, respectively. Higher levels of 137Cs radioactivity were measured in the northern and inner portion of the bay adjacent to major river systems, agricultural and highly industrialized urban areas. 137Cs isotope increased in activity in most of the samples especially in the northwestern areas of Bataan and Pampanga with five times more than the activity from the first sampling measurements. Nevertheless, radioactivity concentrations observed in surface sediments along the bay are within the range of radioactivity in several areas monitored in the Northern Hemisphere. The country has been frequented by tropical cyclones and storms that have caused erosion, which may have introduced elevated material input in the bay. In addition, wind-driven circulation especially in the shallower areas of the bay is a possibility for the substantial sediment movement and accumulation along this coast. Conversely, areas with higher 137Cs have lower values of 210Pb. In an undisturbed environment, 210Pb deposition values are assumed nearly constant. Hence, changes in the radioactivity concentration levels of these radionuclides can be an indicator of pollution input from land-based sources, sediment movement and reworking in the coastal areas. At present, there is very limited information on the radioactivity level of various radioisotopes in Manila Bay.The data obtained are benchmark values against which changes that will be occurring in the bay can be assessed. (author)

  3. Study on accumulation of 137Cs in aquatic organisms

    FengDing-Hua; CheungT

    1998-01-01

    The organisms were cultivated for 7d in well water contaminated with 137Cs,The experimental results show that the accumulation level of tissues of carassius auratus had the order of gill>viscera>epidermis(including scales)>bone(including head and tail)>flesh.The concentration capability of them had the order of shrimp>carassius auratus>ophiocephalus argus,The concentration factors(CF) of shrimp was 12.6 times of that of ophiocephalus argus.

  4. 137Cs, trace and toxic elements distribution in Austrian mushrooms

    Various mushroom species have been analyzed for their elemental composition (i.e., Al, B, Ba, Ca, Cd, Cr, Cu, Fe, K, Mg, Mn, Na, P, Sr and Zn) by means of ICP-AES. The accuracy of the measurements was confirmed by analyzing a series of the same samples by short time activation analysis. The data were evaluated statistically including the values of 137Cs. The results denote that the distribution of these elements and their correlation coefficients are highly distinctive for each mushroom species. K, Na and P were found to correlate negatively with 137Cs in most species. Suillus grevillei and Cantharellus cibarius show high Be values (0.27 and 0.30 μg g-1, respectively), while Pb was high in Suillus grevillei (16.3 μg g-1) and Amanita rubescens (9.3 μg g-1). Higher levels of Cd were found in Rozites caperata and Russula vesca with a mean of 9.2 and 16.1 μg g-1, respectively. Cluster analysis was applied to classify these samples according to their botanical species using their elemental composition . The concentrations of Al, Cr, Mn, Na and 137Cs have no influence on the classification of these samples. (author) 9 refs.; 3 figs.; 3 tabs

  5. Whole-body 137Cs and 137Cs levels in the Greek population following the 1986 Chernobyl accident

    One of the consequences of the reactor accident at Chernobyl was the contamination of foodstuffs with 134Cs and 137Cs. Whole-body measurements were carried out over a four year period to determine the committed effective dose to the Greek population from internal contamination with 134Cs and 137Cs. The mean 50 year committed effective dose in residents of Ioannina was found to be 495 μSv for men, 330 μSv for women and 300 μSv for children. Measurements on subjects living in other parts of Greece showed that the average level of internal contamination over the country was about 10% higher than Ioannina, resulting in a 4.5 kSv collective effective dose to the Greek population. (author)

  6. Dissolution behavior of 137Cs absorbed on the green tea leaves

    The green tea leaf was dipped in the 137CsCl solution to elucidate the dissolution behavior of 137Cs. The IP observation showed that 137Cs was not uniformly adsorbed on the tea leaf, even if the tea leaf was dipped in the homogeneous solution. The activation energy of 137Cs dissolution was estimated to be 0.045 eV, indicating that most of 137Cs would exist as the adsorbed state. The dissolution behaviors as a function of cesium and potassium concentrations and pH, were also studied. (author)

  7. Dissolution behavior of 137Cs absorbed on the green tea leaves

    The green tea leaves was dipped in the 137CsCl solution to elucidate the dissolution behavior of 137Cs contaminated on the green tea leaves. It was found that the amount of 137Cs dissolved into tea water was controlled by the temperature of water, and the activation energy of 137Cs dissolution was estimated to be 0.045 eV, indicating that most of 137Cs would exist as the adsorbed state. In addition, the dissolution behavior was controlled by the concentration of stable Cs dissolved in water, although no large correlation with pH was observed. (author)

  8. The Role of Prussian Blue in Eliminating the Compositional Effects of 137Cs Internal Contamination

    Seventy male albino rats of two ages: growing (2-months age, 102 + 10 g /rat) and adults (4- months age, 280 + 15 g / rat) were used in this study. The rats were fed on a balanced diet (21% crude proteins, 3% crude fats and 4% crude fibers). The treatments of oral administration of a single dose (3700 Bq/growing rat and 7400 Bq/adult rat) of 137Cs (137Cs Cl salt) and prussian blue (PB, 300 mg/kg body weight/day for 60 days) were as the following combinations: [1] without 137Cs or PB, [2] 137Cs only, [3] PB only, [4] PB one day before 137Cs, [5] PB immediately after 137Cs, [6] PB one day after 137Cs, and [7] PB one week after 137Cs. All of body weight, total body water (TBW), fat-free body (FFB), total body fat (TBF), fat-free dry body (FFDB), total body protein (TBP), and total body ash (TBA). The data revealed that: adult rats had a significant (P137Cs treatment caused decreases in final body weight; % change of body weight, TBW, FFB, FFDB, TBP, TBA. In both growing and adult rats, PB administration, only before or at the same time of irradiation, could eliminate the effects of 137Cs-gamma irradiation on : final body weight, % change in body weight, FFB, FFDB, TBP. However, PB administration, one or seven days post treatment, eliminated 137Cs treatments effects on TBF

  9. Relationship between 137Cs concentration and cultivated history on loessial hillslopes

    There are close linkages between soil loss degree and soil disturbance degree by human. So it is a key problem to know that how human activity affects soil loss. To analyse the correlation of 137Cs loss degree with hillslopes' cultivated histories, the concentrations of 137Cs on different kinds of loessial hillslopes with different cultivated histories, abandoned ages and different patterns of reforestation are studied. The result shows that there is a linear relationship among 137Cs areal concentrations, cultivation ages and slope gradients. the regressive equation is as follows: X=2356.79-22.77 t-35.53 S. Variant coefficient of 137Cs areal concentration is 80.11% among hillslopes with different abandonment ages. It is also deduced that 137Cs areal concentration is affected primarily by abandonment ages of hillslopes. The 137Cs loss rates of hillslopes with different vegetation restoration manners show significant differences, as a whole, autogenic restoration 137Cs area concentrations on hillslopes. (authors)

  10. Monitoring of Chernobyl fallout 137Cs in semi-natural coniferous forest of central Sweden

    Monitoring the behaviour of 137Cs in semi-natural coniferous forest ecosystem of central Sweden was investigated between 1990 and 1994. Results demonstrated that soil in the area of study is thin layer characterised with high organic matter fraction and acidic pH. Most of Chernobyl fallout deposited 137Cs retained in the upper 5 cm with venial migration into deeper layers of soil profile The activity concentration of 137Cs in the dominant plants showed some variation, which presumed to be due to high variations in the different soil parameters and species-specificity of plants in 137Cs uptake. Fractionation of soil bound 137Cs using sequential extracted procedure predicted that easily extractable 137Cs fraction that includes water soluble and NH4OAc exchangeable comprises ∼25% of total soil radiocaesium inventory in the upper 5 cm layer of forest soil. These fractions, represent the soil mobile 137Cs in the forest ecosystem. About 37% of total forest soil 137Cs inventory could be accounted for soil organically bound 137Cs that include oxidizable and acid digestible organic matter. These fractions require a long term big-degradation process by soil micro-organisms, before becoming available for plant uptake. More over a substantial fraction Of 137Cs was firmly bound onto soil compartments of organic and/or mineral nature as a residual (36%). This means that binding processes of 137Cs onto humic forest soil with high fraction of organic matter and acidic reaction is time dependent. The most distinguished soil parameters that might influenced 137Cs transfer to and/or uptake by natural plants in the area of study were soil OM%, and soil pH. Soil biological activity might also be considered, (although it was not determined in this study). The long term 137Cs availability in this type of forest soil must be related to the organically bound 137Cs fractions. (author)

  11. Fukushima 137Cs at the base of planktonic food webs off Japan

    Baumann, Z.; Fisher, N. S.; Gobler, C. J.; Buesseler, K. O.; George, J. A.; Breier, C. F.; Nishikawa, J.

    2015-12-01

    The potential bioaccumulation of 137Cs in marine food webs off Japan became a concern following the release of radioactive contaminants from the damaged Fukushima nuclear power plant into the coastal ocean. Previous studies suggest that 137Cs activities increase with trophic level in pelagic food webs, however, the bioaccumulation of 137Cs from seawater to primary producers, to zooplankton has not been evaluated in the field. Since phytoplankton are frequently the largest component of suspended particulate matter (SPM) we used SPM concentrations and particle-associated 137Cs to understand bioaccumulation of 137Cs in through trophic pathways in the field. We determined particle-associated 137Cs for samples collected at 20 m depth from six stations off Japan three months after the initial release from the Fukushima nuclear power plant. At 20 m SPM ranged from 0.65 to 1.60 mg L-1 and rapidly declined with depth. The ratios of particulate organic carbon to chlorophyll a suggested that phytoplankton comprised much of the SPM in these samples. 137Cs activities on particles accounted for on average 0.04% of the total 137Cs in seawater samples, and measured concentration factors of 137Cs on small suspended particles were comparatively low (∼102). However, when 137Cs in crustacean zooplankton was derived based only on modeling dietary 137Cs uptake, we found predicted and measured 137Cs concentrations in good agreement. We therefore postulate the possibility that the dietary route of 137Cs bioaccumulation (i.e., phytoplankton ingestion) could be largely responsible for the measured levels in the copepod-dominated (%) zooplankton assemblages in Japanese coastal waters. Finally, our data did not support the notion that zooplankton grazing on phytoplankton results in a biomagnification of 137Cs.

  12. Root endophytic bacteria of a (137)Cs and Mn accumulator plant, Eleutherococcus sciadophylloides, increase (137)Cs and Mn desorption in the soil.

    Yamaji, Keiko; Nagata, Satoshi; Haruma, Toshikatsu; Ohnuki, Toshihiko; Kozaki, Tamotsu; Watanabe, Naoko; Nanba, Kenji

    2016-03-01

    We found that root endophytes of (137)Cs accumulator plant produce siderophores, resulting in the desorption of (137)Cs from the contaminated soil collected at Fukushima, Japan. We selected an endemic Japanese deciduous tree, Eleutherococcus sciadophylloides (Franch. et Sav), that accumulates high concentrations of (137)Cs and Mn. Root endophytic bacteria were isolated from E. sciadophylloides and microbial siderophore production was evaluated via chrome azurol S (CAS) Fe and CAS Al assays. Of the 463 strains that we isolated, 107 (23.1%) produced the siderophores. Using eight strains that showed high siderophore production in our assays, we examined desorption of (137)Cs, Mn, Fe and Al by the bacterial culture filtrates from (137)Cs-contaminated soil after decomposing the soil organic matter using hydrogen peroxide. We found (137)Cs and Mn desorption concomitant with Al and Fe desorption, as well as a decrease of pH. We also detected succinic acid, a well-known siderophore, in the bacterial culture filtrates of our two root endophytic bacteria. Our results strongly suggest that the root endophytic bacteria of E. sciadophylloides produce the siderophores that enhance (137)Cs and Mn desorption in the rhizosphere, making the resulting (137)Cs and Mn ions easier for E. sciadophylloides to absorb from the rhizosphere. PMID:26760221

  13. Immobilization of 137Cs on cement-zeolite composites

    The research has been mainly concerned with the solidification of radioactive waste in cement based matrices to reduce the mobility of cesium in the solid form. Zeolite was fixed in a cement based matrix and exposed to synthetic ground water. The zeolite can replace sand materials that are used in the cement formulations. The influences of different weights of zeolite and sand on the diffusion coefficients for 137Cs were studied using the solid waste form treated in ground water. (author). 3 refs, 3 figs, 8 tabs

  14. A review: study on the behavior of 137Cs in agricultural environment of China

    In China, study on the behavior of137Cs in agricultural environment was begun in 1960. Many papers on the behavior of 137Cs in soil-plant system and the estimation of 137Cs radioactivity in soil and food were published. The absorption, accumulation and distribution of 137Cs in plant, the relationship between absorption of 137Cs by plant and contaminating way and form, the 137Cs radioactivity in soil and food and its transfer coefficient in soil-plant system, the effects of the characters of soil and plant as well as the living stages on the transfer are concerned. The results show that the average radioactivity of 137Cs in soil of China is 10.45 Bq/kg, and the deposition densities decrease with the latitude decreasing. The transfer coefficient of 137Cs from soil to the agricultural products is about 0.12∼8.19 x 10-3. The distribution of 137Cs in rice plant is in the order of the root>glume>leaf>stem>rice. The radioactivity of aerial part accumulates mainly in the glume. The countermeasures to alleviate the adverse effects of 137Cs contamination need further study

  15. 137Cs inventory in semi-isolated basins of the western South Pacific

    Yamada, M.; Wang, Z.

    2007-12-01

    The main introduction routes of 137Cs into the Pacific Ocean are worldwide global fallout from atmospheric nuclear weapons testing and close-in fallout from U. S. tests conducted on the Bikini and Enewetak Atolls. The objectives of this study are to measure the 137Cs activities in water columns of the western South Pacific Ocean and to discuss the processes controlling the 137Cs inventory. The 137Cs activities were determined for seawater samples from the East Caroline, Coral Sea, New Hebrides, South Fiji and Tasman Sea Basins of the western South Pacific Ocean. The 137Cs activities in surface waters ranged from 1.7 Bq m- 3 in the Tasman Sea Basin to 2.3 Bq m-3 in the East Caroline Basin. The latitudinal 137Cs distributions in surface waters showed the opposite trend to the expected deposition density from global fallout. The distribution profiles of 137Cs activity at these six western South Pacific Ocean stations did not differ from each other significantly. The total 137Cs inventories in the western South Pacific Ocean ranged from 850 Bq m-2 in the Coral Sea Basin to 1270 Bq m-2 in the South Fiji Basin. Higher 137Cs inventories were observed at middle latitude stations in the subtropical gyre than at low latitude stations. The 137Cs inventories were 1.9 - 4.5 times higher than that of the expected deposition density of atmospheric global fallout at the same latitude. The possible sources of excess 137Cs inventories in the western South Pacific Ocean might be attributable to both the inter-hemisphere dispersion of the atmospheric nuclear weapons testing 137Cs from the northern stratosphere to the southern one and its subsequent deposition, and water- bearing transport of 137Cs from the North Pacific Ocean to the South Pacific.

  16. {sup 137}Cs applicability to soil erosion assessment: theoretical and empirical model; Aplicabilidade do {sup 137}Cs para medir erosao do solo: modelos teoricos e empiricos

    Andrello, Avacir Casanova

    2004-02-15

    The soil erosion processes acceleration and the increase of soil erosion rates due to anthropogenic perturbation in soil-weather-vegetation equilibrium has influenced in the soil quality and environment. So, the possibility to assess the amplitude and severity of soil erosion impact on the productivity and quality of soil is important so local scale as regional and global scale. Several models have been developed to assess the soil erosion so qualitative as quantitatively. {sup 137}Cs, an anthropogenic radionuclide, have been very used to assess the superficial soil erosion process Empirical and theoretical models were developed on the basis of {sup 137} Cs redistribution as indicative of soil movement by erosive process These models incorporate many parameters that can influence in the soil erosion rates quantification by {sup 137} Cs redistribution. Statistical analysis was realized on the models recommended by IAEA to determinate the influence that each parameter generates in results of the soil redistribution. It was verified that the most important parameter is the {sup 137} Cs redistribution, indicating the necessity of a good determination in the {sup 137} Cs inventory values with a minimum deviation associated with these values. After this, it was associated a 10% deviation in the reference value of {sup 137} Cs inventory and the 5% in the {sup 137} Cs inventory of the sample and was determinate the deviation in results of the soil redistribution calculated by models. The results of soil redistribution was compared to verify if there was difference between the models, but there was not difference in the results determinate by models, unless above 70% of {sup 137} Cs loss. Analyzing three native forests and an area of the undisturbed pasture in the Londrina region, can be verified that the {sup 137} Cs spatial variability in local scale was 15%. Comparing the {sup 137} Cs inventory values determinate in the three native forest with the {sup 137} Cs inventory

  17. Reconstruction of 137Cs activity in the ocean following the Fukushima Daiichi Nuclear Power Plant Accident

    Tsumune, Daisuke; Aoyama, Michio; Tsubono, Takaki; Tateda, Yutaka; Misumi, Kazuhiro; Hayami, Hiroshi; Toyoda, Yasuhiro; Maeda, Yoshiaki; Yoshida, Yoshikatsu; Uematsu, Mitsuo

    2014-05-01

    A series of accidents at the Fukushima Dai-ichi Nuclear Power Plant following the earthquake and tsunami of 11 March 2011 resulted in the release of radioactive materials to the ocean by two major pathways, direct release from the accident site and atmospheric deposition. We reconstructed spatiotemporal variability of 137Cs activity in the ocean by the comparison model simulations and observed data. We employed a regional scale and the North Pacific scale oceanic dispersion models, an atmospheric transport model, a sediment transport model, a dynamic biological compartment model for marine biota and river runoff model to investigate the oceanic contamination. Direct releases of 137Cs were estimated for more than 2 years after the accident by comparing simulated results and observed activities very close to the site. The estimated total amounts of directly released 137Cs was 3.6±0.7 PBq. Directly release rate of 137Cs decreased exponentially with time by the end of December 2012 and then, was almost constant. The daily release rate of 137Cs was estimated to be 3.0 x 1010 Bq day-1 by the end of September 2013. The activity of directly released 137Cs was detectable only in the coastal zone after December 2012. Simulated 137Cs activities attributable to direct release were in good agreement with observed activities, a result that implies the estimated direct release rate was reasonable, while simulated 137Cs activities attributable to atmospheric deposition were low compared to measured activities. The rate of atmospheric deposition onto the ocean was underestimated because of a lack of measurements of dose rate and air activity of 137Cs over the ocean when atmospheric deposition rates were being estimated. Observed 137Cs activities attributable to atmospheric deposition in the ocean helped to improve the accuracy of simulated atmospheric deposition rates. Although there is no observed data of 137Cs activity in the ocean from 11 to 21 March 2011, observed data of

  18. Determination of Corrections in the Absolute Measurement of 137Cs

    A method, of determining corrections in absolute measurements of 137Cs by 4π proportional counter is described. The correction for self-absorption of 137Cs beta particles from sources formed by vacuum deposition of CsCl on standard carrier films was determined. These samples, which had negligible self-absorption, were measured by 4π counter. The radioactive substance on the film was then dissolved, and by the addition of carrier was converted to a form similar to that of sources usually used for absolute measurement. The correction determined for self-absorption was higher than the value expected from comparison with other radionuclides having near Eβmax. The correction for internal conversion coefficient and gamma efficiency of the beta detector was determined with 137mBa samples. Barium was separated as BaSO4 precipitate and deposited on a standard carrier film used for absolute measurement with a layer thickness of about 1 mg/cm2. These samples were simultaneously measured by means of a 4π beta proportional counter and a Nal(Tl) scintillation counter. From corresponding counting rates in both counters, and from both known efficiencies, the value for a correction appropriate to one disintegration of 137mBa was calculated. The values measured were used further for computation of the internal conversion coefficient and the half-life of 137'mBa, which was ascertained to be 155 ± 3 s. (author)

  19. Body burden and distribution of 137Cs in reindeer

    The whole body was collected from 6 reindeer that had been grazing contaminated pasture and from 6 reindeer that had been fed uncontaminated feed the last weeks before slaughter. The body was emptied from in-gesta and weighed. Samples were taken from skeletal muscle, kidneys, heart, liver, lungs, rumen wall, bone and blood. The total activity of 137Cs in the ingesta-free body and the activity concentration of l37Cs in the different tissues were determined. The highest acitivity concentrations of l37Cs were found in skeletal muscle and in kidneys. Activity concentrations in kidneys, heart, liver, lungs and rumen wall, relative to skeletal muscle, were lower in reindeer with decreasing radiocaesium levels, compared to reindeer with continuous intake of radiocaesium, indicating a more rapid elimination in these tissues than in muscle. The ratios between average activity concentration of 137Cs in whole body and acitivity concentration in muscle from the same animal, ranged from 0.51 to 0.62. A factor of 0.57 is suggested for calculating average body activity concentration of radiocaesium from known activity concentration in muscle

  20. Analysis of 137Cs in fission based neutron dosimetry

    137Cs analysis is based on dissolving an irradiated fission dosimeter and chemically separating the cesium from the rest of the fission material. The samples consisted of uranium and neptunium in the form of metal or oxide. The uranium samples were dissolved in nitric acid and the neptunium samples in a mixture of nitric acid and chloric acid with addition of hydrogen peroxide. Cs was precipitated into a mixture of ammonium molyndophoshate and cellulose powder. A preparate for measurement was made from the precipitate and covered with polyethen plastic. Since other fission products than cesium were precipitated as well from the more recently irradiated samples, the activity measurements could not be carried out with a NaI(Tl) cavity crystal, but had to be made with a less efficient but more selective germanium semiconductor crystal. The method is well suited for 137Cs determination, especially for older dosimeters where the more short-lived fission products have decayed. (orig.) (6 refs., 7 figs., 7 tabs.)

  1. Fractionation of 137Cs and Pu in natural peatland

    High Cs-137 concentrations in plants growing on peatland inspired us to investigate the quantity of its bioavailable fraction in natural peat. Our investigation aims to: a) estimate the quantity of bioavailable Cs-137 and Pu present in peat, b) verify the similarity of Cs-137 and K-40 behaviours, and c) perform a quantification of Cs-137 and Pu transfer from peat to plants. We analysed the vertical distribution of Cs-137 and Pu isotopes in the peat and their concentrations in plants growing on these places. Bioavailability of radionuclides was investigated by sequential extraction. Sequential analyses revealed that it was the upper layer which contained the majority of Cs-137 in an available form while deeper layers retained Cs-137 in immobile fractions. We can conclude that 18% of all Cs-137 in the peat is still bioavailable. Despite of the low quantity of bioavailable fraction of Cs-137 its transfer factor reached extremely high values. In the case of Pu, 64% of its total amount was associated with fulvic/humic acids which resulted in the high transfer factor from peat to plants. 27 years after the Chernobyl nuclear accident, the significant part of radionuclides deposited in peatland is still bioavailable. - Highlights: • Decrease of exchangeable 137Cs and its increase in residual fraction with depth. • High 137Cs transfer factor contrary to its low quantity in bioavailable fractions. • Fulvic/humic acids are a more effective carrier for Pu than for Cs

  2. The use of tree bark as long term biomonitor of (137)Cs deposition.

    Cosma, Constantin; Iurian, Andra-Rada; Incze, Reka; Kovacs, Tibor; Žunić, Zora S

    2016-03-01

    Airborne (137)Cs originated from the nuclear tests in the atmosphere and from the Chernobyl nuclear disaster was retained by the trees biomass and nowadays it can still be found in various concentrations in tree barks from Romania and other European countries. This study brings the first results of (137)Cs presence in tree bark from Romania on different considerations: (i) data dispersion in spruce and oak bark from NW, SW and central Romania, and the spatial variability of (137)Cs within oak and spruce bark from a natural protected forest area from Balvanyos area (Covasna County), known to be highly affected by the Chernobyl nuclear release; (ii) comparison of (137)Cs content in different tree bark species (oak, spruce, poplar and cherry); (iii) differences in (137)Cs concentrations with the bark depth layers and around the tree trunk; and (iv) comparison of mean (137)Cs values in spruce/oak bark from Romania with data from other European countries. PMID:26771244

  3. Distribution of Na, K, Rb, Cs, and 137Cs in some Austrian higher fungi

    The level of 137Cs in 28 species of mushroom collected and analyzed between 1986 and 1992, after the Chernobyl accident, are reported. Xerocomus badius was found to accumulate 137Cs (the median value of 58 samples is 3667 Bq/kg). The 137Cs content of Rozites caperata, Scleroderma vulgare, and Tylopilus felleus exceeded 600 Bq/kg. Some of these samples collected in August 1992 were investigated for their 134Cs and 137Cs content as well as their Na, K, Rb, and Cs levels by applying instrumental neutron activation analysis (INAA). The results show a high correlation coefficient (0.80) between the contents of 137Cs and Na, but none between 137Cs and K

  4. Uptake of 137Cs in cultured fresh water fish (Cyprinus carpio): physiological and histological effects

    An experiment was conducted in fresh-water fish (Cyprinus carpio) cultured, in small water tanks, artificially contaminated with radioactive 137Cs (3000 Bq/1) to determine the uptake of 137Cs and its physiological and histological effects in different fish organs. It was found that 137Cs was located in muscular tissues, gills, head muscles, liver and kidneys. Moderate amounts were found in spleen, eyes, gonads, intestine and urinary bladder. It seems that sorption was of much less importance than ingestion in the uptake of 137Cs. The histological examination in musculature tissue, revealed an acute hyperemia with focal haemorrages which may be due to allergic effects of 137Cs. Hyperemia and focal fatty degeneration of hepatic cells was also noted in the liver which may be due to toxic effects of 137Cs. Diffused hyperemia has also occurred in the brain and focal degeneration of epithelial cells of renal tubules. (Author)

  5. Inferring the chemical form of 137Cs deposited by the Fukushima Dai-ichi Nuclear Power Plant accident by measuring (137)Cs incorporated into needle leaves and male cones of Japanese cedar trees.

    Kanasashi, Tsutomu; Takenaka, Chisato; Sugiura, Yuki

    2016-05-15

    We hypothesized that the water-soluble (ionic) and water-insoluble (stable) radiocesium from the initial fallout of the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident was distributed in various proportions in the surrounding areas and that this distribution was reflected in the trees that suffered deposition from the initial fallout. This study attempted to evaluate local variations in the chemical form of (137)Cs derived from the initial fallout of the FDNPP accident and whether its chemical form affected the radiocesium concentration in the tissues currently growing in trees, even after the initial fallout ceased. For these estimations, the ratio between the (137)Cs concentration in Cryptomeria japonica needle leaves in the tree crown, which existed before the FDNPP accident and subsequently directly exposed to the initial fallout ((137)Cs pre-accident N), and the amount of (137)Cs in the initial fallout itself ((137)Cs fallout) was determined ((137)Cs pre-accident N/(137)Cs fallout) at 66 sites. In addition, the (137)Cs ratios between the male cones produced in 2012 ((137)Cs male cone) and needle leaves that had elongated in the spring of 2011 ((137)Cs 2011N) was determined at 82 sites ((137)Cs male cone/(137) Cs 2011N). Most of the sites with lower (137)Cs pre-accident N /(137)Cs fallout ratios were distributed in eastern Fukushima, relatively close to the Pacific Ocean coastline. Lower (137)Cs pre-accident N/(137)Cs fallout and higher (137)Cs malecone/(137)Cs 2011N were found to be associated with higher proportions of (137)Cs in ionic forms. These observations are consistent with the hypothesis, and likely reflect regional variations in the chemical form of the deposited radiocesium. PMID:26990074

  6. 137Cs and 90Sr concentration in the Baltic Sea coastal zone

    The results of the 137Cs and 90Sr concentration measurements in the Baltic Sea coastal zone (near the settlement of Juodkrante) are presented. The concentration variation range is from 0.3 to 1.2 nCi/m3. The maximum 137Cs concentration is observed in autumn and the minimum one - in summer. 137Cs/90Sr concentration ratio in summer and autumn of 1977 was over 1, and that of April 1976 was less than 0.5

  7. The organic matter of forest soil as an incorporator of 137Cs

    The decomposition of a forest litter in forest ecosystems contaminated by radionuclides is accompanied by the accumulation of organomineral compounds associated with 137Cs in deeper soil layers. The highest level of 13Cs in the upper organic-reach soil layers was found in the insoluble fraction of organic matter, hemicellulose and cellulose. Due to a high level of the 137Cs accumulation in a forest litter, the last generates a substantial part of the 137Cs background in forests

  8. Possibility of soil clean-up from 137Cs in coast part of drainage system

    The net of drainage canals is used for the collection of the surface ground waters on the radioactive waste storage at the MosNPO RADON. The soils of the drainage system were contaminated by 137-Cs migrating in the direction of the common flow. A unique technology was elaborated permitting to extract 137Cs from soil 90% and to concentrate 137-Cs on the selective inorganic sorbent (nickel ferrocyanide). This technology combines electrokinetics, membrane and sorption methods of the contaminated media cleaning

  9. {sup 137}Cs contaminated waste disposal in cement factory: Environmental problems; Smaltimento di scorie contaminate da {sup 137}Cs in un cementificio: problematiche ambientali

    Bianchi, D.; Cammarata, E.; Marzolla, N.; Rabbia, G.; Vescovi, A.; Astori, E. [Alessandria USL 20, Alessandria (Italy). Lab. di sanita` pubblica; Cagliero, S. [Cuneo USL 15, Cuneo (Italy). Lab. di sanita` pubblica

    1995-09-01

    In the course of utilization (May-June `91) of aluminum slags polluted by {sup 137}Cs at the cement factory Presacementi in Robilante (Cuneo, Italy) and during the following months, samples were taken in particular points of the plant, at fixed frequencies. Samples were analyzed to determine {sup 137}Cs concentration. Collected data were used to study the behaviour of the element throughout the process. Emissions and ground level air concentrations were estimated from the available data. Contamination of the manufactured cement were monitored until negligible values of {sup 137}Cs concentration were attained.

  10. Rates of leaching of 137Cs and potassium from different plant litters

    Mature plants of Calluna vulgaris, Trifolium repens and Agrostis capillaris were labelled with 137Cs by uptake through the roots. Shoot material was allowed to dry to give plant litters adequately labelled for leaching experiments, using microcosms subjected to a number of applied treatments. Measurements were made of 137Cs activity, potassium content and pH on the leachates from each microcosm obtained every 2 weeks over a 3-month period. The respiration rate of the litter was also measured to give an index of microbial activity. At the end of the experiment, 137Cs and K contents of the residual litter were measured. Generally, the rate of release of 137Cs from Calluna litter was slower than that from Trifolium or Agrostis. After 3 months, the loss of 137Cs from Calluna litter had stabilised at about 30-40% of the original. Trifolium had lost 60% of the initial 137Cs over the same period, whilst Agrostis had lost about 70%. Repeated drying and rewetting treatment, compared to a continuous moistened state, resulted in the stabilisation of 137Cs within Trifolium and Agrostis litters. In Agrostis and Trifolium, the release of potassium was greater and more rapid than the release of 137Cs, with only 10% of the original K remaining in the litter after 2 months. In Calluna, the release of K resembled the release of 137Cs more closely. (author)

  11. 137Cs contamination of Techa river flood plain in Brodokalmak settlement

    137Cs contamination of the Techa river flood plain inside the Brodokalmak settlement has been mapped. The collimated scintillated detector technique was used for 137Cs deposit measurements. The 137Cs contamination is very heterogeneous. A comparison of this technique with the traditional sample method was performed at selected locations. The sampling data are in good agreement with in-situ data. Soil surface activity of 90Sr was determined from the samples. It was shown that 137Cs contamination correlates with 90Sr contamination within the flood plain of the settlement

  12. Effect of arbuscular mycorrhizal (AM) fungi on 137Cs uptake by plants grown on different soils

    The potential use of mycorrhiza as a bioremediation agent for soils contaminated by radiocesium was evaluated in a greenhouse experiment. The uptake of 137Cs by cucumber, perennial ryegrass, and sunflower after inoculation with a commercial arbuscular mycorrhizal (AM) product in soils contaminated with 137Cs was investigated, with non-mycorrhizal quinoa included as a “reference” plant. The effect of cucumber and ryegrass inoculation with AM fungi on 137Cs uptake was inconsistent. The effect of AM fungi was most pronounced in sunflower: both plant biomass and 137Cs uptake increased on loamy sand and loamy soils. The total 137Cs activity accumulated within AM host sunflower on loamy sand and loamy soils was 2.4 and 3.2-fold higher than in non-inoculated plants. Although the enhanced uptake of 137Cs by quinoa plants on loamy soil inoculated by the AM fungi was observed, the infection of the fungi to the plants was not confirmed. - Highlights: ► Effect of soil inoculation on 137Cs uptake by crops was studied in greenhouse. ► 137Cs uptake by inoculated sunflower plants was most pronounced. ► The higher 137Cs uptake by inoculated sunflower due to presence of mycorrhiza. ► Studies suggest potential for use of mycorrhiza on contaminated sites.

  13. Effect of application timing of potassium fertilizer on root uptake of 137Cs in brown rice

    We investigated the optimal timing and quantity of K to reduce radiocesium in brown rice. The concentration of 137Cs in brown rice was reduced from 32 Bq kg-1 without K fertilizer to 2.0 Bq kg-1 with 16 g m-2 of basal K. The concentration of exchangeable 137Cs in the soil decreased from 234 to 25 Bq kg-1 with increasing application of K fertilizer from 0 to 57 g m-2. Hence, heavy application of K fertilizer in the early growing period can decrease the uptake of 137Cs by rice plants and the concentration of exchangeable 137Cs in the soil. (author)

  14. Concentrations of 137Cs in soils and selected forest plants in Taiwan

    Fallout 137Cs activities in soils and trees were measured from samples taken in mountainous areas and along three cross-island highways in Taiwan. Typical concentration in near-surface samples is about 5 Bq kg-1 depending on soil density. No correlation was found between the concentrations of 137Cs and stable elements in soils. Mechanical disturbance and soil density were identified as major causes for redistribution of 137Cs in both forest soils and trees. The transfer coefficient of 137Cs from soil to bastard banian estimated is 0.23. (author)

  15. 137Cs in carpets of the forest moss Pleurozium schreberi, 1961-1973

    Accumulation, retention and internal cycling of the fallout radionuclide 137Cs (physical half-life=30.2 a) were studied in forest moss Pleurozium schreberi (Brid.) Mitt. collected in southern Sweden during the period 1961-1973. The highest 137Cs concentrations occurred in the green top parts of the living moss. A major part of the deposited 137Cs is available for transport from the dying to growing parts of the moss.Elimination of 137Cs from living moss, as well as from dead moss, throughout 1968-1973, can be characterized by the same mean residence time (4+-1 a). 137Cs and naturally occurring stable K show different behaviour in the moss, so that the 137Cs/K ratio is higher by a factor of approximately 2 in the dead parts of the moss than in the living parts. The vertical distribution of 137Cs in the moss-covered ground has been described theoretically. Relative penetration of 137Cs is about 5 times higher in ground covered by moss-carpets than in ground covered by lichen-carpets. Throughout 1969-1973, the total amount of 137Cs retained in the moss-carpet was 64.2+-2.2 nCi.m-2. (author)

  16. Transfer of 137Cs from soil to plants in a wet montane forest in subtropical Taiwan

    The distribution of 137Cs in an undisturbed, multistoried, subtropical wet montane forest ecosystem surrounding Yuanyang Lake (lake surface level ca. 1670 m, in northeastern Taiwan), was investigated. The mossy forest here represents a currently-rare perhumid temperate environment in subtropical region. The radioactivity concentration of 137Cs was determined by γ-spectroscopy with a Ge(Li) detector. Although the soil is extremely acidic (pH 3.3 to 3.6) and the rainfall is high, 137Cs is evidently retained in the organic layer. The radioactivity concentration of 137Cs in surface soil ranges from 28 to 71 Bq x kg-1. The concentrations of 137Cs in the ground moss layer and litter were much lower than that in the soil organic layer; this suggests that 137Cs detected is not from the newly deposited radioactive fallout. The radioactivity concentration and transfer factor (TF) of 137Cs varied with plant species. Shrubs and ferns have higher values than a coniferous tree (Taiwan cedar). The TF in this ecosystem is as high as 0.21 to 1.88. The high values of TF is attributed to the abundance of the organic matter in the forest soils. The rapid recycling of 137Cs through the soil-plant system of this undisturbed multistoried ecosystem suggests the existence of an internal cycling that help the accumulation of 137Cs in this ecosystem. (author)

  17. 137Cs radiation burden on children from a highly contaminated area of Belarus

    The radiation burden from 137Cs sources on 22 children from a small Byelorussian village was studied from 1992 to 1994. Foodstuff, whole body burden and urinary excretion of 137Cs were measured, intake rates, biological half-lives and doses were calculated. The median value for the 137Cs whole body incorporation level was found to be 124 Bq, the biological half life was calculated as 68 d for girls and 50 d for boys. The internal dose caused by 137Cs was found to be negligible in comparison to that from external sources. No deviation from normal values could be shown in simultaneously studied clinico-chemical parameters

  18. The effect of fertilizer applications on 137Cs uptake by different plant species and vegetation types

    A trial carried out in a greenhouse over a two-year period is discussed. The effects on 137Cs concentration in plants, roots and soil have been investigated versus the grassland species composition (legume, grass and mixture) and eight combinations of mineral fertilizers (NPK). The results indicate: (a) the effect of K fertilizer in reducing 137Cs plant absorption; (b) the effect of N fertilizer in favouring grass growth and radiocaesium absorption; (c) for all fertilizer combinations, a higher 137Cs storage in the root system of the legumes and a lower 137Cs absorption in the plants. (author)

  19. The 137Cs activity and its geographical significance in terrestrial ecosystem of Great Wall Station, Antarctica

    2000-01-01

    The radioactive isotope——137 Cs is one of the important tracers for studying the physical processes and the human impacts on the environment. Based on the investigation results of the terrestrial ecosystem of Great Wall Station, Antarctica, it was shown that there are some artificial radioactive elements——137Cs in Antarctic terrestrial ecosystem. The sequence of 137Cs specific activities is as follows: crustaceous lichen>fruticose lichen>surface-moss>surface soil, and the crustaceous lichen is one of the most sensitive ways in monitoring the impact of the long-term diffusion of 137Cs on the environment.

  20. 137Cs use in estimating soil erosion: 30 years of research

    Significant amounts of fallout 137Cs from nuclear weapons tests were introduced to the landscape during the 1950s and 1960s. Once 137Cs reaches the soil surface it is strongly and quickly adsorbed by clay particles, and is essentially nonexchangeable in most environments. Thus, 137Cs becomes and effective tracer of the movement of soil particles across the landscape. Over the past 30 years, researchers have shown that 137Cs can be used to study soil movement. Early work used empirical relationships between soil loss and 137Cs loss to estimate erosion. This was followed by the development of proportional and theoretical models to relate 137Cs movement and soil redistribution. Most of the problems related to the 137Cs technique are the same as those encountered with other techniques (i.e., sampling, measurement). The 137Cs technique can make actual measurements of soil loss and redeposition in fields, fostering the formulation of better plans to conserve the quality of the landscape. This paper reviews the development of the 137Cs technique to show how it can be used to understand erosion and soil movement on the landscape. (author)

  1. Arbuscular mycorrhizal fungi mediated uptake of {sup 137}Cs in leek and ryegrass

    Rosen, Klas; Weiliang, Zhong; Maertensson, Anna [Department of Soil Sciences, Swedish University of Agricultural Sciences P.O. Box 7014, SE-750 07 Uppsala (Sweden)

    2005-02-15

    In a first experiment of soil contaminated with {sup 137}Cs, inoculation with a mixture of arbuscular mycorrhizae enhanced the uptake of {sup 137}Cs by leek under greenhouse conditions, while no effect on the uptake by ryegrass was observed. The mycorrhizal infection frequency in leek was independent of whether the {sup 137}Cs-contaminated soil was inoculated with mycorrhizal spores or not. The lack of mycorrhizae-mediated uptake of {sup 137}Cs in ryegrass could be due to the high root density, which was about four times that of leek, or due to a less well functioning mycorrhizal symbiosis than of leek. In a second experiment, ryegrass was grown for a period of four cuts. Additions of fungi enhanced {sup 137}Cs uptake of all harvests, improved dry weight production in the first cut, and also improved the mycorrhizal infection frequencies in the roots. No differences were obtained between the two fungal inoculums investigated with respect to biomass production or {sup 137}Cs uptake, but root colonization differed. We conclude that, under certain circumstances, mycorrhizae affect plant uptake of {sup 137}Cs. There may be a potential for selecting fungal strains that stimulate {sup 137}Cs accumulation in crops. The use of ryegrass seems to be rather ineffective for remediation of {sup 137}Cs-contaminated soil.

  2. Uptake and translocation of {sup 137}Cs by Houttuynia cordata (in water culture)

    Kimura, Shojiro; Yamaoki, Rumi [Osaka Univ. of Pharmaceutical Sciences, Takatsuki (Japan)

    2001-08-01

    The water culture experiment of Houttuynia cordata of the medicinal plant was carried out, and basic study on {sup 137}Cs accumulation characteristic and internal circulation in H. cordata in the fruiting stage was investigated since the flowering season. H. cordata accumulated 80% of {sup 137}Cs absorbed unlike K to the root, rhizome, terminal bud of the underground part for the rhizome reproduction. {sup 137}Cs content to the young leaf, spike, involucre increased in the flowering season. Thereafter, {sup 137}Cs was recirculated to the developing organs in second generations such as the rhizome and bud. (author)

  3. Uptake and translocation of 137Cs by Houttuynia cordata (in water culture)

    The water culture experiment of Houttuynia cordata of the medicinal plant was carried out, and basic study on 137Cs accumulation characteristic and internal circulation in H. cordata in the fruiting stage was investigated since the flowering season. H. cordata accumulated 80% of 137Cs absorbed unlike K to the root, rhizome, terminal bud of the underground part for the rhizome reproduction. 137Cs content to the young leaf, spike, involucre increased in the flowering season. Thereafter, 137Cs was recirculated to the developing organs in second generations such as the rhizome and bud. (author)

  4. Long-term behaviours of 137Cs in simulated crop fields

    In order to understand the long-term behaviour of 137Cs in crop fields, root uptake and underground distribution of 137Cs were investigated through a greenhouse experiment where 137Cs was mixed with topsoil in culture boxes and rice, soybean and Chinese cabbage were grown for 4 years. Soil-to-plant transfer factors of 137Cs for hulled rice, rice straw, soybean seed and Chinese cabbage reduced by factors of 3-10 depending on crops, and leaching of 137Cs from the rice culture box decreased by a factor of about 7, in 3 years. The 137Cs transfer factor for soybean seed were several times higher than that for hulled rice. The amount of 137Cs leaching during the growing season of rice was as low as 0.025% of applied activity even in the 1st year. The uniformity of 137Cs distribution in topsoil tended to improve year by year. The present results may be utilized as basic information for the environmental impact assessment and the counter-measure decision when crop fields are contaminated with 137Cs

  5. Soil-dependent uptake of 137Cs by mushrooms: experimental study in the Chernobyl accident areas

    The influence of agrochemical properties of forest soils and growth conditions on 137Cs aggregated transfer factors from soil to different species of forest mushrooms have been analysed. Statistically significant correlations between 137Cs soil to mushroom aggregated transfer factors and agrochemical soil properties have been revealed. The experimental data show that 137Cs aggregated transfer factors depend on the mushroom's trophic group, biological family, genus and species. They also strongly depend on forest soil properties and their values can be estimated with the use of multiple regression equations constructed from agrochemical soil parameters which most closely correlate with the 137Cs transfer parameters for particular mushroom groups

  6. Distribution characteristics of 137Cs in soil profiles under different land uses and its implication

    This paper presents a study of the distribution of 137Cs in soils under three different land uses in a semiarid watershed. The results showed the average inventory of 137Cs in the cultivated land, woodland and grassland was 888, 1489 and 1650 Bq/m2, respectively. The pattern of depth distribution of 137Cs in the soil profiles with cultivated land, woodland and grassland was disturbed, eroding and aggrading, and normal profiles, respectively. The coefficient of variation of 137Cs inventory varied from 8.9 to 38.8 % for different land uses. (author)

  7. Arbuscular mycorrhizal fungi mediated uptake of 137Cs in leek and ryegrass

    In a first experiment of soil contaminated with 137Cs, inoculation with a mixture of arbuscular mycorrhizae enhanced the uptake of 137Cs by leek under greenhouse conditions, while no effect on the uptake by ryegrass was observed. The mycorrhizal infection frequency in leek was independent of whether the 137Cs-contaminated soil was inoculated with mycorrhizal spores or not. The lack of mycorrhizae-mediated uptake of 137Cs in ryegrass could be due to the high root density, which was about four times that of leek, or due to a less well functioning mycorrhizal symbiosis than of leek. In a second experiment, ryegrass was grown for a period of four cuts. Additions of fungi enhanced 137Cs uptake of all harvests, improved dry weight production in the first cut, and also improved the mycorrhizal infection frequencies in the roots. No differences were obtained between the two fungal inoculums investigated with respect to biomass production or 137Cs uptake, but root colonization differed. We conclude that, under certain circumstances, mycorrhizae affect plant uptake of 137Cs. There may be a potential for selecting fungal strains that stimulate 137Cs accumulation in crops. The use of ryegrass seems to be rather ineffective for remediation of 137Cs-contaminated soil

  8. Some biological factors related to the 137Cs concentration of marine organisms

    Marine Ecology Research Institute has been studying the factors controlling the concentration of radionuclides in marine biota. Weight of fish seemed to be an important factor controlling the concentration of 137Cs because of the good correlation observed between the weight and the concentration of 137Cs. Food habits also seemed to be an important factor because fishes in higher trophic levels tended to indicate higher concentration factors and a positive correlation was observed between the concentrations of predator fishes and those of the foodstuff. Gender could be another factor controlling the concentration of 137Cs because the difference of 137Cs between gender was observed in rockfish and marbled sole. (author)

  9. Uptake of {sup 137}Cs by fresh water fish

    Man, C.K.; Kwok, Y.H

    2000-02-01

    The uptake and discharge rates of {sup 137}Cs by fresh water fish at different radionuclide concentrations have been studied. A dual compartment model was used to fit the experimental data. The discharge rates have been found to be negligible for the duration of the experiment of 10 days. The uptake rates were independent of radionuclide concentrations for a particular type of fresh water fish and were different for different types of fish. The uptake rates of carp, tilapia and snakehead were 1.58, 1.66 and 2.23, in unit of 10{sup -6} h{sup -1}, respectively. It was also estimated that the consumption of fresh water fish, even if the water were contaminated as much as that in the Chernobyl accident, leads to negligible latent cancer fatality to the Hong Kong population.

  10. Uptake of 137Cs by fresh water fish

    The uptake and discharge rates of 137Cs by fresh water fish at different radionuclide concentrations have been studied. A dual compartment model was used to fit the experimental data. The discharge rates have been found to be negligible for the duration of the experiment of 10 days. The uptake rates were independent of radionuclide concentrations for a particular type of fresh water fish and were different for different types of fish. The uptake rates of carp, tilapia and snakehead were 1.58, 1.66 and 2.23, in unit of 10-6 h-1, respectively. It was also estimated that the consumption of fresh water fish, even if the water were contaminated as much as that in the Chernobyl accident, leads to negligible latent cancer fatality to the Hong Kong population

  11. 137Cs leaching through cement-radwaste matrix

    To assess the safety for disposal of radioactive mortar-waste composition, the leaching of 137Cs from a waste composite into a surrounding fluid has been studied. Leaching tests were carried out in accordance with a method recommended by IAEA. Determination of retardation factors, KF and coefficients of distribution, kd, using a simplified mathematical model for analyzing the migration of radionuclides, has been developed. In our experiment we have achieved the lowest leaching values after 120, days for each samples. Results presented in this paper are examples of results obtained in a 30 year mortar and concrete testing project, which will influence the design of the engineered trenches system for a future central Serbian radioactive waste storage center. (author)

  12. 137Cs penetration through concrete in radioactive waste management

    To assess the safety for disposal of radioactive waste-concrete composition, the leaching of 137Cs from a waste composite into a surrounding fluid has been studied. Leaching tests were carried out in accordance with a method recommended by IAEA. Determination of retardation factors, KF and coefficients of distribution, kd, using a simplified mathematical model for analyzing the migration of radionuclides, has been developed. In our experiment we have achieved the lowest leaching values after 60 days in samples. Results presented in this paper are examples of results obtained in a 20 year mortar and concrete testing project, which will influence the design of the engineered trenches system for a future central Serbian radioactive waste storage center. (author)

  13. Recent 137Cs deposition in sediments of Admiralty Bay, Antarctica

    Cesium-137, radium-226 and lead-210 profiles of a 25 cm sediment core give an indication of recent changes in land-ocean interactions at a polar coastal environment (Admiralty Bay, King George Island, Antarctica). The linear sedimentation accumulation rate at the study site calculated from the unsupported 210Pb profile was 6.7 mm/year from 1965 to 2005. A 3.5-fold increase in 137Cs concentrations was observed in the top layer of this sediment core. This sharp increase seems to indicate a recent redistribution of fallout radionuclides previously deposited on soil, vegetation and snow. These results imply enhanced land-ocean interactions at this site likely as a result of climate change. Because our results are based on a single core, additional investigations are needed to confirm our observations.

  14. Atmospheric deposition of radioactive cesium (137Cs) associated with dust events in East Asia

    Since the cessation of atmospheric nuclear testing in 1980, there has been no known serious atmospheric contamination by radioactive cesium (sup(137)Cs) apart from the Chernobyl nuclear reactor accident in 1986. There now remain only small amounts of anthropogenic radionuclides in the atmosphere that can be directly related to past testing. However, sup(137)Cs is still regularly found in atmospheric deposition samples in Japan. In this study, we analyzed sup(137)Cs monitoring data, meteorological data, and field survey results to investigate the recent transport and deposition of sup(137)Cs associated with dust phenomena. Monthly records of nationwide sup(137)Cs deposition in Japan during the 1990s show a consistent seasonal variation, with higher levels of deposition occurring in spring. In March 2002, an unexpectedly high amount of sup(137)Cs was deposited in the northwestern coastal area of Japan at the same time as an Asian dust event was observed. Analysis of land-based weather data showed that sandstorms and other dust-raising phenomena also occurred in March 2002 over areas of Mongolia and northeastern China where grassland and shrubs predominated. Furthermore, radioactivity measurements showed sup(137)Cs enrichment in the surface layer of grassland soils in the areas affected by these sandstorms. These results suggest that grasslands are potential sources of sup(137)Cs-bearing dust. Continued desertification of the East Asian continent in response to recent climate change can be expected to result in an increase in sup(137)Cs-bearing soil particles in the atmosphere, and their subsequent re-deposition in Japan. However, soil dust is also raised around Japanese monitoring sites by the strong winds that are common in Japan in spring, and this local dust might also contribute to sup(137)Cs deposition in Japan. To estimate the relative contributions of local and distant dust events to the total sup(137)Cs deposition, we monitored deposition of mineral particles

  15. Estimation of vertical migration velocity of 137Cs in the Mount IDA/Kazdagi, Turkey

    This paper presents the results obtained from a radioecological study carried out in the forest sites of Mount IDA (Kazdagi)/Edremit, Turkey. For 118 soil profiles, the depth distribution of 137Cs activity was established by fitting the experimental points to an exponential, a gaussian or a log-normal function. The relaxation lengths were in the range of 1.09–16.7 cm with a mean of 5.73 cm, showing a slow transport and a strong retention capacity of 137Cs even after the 26-y period of Chernobyl accident. From the data for the vertical distribution of 137Cs in soil profiles, the mean annual migration velocity of 137Cs was in the range of 0.11–0.62 cm year−1 with a mean of 0.30 cm year−1. Statistically significant correlations between the thickness of the humus layer and the mean annual velocity of 137Cs were found for both coniferous and mixed forest sites. The mean annual velocity of 137Cs in the forests sites with Pinus nigra var pallasiana was significantly higher than sites with Pinus brutia. External dose-rates from the 137Cs in forest soils were estimated using a conversion factor used in many studies and comprised with the external dose-rates determined according to the vertical distribution of 137Cs within the soil depth profiles. It is clearly seen that both levels and spatial distribution patterns of the external dose-rates from 137Cs were influenced considerably with the vertical migration rate and the vertical distribution of 137Cs. - Highlights: • The vertical migration of 137Cs was investigated in the forests at the Mount IDA. • The relaxation lengths of 137Cs are found in the range of 1.09–16.67 cm. • The mean annual velocity of 137Cs is found in the range of 0.11–0.62 cm year−1. • External dose-rates determined using the vertical distribution of 137Cs. • The external dose-rates were influenced with the vertical distribution of 137Cs

  16. 137Cs distribution and geochemistry of Lena River (Siberia) drainage basin lake sediments

    The Lena River is the second largest river that discharges into the Arctic Ocean. It is therefore important to determine not only the direct impact its discharge has on the 137Cs concentration of the Arctic, but also the potential its drainage basin has as a 137Cs source. 137Cs surface sediment concentrations and inventory values, which range from 4.97 to 338 Bq kg-1 and 357 to 1732 Bq m-2, respectively, were determined for the Lena River drainage basin lake samples, via gamma analysis. The average geochemical and mineralogical composition of a subset of samples was also determined using neutron activation analysis, X-ray diffraction and X-ray fluorescence spectrometry techniques. Results of these geochemical analyses allowed for the identification of key geochemical factors that influence the distribution of 137Cs in the Lena River drainage basin. 137Cs profiles indicate that Lena River drainage basin lacustrine sediments serve as a record of 137Cs fallout. Based on the downcore 137Cs, %illite, %smectite, %Al and %Mn distribution patterns, it was concluded that a small fraction of non-selectively bound 137Cs was remobilized at depth in some cores. Inconsistencies between the actual 137Cs fallout record and the 137Cs profiles determined for the lake sediments were attributed to 137Cs remobilization in subsurface sediments. In addition to establishing the agreement between the global atmospheric fallout record and the downcore 137Cs distribution patterns determined for these sediments, results indicate that 137Cs deposited during periods of maximum atmospheric release was buried and is not susceptible to surface erosion processes. However, mean 137Cs concentrations of the lacustrine surface sediments (125 Bq kg-1) are still significantly higher than those of the nearby Lena River estuary (11.22 Bq kg-1) and Laptev Sea (6.00 Bq kg-1). Our study suggests that the Lena River drainage basin has the potential to serve as a source of 137Cs to the adjacent Arctic Ocean

  17. Uptake, retention and organ/tissue distribution of 137Cs by Japanese catfish (Silurus asotus Linnaeus)

    The work describes the uptake, retention/biological elimination and organ/tissue distribution of 137Cs by Japanese Catfish (Silurus asotus Linnaeus) under laboratory conditions. The fish were divided in to three groups viz. large, medium and small based on their size and age and reared into the 137Cs spiked water. The concentration of 137Cs in the whole body of the live fish was measured at certain intervals up to 60 days. A significant accumulation of 137Cs was found but a steady state condition was not achieved by the end of the experiment. The Bfs at steady state condition and the required time were estimated to be 1.55 and 255 d, 1.76 and 180 d and 1.99 and 160 d for large, medium and small size fish respectively. To determine the effective halflife of 137Cs, the fish were transferred and reared into the non contaminated host water. The concentration of the remaining 137Cs in the whole body of the live fish was measured up to 66 days. The average effective half-life of 137Cs in the fish species was found to be ∼ 142 days for all size of fish. The uptake rate and the retention capability of juvenile fish were found to be higher and therefore, more susceptible to 137Cs than adult and old fish and could be an important source of 137Cs in the human food chain. The distribution of 137Cs in different organs/tissues of the fish were determined. Accumulation of 137Cs in muscle/flesh of the fish was found to be ∼ 75% of whole body accumulation. (author)

  18. Uptake, retention and organ/tissue distribution of 137Cs by Japanese catfish (Silurus asotus Linnaeus)

    The work describes the uptake, retention/biological elimination and organ/tissue distribution of 137Cs by freshwater Japanese catfish (Silurus asotus Linnaeus) under laboratory conditions. The fish were divided into three groups based on their size and age and reared in 137Cs-spiked water. The concentration of 137Cs in the whole body of the live fish was measured at regular intervals up to 60 days. A significant accumulation of 137Cs was found, but a steady state condition was not achieved by the end of the experiment. The bioaccumulation factors at steady state and the required time to reach steady state were estimated to be 1.55 and 255 days, 1.76 and 180 days and 1.99 and 160 days for large, medium and small size fish, respectively. To determine the effective half-life of 137Cs, the fish were transferred and reared in the non-contaminated host water. The concentration of the remaining 137Cs in the whole body of the live fish was measured up to 66 days. The average effective half-life of 137Cs in the fish species was found to be ∼142 days for fish of all sizes. The distribution of 137Cs in different organs/tissues of the fish was determined. Accumulation of 137Cs in muscle/flesh of the fish was found to be ∼75% of whole body accumulation. The uptake rate and the retention capability of juvenile fish were found to be higher and therefore, these were more susceptible to 137Cs than adult and old fish, and could be an important source of 137Cs in the human food chain

  19. Fire as an agent in redistributing fallout 137Cs in the Canadian boreal forest

    The presence of fallout 137Cs in the boreal forest and the effect of fire in redistributing 137Cs were studied in the remote region of Wood Buffalo National Park, N.W.T., Canada. Results of a preliminary study of five burned (the fire occurred in 1981) and five unburned stands conducted in 1986 revealed that 137Cs concentrations were higher in the surface soil of the burned stands than in the unburned ones. In 1989, a comprehensive study was conducted, in which one burned and one unburned white spruce stand were sampled in greater detail. The latter investigation also revealed a difference in the distribution of 137Cs within the burned stand compared to the unburned one. Specifically, in the unburned stand, the highest 137Cs concentration was identified in the epiphytic lichens and in the mosses, whereas in the burned stand, the highest concentration was measured in the surface organic soil. These results indicate that fire caused the mobilization of part of the 137Cs bound to the above-ground matter and concentrated it in the ash layer of the burned surface soil. An additional ecologically important finding in our study was that significantly lower total 137Cs load was observed in the burned stand compared to the unburned one. Hence, our data not only provide evidence that 137Cs is being redistributed within the burned stand to the surface soil, but also that part of the 137Cs is lost due to fire, presumably contaminating other ecosystems. Volatilization and fly-ash during the fire, and runoff (e.g. from snow melt) after the fire are the most likely mechanisms for the 137Cs removal. These findings point to fire as an agent of 137Cs secondary contamination for initially unaffected systems, as well as for those previously contaminated

  20. Study on separation of 137Cs from 235U fission process waste - utilization of silica gel-supported ferrocyanide complex salt for 137Cs picking

    In connection with the potential domestic demand especially in the fields of industry and nuclear medicine, the separation of 137Cs from 235U fission process waste is to be of interest although its economic value could be a polemic. A preliminary study on the separation of 137Cs from the 235U fission process waste generated in the production of 99Mo in P.T. BATAN Teknologi, Serpong, was performed through experiments on 137Cs picking from sample solution of the radioactive fission waste (RFW). The presented study is aimed to gain experimental data supporting utilization of the matrix of silica gel-supported ferrocyanide complex salt for the separation of 137Cs from RFW. Subsequent step would be the recovery and purification of 137Cs as part of production technology of 137Cs. The RFW sample was batch-treated with the matrix of silica gel-supported ferrocyanide complex salt which was synthesized from silica gel, potassium hexacyanoferrate(II) and copper(II) chloride. The binding of radioisotopes in RFW on the matrix was observed by γ-spectrometry of the RFW solution before and during the treatment. The results showed that approximately 85% of 137Cs could be picked from the RFW sample into the matrix. Less amount of 95Zr and 95Nb was bound into the matrix. 103Ru was slightly bound into the matrix whereas 141/144Ce and 129mTe were not. It was observed that by using 0.2 and 0.4 g of matrix for 10 ml of RFW, the amount of matrix influenced the binding quantity of 95Zr and 95Nb but not that of 137Cs. (author)

  1. 40K, 134Cs and 137Cs in pollen, honey and soil surface layer in Croatia

    Specific activities of 40K, 134Cs and 137Cs in pollen, honey and in the first 25 cm of the surface soil layer were measured by gamma-spectrometry. Specific activity of 40K in pollen is about 1 order of magnitude higher than in honey. A 40K soil-to-pollen transfer coefficient (TC(40K)) of 0.436 ± 0.054 and a soil-to-honey transfer coefficient TC(40K) of 0.052 ± 0.008 were calculated as the mean of their respective values in 26 different segments of soil profile. Both parameters have very stable values over time as well as through different segments of vertical soil profile. 134Cs and 137Cs specific activities in pollen and honey decrease with time, resulting in a decrease of 137Cs soil-to-honey transfer factors (Tf(137Cs)) over time. The increase of the soil-to-honey Tf(137Cs) with increasing soil depth is a consequence of vertical distribution of 137Cs in soil. Soil-to-honey T f(137Cs) values are highest in meadow and mixed honey types and lowest in bush/tree honey. Similar trends are found for both Tf(134Cs) and Tf(137Cs). The results presented here indicate the importance of the caesium inventory in soil segments where plant root systems are developed

  2. Field measurements of 137Cs behaviour in the litter layers of a pine forest in Ireland

    The migration of 137Cs down the forest soil profile is complex and governed by both physical and biological processes. In this forest study, two physic migration processes (137Cs leaching and little accumulation) have been evaluated and their contribution to the migration of the Chernobyl contamination compared. 1 ref., 3 figs

  3. 137Cs in Finnish wild berries, mushrooms and game meat in 2000-2005

    Activity concentrations of 137Cs in wild berries, mushrooms and game meat were measured in samples collected during 2000-2005 in areas with varying 137Cs deposition levels in Finland. Depending on the 137Cs deposition levels in the sampling areas, the areal-mean activity concentrations of 137Cs were 10-230 Bq kg-1 in wild berries, 20-240 Bq kg-1 in moose meat and 10-3000 Bq kg-1 in all mushroom species. Compared with the 137Cs level of samples collected in 1986 in the corresponding areas, the reduction in the 137Cs level was about one third for wild berries, equal to the rate of radioactive decay of 137Cs. More reduction was observed in the activity concentrations of 137Cs in moose meat, on average up to 50% since 1986. The aggregated transfer coefficients from soil to wild berries showed no change since 1986-1988, while there was about one third reduction in those from soil to game meat. (orig.)

  4. Effect of some chemical compounds on assimilation of 137Cs by hens

    Data on the decrease of 137Cs transition to the organism of laying hens after introduction of ferrocyanide and certain minerals into their ration are presented.It is established that introduction of any high capacity substances into gastrointestinal tract decreases 137Cs contact with its wall decreasing its assimilation by organism

  5. 137Cs vertical distribution at the deep basins of the North and Central Aegean Sea, Greece

    Large volume seawater samples were collected for the determination of 137Cs concentration along with depth in the deep basins of North and Central Aegean Sea. The vertical 137Cs distribution showed maximum concentration at the bottom of the basins, while the minimum values corresponded to the intermediate layer, where Levantine water exists. The surface 137Cs activity is found to lie between the two limits and is originated from the Black Sea waters. The typical oceanographic advection–diffusion balance model is modified to a diffusion-settling-decay balance model to better understand the vertical distribution and variation of the 137Cs concentration in the deep basins. In addition, the diffusivity of each basin, as well as the settling speed of particulate 137Cs is also estimated. The results are compared with theoretical approach as well as with previous data. - Highlights: • Three deep basins were studied using 137Cs as a tracer. • Deep waters constitute 137Cs repositories due to deep water formation followed Chernobyl accident. • Diffusivities, as well as particulate 137Cs settling speeds are estimated

  6. Global distribution of 137Cs inputs for soil erosion and sedimentation studies

    A global distribution of 137Cs deposition from the atmospheric nuclear tests, with estimates for 1996, excluding Chernobyl contribution, is presented, based on the global deposition data for 90Sr. The data can be used to identify areas and countries, especially in the southern hemisphere, where the 137Cs inventories are appropriate for soil erosion and sedimentation studies. (author)

  7. Investigation of radionuclide 137Cs sorption by natural and synthetic zeolites

    Sorption-selective properties of natural zeolite-clinoptilolite, from the Sokirnitsky deposit of Ukraine, and synthetic zeolites relatively to radionuclide 137Cs and depending on pH and temperature were studied. A high sorption ability of clinoptilolite relatively to 137Cs was determined

  8. Uptake of 137Cs from acidic solution by ammonium molybdophosphate (AMP) immobilized in calcium alginate

    The uptake rate for Cs+ for AMP-Ca ALG was fairly fast and the uptake attained an equilibrium within 3 hours. The observed uptake varies between 80-96% depending on the concentration of 137Cs. 137Cs is one of the major radionuclide in the effluent generated at the middle and back end of nuclear fuel cycles

  9. Behavior of 137Cs concentrations in the North Pacific in an ocean general circulation model

    Tsumune, Daisuke; Aoyama, Michio; Hirose, Katsumi

    2003-08-01

    We have carried out a first simulation of the spatial distributions and the temporal variations of 137Cs concentrations in the North Pacific in off line calculations by using archived output of an ocean general circulation model (OGCM) developed by the National Center of Atmospheric Research (NCAR). Artificial radionuclides including 137Cs are introduced into ocean surface due to global fallout originating from the large-scale atmospheric nuclear weapons tests in 1961-1962. The distribution of radioactive deposition used as forcing for this simulation is estimated from global precipitation data and observed values of annual deposition of radionuclides at the Meteorological Research Institute (MRI) in Japan. 137Cs originating from global fallout have been transported into the ocean interior by advection and diffusion, and the 137Cs concentrations reduced by radioactive decay. We assess the skill of the model calculations by comparing simulated values of 137Cs in seawater with the observed values included in the database compiled by MRI because 137Cs is one of the most useful tracers regarding water motion in the ocean. The vertical and horizontal distributions of the calculated 137Cs concentrations were in good agreement with those of the observed 137Cs concentrations, except in the deep layer.

  10. Long-term ingestion dose monitoring in a population group with increased 137Cs intake

    137Cs amounts and ingestion doses in Czech population have been monitored by whole-body counting since the Chernobyl accident. Indirect estimation of the retention through measurement of 137Cs excreted with urine in 24 hours has also been performed since 1987. The 137Cs content in human body can be calculated from the urine data provided that the intake of 137Cs during the period of interest is constant. In a semi-natural environment, the 137Cs content in mushrooms, wild berries and game decreases due to its natural decay solely. The 137Cs content in people who mostly consume venison and have been living in an area with elevated contamination has been monitored, mostly through measurement of 137Cs in urine. In parallel, measurements with a mobile whole-body counter have also been performed. Currently, annual doses from the ingestion of 137Cs in the inhabitants are very low (0.001 to 0.002 mSv.year-1). In a group of hunters in the Jeseniky Mountains (Northern Moravia) the doses were estimated to 0.10 mSv.year-1. (orig.)

  11. Regularities of 137Cs distribution for the Mozyr' Poles'e landscapes

    Long-term investigations revealed lateral redistribution of 137Cs in geochemical conjugation of elementary landscapes of the Mozyr Poles'e. The systematic study allowed to separate the zones of accumulation and of prevalently biogenic and mechanical transport of 137Cs and to establish their correlation with landscape- geochemical structure of territory

  12. Assessment of 137Cs Activity Concentration in Soil from Tea Plantation Areas in Cameron Highlands

    137Cs is well known man-made radionuclide produced from nuclear industry. Nuclear weapon tests and nuclear accidents had contributed to presence of 137Cs into the worldwide environment including Malaysia. It has spread out to the entire world through the air and water current. Since Cameron Highlands is located at high altitude, there is a better chance of the 137Cs to settle down on the trees and later the soil underneath. In this study, the soil samples were taken at the slopes of two different tea plantation areas namely A and B. The soil samples were oven dried, ground, sieved and packed and sealed properly in plastic containers before measurement. Each plastic container contains around 450 g of sample. The measurement of 137Cs activity concentration was done using HPGe detector gamma spectrometer. The spectrum was analyzed using Gamma Vision software to calculate the activity concentration of 137Cs with energy peak of 661.66 keV. The activity concentration of 137Cs found in the samples ranged from 0.23 to 1.90 and 0.11 to 3.01 Bq/ kg for tea plantation A and tea plantation B, respectively. From the activity concentration of 137Cs result, it was comparable to the others research regarding to 137Cs in the soil around Asian. (Author)

  13. Distribution of the radionuclide 137Cs in the soils of a wet mountainous forest in Taiwan

    The behavior of 137Cs was studied in the Yuanyang lake ecosystem, a wet mountainous forest in subtropical Taiwan. Soils investigated are either partially podzolic soils or nearly pure peats with a high organic matter concentration in the surface layer. Concentration of 137Cs was highest in the organic surface layers, particularly in the Oe horizon or in the underlying A horizon. The downwards migration to the mineral horizons is limited, in spite of the high rainfall. Topography is a critical factor for the distribution of 137Cs. It is shown that the concentration of 137Cs is highest at the foot of the slope and lower near the summit and near the lakeshore. The variation of the concentration along the landscape has been attributed to erosion-deposition in combination with surface run-off of the undisturbed forest. The amount of 137Cs in the site studied is significantly higher than at any other place in Taiwan. The accumulation of 137Cs is attributed to the high rainfall, which brought large amounts of 137Cs with the precipitation in the early 1960s. A very remarkable feature of the ecosystem is that 137Cs is not leached to the subsoils, but is stored in the biomass. Due to permanent recycling it remains available, without being leached downward

  14. Vertical distribution of 137Cs in the native forest soil at Londrina region (Parana, Brazil)

    The 137 Cs depth distribution has been studied in several areas in the world and its knowledge is very important to verify its behavior in the soil matrix. The form of 137 Cs depth distribution more observed in an undisturbed soil it is exponential type. In this work, the study of 137 Cs depth distribution was accomplished at three native forests and a coffee yard, built before the 137 Cs fallout, in the region of Londrina (Parana). The sampling was conducted in 1 cm, 2 cm, 4 cm and 5 cm increment depth. The 137 Cs inventory observed for the forests was 248 Bq m-2 (Mata1), 338 Bq m-2 (Mata2) and 325 Bq m-2 (MataUEL). No 137 Cs activity was detected in the coffee yard. The 137 Cs depth distribution for the three forests presented the exponential type. For the soil class of the forests, 137 Cs adsorbed on the soil particles can be considered fixed or slowly exchangeable. (author)

  15. Foliar leaching of 137Cs from Eriophorum vaginatum L., Scirpus caespitosus L. and Erica tetralix L

    Evidence of extensive leaching losses of nutrients, particularly of K, suggest that loss of 137Cs by foliar leaching could be considerable and could stimulate further root uptake and redistribution of 137Cs in plants. This study investigated the foliar leaching of 137Cs from two deciduous graminoid species, Eriophorum vaginatum and Scirpus caespitosus and one evergreen shrub, Erica tetralix. Plants were labelled with 137Cs via the roots and subjected to a leaching treatment in August and November and changes in both leachate and plant 137Cs activity were determined. Leaching losses were significantly reduced in November compared with August in the deciduous species, but not in the evergreen E. tetralix. A reduction in the total activity of 137Cs of leached plants was observed not only in leaves but also in stems and roots in some instances, suggesting that 137Cs from these organs had been redistributed to replenish that lost by leaching from the leaves. The data suggest that leaching losses were greater from older and senescent leaves than from younger leaves of E. vaginatum. The extent to which this is an accurate representation of foliar leaching of field-grown plants by rainfall, and the likely fate of 137Cs lost by foliar leaching are discussed. (author)

  16. Volatility of 137Cs and 90Sr from high-level waste glass

    Volatility of 137Cs and 90Sr from simulated high-level waste glass was examined in a closed system. The sample containing 137Cs or 90Sr was placed in a double-crucible, heated at a given temperature for 3 days and cooled to room temperature. Then the activity of 137Cs or 90Sr of the crucible was measured. Volatility of 137Cs at 8000C was measured to be about 2 x 10-2 g/cm2.day. The amount of the leakage of 137Cs from the inner crucible to the outer crucible was very small. Volatility of 137Cs at 4000C was about 1.6 x 10-6 g/cm2.day, which was almost the same as that of 90Sr at 4000C. This may indicate that fine particles adhering to the surface of the sample are the main cause of air contamination when the temperature is less than 4000C. Part of the 137Cs that was deposited on the surface of the outer crucible (stainless steel) dissolved in water at room temperature, which means that 137Cs deposited on a stainless steel surface may be easily removed by a decontamination process

  17. 137Cs Transfer Factor from Latosol Soil to Swamp Gabbages (Ipomea Reptans Poir)

    A study of 137Cs transfer factor from Latosol soil to swamp cabbages plant has been conducted using pot treatment system with complete random design. The aim of the research is to determine transfer factor of 137Cs from latosol soil to swamp cabbages plant. Cs-137 concentration administered was 7.5287 kBq/pot. The number of swamp cabbages planted in 137Cs treated soil and in cannot soil respectively was 12 pots filled with 1 kg soil/pot. After harvest, the weight of dried plant was measured. Transfer factor was determined according to the accumulation of 137Cs concentration in swamp cabbages and soil and counted using Spectrometer Gamma. It was found that is a significant difference between 137Cs concentration in swamp cabbages planted inthe treated soil and that of control soil. Transfer factor ranges between 0.02 and 0.13 with the averageof 0.08. (author)

  18. Uptake of 90Sr and 137Cs by mushrooms following the Chernobyl accident

    After the Chernobyl accident high concentrations of radionuclides were found in Sweden in mushrooms and the contents of 90Sr and 137Cs were measured. The level of 90Sr was generally low and, in proportion to 137Cs, 2-3 orders of magnitude lower than in the fallout. The contents of 137Cs varied among species, while the geographical distribution of the radioactivity largely followed the soil deposition. Extreme local variation occurred and the ratio 134Cs/137Cs diverged from other biological samples leading to the conclusion that old fallout was involved in the uptake. Transfer factors calculated for the uptake of 137Cs exhibited no correlation with the fallout levels, being mainly correlated with the different species. The problems associated with the definition of transfer factors for mushrooms were discussed. (author)

  19. Accumulation and Elimination of 137Cs Radionuclide by gold fish (Cyprinus Carpio)

    A study to estimate accumulation and elimination of 137Cs radionuclide by gold fish (Cyprinus Carpio) has been carried out. The experiment used aquarium as a cultivating media. Gold fish was placed into aquarium filled with 70 liter of water and 137Cs concentration of 10 Bq/ml. From the observing time of 40 days it was found that activity concentration in fish became saturated in 30th day. Saturation after the 30th day was confined by additional observation using 137Cs concentration of 5 and 15 Bq/ml. Saturated concentration fish was then transfered to inactive aquarium to determine is elimination rate. Transfer factor, i.e. the ratio of 137Cs concentration in fish to that in water, was found to be (12.99+0.28) ml/g, whereas the elimination rate of 137Cs was found to be 0.046 day, which correspond to a biological half life of 15 days

  20. Neural networks in analysing 137Cs behaviour in the air in the Belgrade area

    Samolov Aleksandra D.

    2014-01-01

    Full Text Available The application of the principal component analysis and artificial neural network method in forecasting 137Cs behaviour in the air as the function of meteorological parameters is presented. The model was optimized and tested using 137Cs specific activities obtained by standard gamma-ray spectrometric analysis of air samples collected in Belgrade (Serbia during 2009-2011 and meteorological data for the same period. Low correlation (r = 0.20 between experimental values of 137Cs specific activities and those predicted by artificial neural network was obtained. This suggests that artificial neural network in the case of prediction of 137Cs specific activity, using temperature, insolation, and global Sun warming does not perform well, which can be explained by the relative independence of 137Cs specific activity of particular meteorological parameters and not by the ineffectiveness of artificial neural network in relating these parameters in general. [Projekat Ministarstva nauke Republike Srbije, br. TR34034

  1. Intake estimation and dose assessment of 90Sr, 137Cs around QNPP base

    90Sr and 137Cs are important radionuclides in environmental investigation related to nuclear power stations. A mode of intake estimation and dose assessment via various food chains is made in this paper. Based on daily food consumption and dietary composition for Chinese reference man and for man of Zhejiang province and the concentration of 137Cs and 90Sr around QNPP Base, the intake estimation and dose of 90Sr and 137Cs around QNPP Base are calculated. It shows that the main food sources of intake of 90Sr and 137Cs are rice,vegetable and aquatic product. Also the public average annual committed effective dose of 90Sr(2.5 μSv)is obviously higher than the contribution of dose of the 137Cs(0.36 μSv). A practical estimation method was made by taking QNPP Base as an example in this paper, while no background change occurs after its commercial operation. (authors)

  2. Translocation, accumulation and distribution of 137Cs in rice after foliage contamination

    The single leaf of rice stem was artificially contaminated with 137Cs at different growth stages to study its foliage absorption and translocation. The results showed that the translocation rate of 137Cs to non-contaminated parts of the plant was related with the phyllo-taxis of the contaminated leaf and the majority of 137Cs in the plant was distributed in leaves and stems. For rice being contaminated, there was a positive linear relationship between the accumulation of 137Cs in each non-contaminated part of the plant and the amount of the contamination. The order of the specific activity of 137Cs was: Leaf>Stem>root>ear in non-contaminated parts of the plant

  3. Re-distribution of 137Cs Chernobyl signal in the Aegean Sea

    The present levels of 137Cs in the water column of the Aegean Sea are at all depths, significantly higher than in the pre-Chernobyl period. The concentrations in surface and intermediate water show a linear relationship to salinity, indicating that mixing of Black Sea Water with highly saline waters of Levantine origin is the main process controlling 137Cs levels. The present 137Cs concentrations in deep basins of the North and South Aegean (3.7 - 5.5 Bq m-3) are the highest in the deep waters of the Mediterranean Sea. In the North Aegean the transfer of 137Cs from the surface layers to the bottom took place through the dense water formation events in 1987 and 1993. The 137Cs levels in the deep South Aegean are higher than expected, possibly in relation to a contribution of N-Aegean deep waters. (author)

  4. Seasonality of 137Cs in roe deer from Austria and Germany

    Empirical data on the 137Cs activity concentration in meat of roe deer (Capreolus capreolus) roaming in 3 spruce forest areas and one peat bog area are presented and compared. They cover time series of nearly 20 years after a spike contamination in 1986 originating from Chernobyl. A model is presented which considers three soil compartments to describe the change of the availability of 137Cs with time. The time-dependency of the 137Cs activity concentration in meat of roe deer is a combination of two components: (1) an exponential decay and (2) a peak in the second half of each year during the mushroom season. The exponential decay over the years can be described by a sum of two exponential functions. The additional transfer of 137Cs into roe deer during the mushroom season depends on precipitation. On the peat bog the 137Cs activity concentration in roe deer is higher and more persistent than in spruce forest

  5. 137Cs vertical migration in a deciduous forest soil following the Fukushima Dai-ichi Nuclear Power Plant accident

    The large amount of 137Cs deposited on the forest floor because of the Fukushima Dai-ichi Nuclear Power Plant accident represents a major potential long-term source for mobile 137Cs. To investigate 137Cs mobility in forest soils, we investigated the vertical migration of 137Cs through seepage water, using a lysimetric method. The study was conducted in a deciduous forest soil over a period spanning 2 month to 2 y after the Fukushima nuclear accident. Our observations demonstrated that the major part of 137Cs in the litter layer moved into the mineral soil within one year after the accident. On the other hand, the topsoil prevented migration of 137Cs, and only 2% of 137Cs in the leachate from litter and humus layer penetrated below a 10 cm depth. The annual migration below a 10 cm depth accounted for 0.1% of the total 137Cs inventory. Therefore, the migration of 137Cs by seepage water comprised only a very small part of the total 137Cs inventory in the mineral soil, which was undetectable from the vertical distribution of 137Cs in the soil profile. In the present and immediate future, most of the 137Cs deposited on the forest floor will probably remain in the topsoil successively, although a small but certain amount of bioavailable 137Cs exists in forest surface soil. -- Highlights: • Lysimeter captured 137Cs mobility in a forest soil after the Fukushima accident. • Major part of 137Cs in the litter layer moved into the mineral soil within a year. • Litter-leachate 137Cs was predominantly adsorbed within the topsoil. • The annual migration below a 10 cm depth was 0.1% of the total 137Cs inventory

  6. Effects of radiocesium inventory on 137Cs concentrations in river waters of Fukushima, Japan, under base-flow conditions

    To investigate the behavior of nuclear accident-derived 137Cs in river water under base-flow conditions, concentrations of dissolved and particulate 137Cs were measured at 16 sampling points in seven rivers of Fukushima Prefecture, Japan, in 2012 and 2013. The concentration of dissolved 137Cs was significantly correlated with the mean 137Cs inventory in the catchment area above each sampling point in both sampling years. These results suggest that the concentration of dissolved 137Cs under base-flow conditions is primarily determined by the 137Cs inventory of the catchment area above the sampling point. However, the concentration of particulate 137Cs did not show a clear relationship with either the mean 137Cs inventory or the dissolved 137Cs concentration, thus indicating that particulate and dissolved forms do not effectively interact in rivers. To evaluate the contribution of the 137Cs inventory within catchment areas, we analyzed relations between the 137Cs concentration and the mean 137Cs inventory over the area within certain flow path lengths that were traced along the river and slope above the sampling point. Coefficients of determination for dissolved 137Cs concentrations were highest for the longest flow path, i.e., the whole catchment area, and lower for shorter flow paths. Coefficients of determination for particulate 137Cs concentrations were only moderately high for the shortest flow path in 2012, whereas the values were quite low for all flow paths in 2013. These results suggest that dissolved 137Cs can originate from a larger area of the catchment even under base-flow conditions; however, particulate 137Cs did not show such behavior. The results also show that under base-flow conditions, dissolved and particulate 137Cs behave independently during their transport from river catchments to the ocean. - Highlights: • 137Cs in river water under base-flow conditions was investigated in Fukushima. • Dissolved 137Cs was significantly correlated with 137

  7. 137Cs applicability to soil erosion assessment: theoretical and empirical model

    The soil erosion processes acceleration and the increase of soil erosion rates due to anthropogenic perturbation in soil-weather-vegetation equilibrium has influenced in the soil quality and environment. So, the possibility to assess the amplitude and severity of soil erosion impact on the productivity and quality of soil is important so local scale as regional and global scale. Several models have been developed to assess the soil erosion so qualitative as quantitatively. 137Cs, an anthropogenic radionuclide, have been very used to assess the superficial soil erosion process Empirical and theoretical models were developed on the basis of 137 Cs redistribution as indicative of soil movement by erosive process These models incorporate many parameters that can influence in the soil erosion rates quantification by 137 Cs redistribution. Statistical analysis was realized on the models recommended by IAEA to determinate the influence that each parameter generates in results of the soil redistribution. It was verified that the most important parameter is the 137 Cs redistribution, indicating the necessity of a good determination in the 137 Cs inventory values with a minimum deviation associated with these values. After this, it was associated a 10% deviation in the reference value of 137 Cs inventory and the 5% in the 137 Cs inventory of the sample and was determinate the deviation in results of the soil redistribution calculated by models. The results of soil redistribution was compared to verify if there was difference between the models, but there was not difference in the results determinate by models, unless above 70% of 137 Cs loss. Analyzing three native forests and an area of the undisturbed pasture in the Londrina region, can be verified that the 137 Cs spatial variability in local scale was 15%. Comparing the 137 Cs inventory values determinate in the three native forest with the 137 Cs inventory value determinate in the area of undisturbed pasture in the

  8. 137Cs and 40K partitioning in the system soil-plant under different ecological conditions

    In the environment 137Cs is exclusively of the anthropogenic origin. Among different released fission radionuclides, 137Cs is the most significant one as it contributes to long-term doses to population. It belongs to the group of radionuclides which under accidental situations can disperse worldwide because of air mass transport. 137Cs deposition in the Lithuanian terrestrial and aquatic ecosystems is basically related to the global fallout and contaminated air masses from the Chernobyl NPP accident. An extra load of 137Cs to the Lithuanian terrestrial ecosystems was determined after the Fukushima Daiichi NPP accident as well. Over the recent decades evident changes in the approach to the radiation protection of non-human species from ionizing radiation have taken place. Furthermore, long-term predictions of the mobility and bioavailability of 137Cs are required because of its penetration into the food chain. 40K is a typical lithophilic element and its geochemistry could be similar to that of 137Cs because they both are of the same valence state, +1. Investigation results of 137Cs and 40K behavior in the environmental systems in the literature are rather contradictory. Therefore, the aim of the present study is to assess 137Cs and 40K activity concentration in soil and various plants of a different root system and to compare bioavailability of these radionuclides under different environmental ecological conditions. 137Cs deposition distribution in the upper soil layer is different in the studied territory. The mean 137Cs activity concentrations in soil and plants in the post-Chernobyl period varied in a wide range. 137Cs activity concentrations in soil varied from about 30 Bq/kg to 340 Bq/kg, while in various plants and grasses the range was 45-119 Bq/kg. Mean values of the 137Cs transfer factor ranged from 0.1 to 1.4. The discrimination factor was determined to evaluate the effect of 40K activity concentration in soil and plants on distribution of 137Cs in plants

  9. Hanford Isotope Project strategic business analysis Cesium-137 (Cs-137)

    NONE

    1995-10-01

    The purpose of this business analysis is to address the beneficial reuse of Cesium 137 (Cs-137) in order to utilize a valuable national asset and possibly save millions of tax dollars. Food irradiation is the front runner application along with other uses. This business analysis supports the objectives of the Department of Energy National Isotope Strategy distributed in August 1994 which describes the DOE plans for the production and distribution of isotope products and services. As part of the Department`s mission as stated in that document. ``The Department of Energy will also continue to produce and distribute other radioisotopes and enriched stable isotopes for medical diagnostics and therapeutics, industrial, agricultural, and other useful applications on a businesslike basis. This is consistent with the goals and objectives of the National Performance Review. The Department will endeavor to look at opportunities for private sector to co-fund or invest in new ventures. Also, the Department will seek to divest from ventures that can more profitably or reliably be operated by the private sector.``

  10. Modeling 137CS dispersion from a radiological dispersion device

    This analysis reveals that, if terrorists detonate a RDD containing a relatively small amount of 137Cs (approximately 12-35g), the resulting dispersion can contaminate a relatively large area. The actual magnitude of a terrorist incident involving the release of radioactive material by a dirty bomb depends on the dimensions of the contaminated area and the accompanying contamination density (i.e., radioactivity) distributed within that area. Applying a semiempirical model indicates that the spatial extent of the contaminated area and the level of activity within that area are dependent primarily on local scale meteorological conditions, especially whether rainfall occurs, as well particle size and effective release height. As a result, the magnitude of the consequences of terrorists acquiring non-weapons grade nuclear materials and releasing those materials with a dirty bomb is contingent on a number of factors beyond the scope of active countermeasures, especially the RDD's design elements and local-scale meteorological conditions. Modeling the dispersion of radioactive aerosols throughout an urban landscape, especially with accurate 3-D representation of its complex geometry and meteorology, is indispensable for assessing the potential consequences of a terrorist incident and implementing effective emergency response, health services, and decontamination decisions. (orig.)

  11. Hanford Isotope Project strategic business analysis Cesium-137 (Cs-137)

    The purpose of this business analysis is to address the beneficial reuse of Cesium 137 (Cs-137) in order to utilize a valuable national asset and possibly save millions of tax dollars. Food irradiation is the front runner application along with other uses. This business analysis supports the objectives of the Department of Energy National Isotope Strategy distributed in August 1994 which describes the DOE plans for the production and distribution of isotope products and services. As part of the Department's mission as stated in that document. ''The Department of Energy will also continue to produce and distribute other radioisotopes and enriched stable isotopes for medical diagnostics and therapeutics, industrial, agricultural, and other useful applications on a businesslike basis. This is consistent with the goals and objectives of the National Performance Review. The Department will endeavor to look at opportunities for private sector to co-fund or invest in new ventures. Also, the Department will seek to divest from ventures that can more profitably or reliably be operated by the private sector.''

  12. Variability of 137Cs inventories in undisturbed soils across the territory of Viet Nam

    Inventories of 137Cs were measured in putatively undisturbed soils at 292 locations throughout the territory of Viet Nam. Logarithms of these values were regressed against characteristics of the sampling sites, such as geographical co-ordinates, annual rainfall and physico-chemical parameters of soil. The regression model containing latitude and annual rainfall, as explanatory variables, could explain 76% of the variation in logarithmic inventory values. The model was interpreted to represent the spatial distribution of 137Cs deposition density while the regression residuals were assigned to the loss or gain of 137Cs due to soil erosion or accretion at the sampling sites. Depth-distribution profiles of 137Cs, measured at eight selected sites, provided support for this interpretation. In particular, a linear relationship was found between the residual and the 137Cs-penetration depth. Although, on average, the measured inventories differed from the deposition values by 31%, the 137Cs deposition density could be predicted by the regression model with a ±7% relative uncertainty at a 95% confidence level. The model has, therefore, been used to provide 137Cs baseline values in soil-erosion studies. These results are in general agreement with the global pattern published in 1969 by the United Nations Scientific Committee on the Effects of Atomic Radiation, and provide further insights into the spatial distribution of nuclear-test fallout deposition in East Asia. (author)

  13. Physical and chemical parameters affecting transport of 137Cs in arid watersheds

    The occurrence and amount of fallout 137Cs were determined in 12 watersheds in the arid southwestern United States. The factors believed to influence the distribution of 137Cs in the watershed soils and in the reservoir sediments were investigated by using stepwise regression techniques. Seventeen parameters, in the case of soils, and 21 parameters, in the case of sediments, were used in the study. Ninety percent of the variation in the 137Cs content of soils, per unit weight, could be predicted in terms of the percentage of soil nitrogen, the R factor (rainfall intensity) of the universal soil loss equation, the percentage of sand in the soils, and the soil cation exchange capacity. Also, 90% of the variation in the content of 137Cs in the watershed soils, per unit area, could be predicted in terms of the fallout intensity, the percentages of silt and clay, and the cation exchange capacity. For reservoir sediments the equivalent predictors of 137Cs accumulation in the sediment profile, per unit weight, were the soil cation exchange capacity, the January-March average precipitation, and the soil contents of total P and N. The distribution of 137Cs in sediments per unit area was similarly predicted by watershed area, percentage of total soil C, reservoir surface area, areal concentration of 137Cs in the watershed soils, and soil organic matter

  14. Uptake of 137Cs from coniferous forest soil by sheep's fescue in pot experiment

    The uptake of Chernobyl fallout radiocaesium (137Cs) from forest soils with low nutrients, high organic matter content, and acidic pH were examined in pot experiments. Results of sheep's fescue (Festuca ovina) two harvests after growing period of 13 weeks each, showed a slight variation in the 137Cs uptake. Transfer factor (TF) for 137Cs based upon soil-to-plant relationships calculated, (Bqkg-1 plant DW/Bqkg-1 soil DW). The ranges were from 0.03 to 3.43 with a mean of 0.34 ± 0.31 for first cut and from 0.03 to 2.28 with a mean of 0.36 ± 0.33 for second cut. Variation in the uptake of 137Cs by sheep's fescue grass might be due to the influence of soil pH and OM % in conjunction with soil moisture. The effect of potassium (K+), stable caesium (Cs+), and ammonium (NH4+) that were added as chlorides on 137Cs uptake by sheep's fescue were also tested in pot experiment under the same conditions of previous set-up. Results from three harvests after growing period of 13 weeks each, demonstrated that K+ reduced the uptake of 137Cs. In contrast the addition of both stable Cs+ and NH4+ found to enhance 137Cs uptake by sheep's fescue. (author)

  15. The latitudinal inventory of sup(137)Cs in vegetation and topsoil in northern Canada, 1980

    The latitudinal distribution of fallout sup(137)Cs in Canada has been determined along a transect extending from 50 degrees to 82 degrees N in 1980. The sup(137)Cs content of lichens, bryophytes, and cushionlike vascular species was measured at 16 sites between Brandon, Manitoba, and Alert, Ellesmere Island. Lichen species were shown to be the most effecive biological monitors of sup(137)Cs deposition because of their specific morphology, longevity, and slow growth rates. Dry, exposed ridges were the sites of the highest sup(137)Cs retention by plants. sup(137)Cs levels in vegetation followed a bell-shaped distribution along the transect and the maximum accumulation was measured in samples collected between 60 degrees and 70 degrees N ((10 nCi msup(-2) at 63 degrees N) (1 Ci = 37 GBq). This distribution is the combined results of the original latitudinal deposition of sup(137)Cs, the expired portion of its physical half-life, and the efficiency of biotic and abiotic removal processes along the studied corridor. It is suggested that the long-term implications of sup(137)Cs in the northern food chain ought to be followed and studied more closely in the light of the data presented

  16. 137Cs dynamics within a reactor effluent stream in South Carolina

    Radiocesium dynamics are being studied in a blackwater creek which had received production reactor releases from the Savannah River Plant in South Carolina. Most 137Cs in the water column is dissolved or in colloidal form and is believed to originate primarily through outflow from an upstream ''contaminated'' reservoir. All ecosystem components in the stream have high 137Cs concentration factors. Radiocesium concentrations are highest in filamentous algae (332 pCi/g-dry) and suspended particulate matter (100 to 200 pCi/g). Other food chain bases had much lower 137Cs levels. Most consumer populations averaged 10 to 50 pCi/g. Radiocesium concentrations decreased in transfers between food chain bases and primary consumers or filter feeders. Omnivores and small predators have similar 137Cs concentrations with bioaccumulation occurring by top-carnivores. Radiocesium levels are around 100 pCi/g in largemouth bass and water snakes. Foodweb components in the stream have reached a dynamic equilibrium in 137Cs concentrations despite a 10 yr absence of reactor operations. Radiocesium levels are apparently being maintained through long-term 137Cs cycling in the upstream reservoir and surrounding flood plain forest systems. Rainfall and other physical processes influence the seasonal 137Cs fluctuations in stream components

  17. Availability and immobilization of 137Cs in subtropical high mountain forest and grassland soils

    To understand the behavior of 137Cs in undisturbed soils after nuclear fallout deposition between the 1940s and 1980s, we investigated the speciation of 137Cs in soils in forest and its adjacent grassland from a volcano and subalpine area in Taiwan. We performed sequential extraction of 137Cs (i.e., fractions readily exchangeable, bound to microbial biomass, bound to Fe-Mn oxides, bound to organic matter, persistently bound and residual). For both the forest and grassland soils, 137Cs was mainly present in the persistently bound (31-41%) and residual (22-62%) fractions. The proportions of 137Cs labile fractions - bound to exchangeable sites, microbial biomass, Mn-Fe oxides, and organic matter - were lower than those of the recalcitrant fractions. The labile fractions in the forest soils were also higher than those in the grassland soils, especially in the volcanic soil. The results suggest that the labile form of 137Cs was mostly transferred to the persistently bound and resistant fractions after long-term deposition of fallout. The readily exchangeable 137Cs fraction was higher in soils with higher organic matter content or minor amounts of 2:1 silicate clay minerals

  18. Vertical distribution of 137Cs activity concentration in marine sediments at Amvrakikos Gulf, western of Greece

    The aim of the present work is the study of 137Cs migration in sediment column taking into account the sedimentation rate in the Amvrakikos Gulf, at the western part of Greece. Marine core sediments were collected and the measurements were performed using the high resolution gamma-ray spectrometry method. The vertical distribution of 137Cs activity concentration, as part of anthropogenic marine radioactivity, provided averaged sedimentation rate by identifying the depths of activity concentrations due to the Chernobyl accident and the nuclear tests signals. Furthermore, 137Cs measurements were reproduced using the proposed one-dimensional diffusion–advection model which provides mainly as an output, the sedimentation rate and the average diffusivity of 137Cs in the sediment column. The proposed model estimates the temporal variation of 137Cs activity concentration from 1987 (one year after the Chernobyl accident) till today (2014). - Highlights: • Two sediment cores were studied using 137Cs as a tracer. • Two peaks are observed due to nuclear tests and Chernobyl accident. • Diffusivities, as well as 137Cs apparent sedimentation speeds are estimated

  19. The occurrence and bioavailability of radioactive 137Cs in small forest lakes in southern Finland

    Following the Chernobyl accident in late April 1986, central Finland was subjected to considerable radioactive fallout. The radioactive isotope of caesium, 137Cs, was potentially the most harmful isotope in the fallout because of its long half-life (30 years). 137Cs activities remained unexpectedly low within the biota (algae, zooplankton, aquatic moss, fish) of some humic forest lakes in southern Finland compared to the clear water lakes within the same district. This observation suggested that humic substances, by binding 137Cs chemically, may reduce its bioavailability in lake water. Our laboratory experiments (throughflow systems; gel chromatography) demonstrated that binding of 137Cs by humic substances was negligible in untreated lake waters; only when most of the alkali metals had been removed with an ion exchange resin was any binding of 137Cs by low molecular humic fractions apparent. Instead, the concentrations of cations (especially potassium) were of overwhelming importance for the bioavailability of 137Cs within the lacustrine ecosystems. The concentrations of 137Cs within food chains are expected to stay at a high level for many years especially in lakes with long water renewal times. (Author)

  20. Foliar absorption and translocation of 137cs in egyptian olive plants

    Foliar absorption and translocation of 137Cs by olive leaves were studied. Olive seedlings were transferred to the greenhouse in pots containing fine Nile silt.. Two seriies of pot experiments were conducted at the Nuclear Research Center site at Inshas. The treatments were conducted on leaves at the two middle nodes of the selected shoots. The lower surface of the olive leaf absorbed more 137Cs at the studied pH values as compared with the upper surface. The results show that changing the pH from 2 to 3 had no have any effect on the foliar absorption of 137Cs. Further increase of pH value caused the 137Cs foliar absorption to show a minimum at pH 5 then a maximum at pH 7. At pH 8 the foliar absorption of 137Cs started to decrease again. The concentration of translocated 137Cs was found to decrease gradually in the leaves above and below the treated ones. Absorption of 137Cs increased with time in the first 24 hours followed by lower absorption rates till the end of the experiment after 148 hours

  1. Fallout 137Cs in cultivated and noncultivated north central United States watersheds

    The cesium (137Cs) concentrations were measured in the soils and sediments of 14 watersheds, 7 cultivated and 7 noncultivated, in the North Central United States. The 137Cs concentration in watershed soils ranged from 56 to 149 nCi/m2, with cultivated watersheds averaging 75 nCi/m2 and noncultivated watersheds averaging 104 nCi/m2. The 137Cs concentration in the reservoir sediments ranged from 74 to 1,280 nCi/m2, with a mean of 676 nCi/m2 for the cultivated watersheds and 365 nCi/m2 for the noncultivated watersheds. The 137Cs concentrations per unit area in sediments were 0.8 to 18.7 times greater than those found in the contributing watershed soils. This indicated that some 137Cs is moving within the watersheds and that the reservoirs are acting as ''traps'' or ''sinks.'' The factors accounting for the variation in 137Cs concentration in the soils and sediments of the watersheds are (i) the erosion potential of the watershed, (ii) the sites for adsorption of 137Cs, and (iii) the input of radioactivity into the watershed

  2. Transfer of 137Cs and stable Cs in soil-grass-milk pathway in Aomori, Japan

    The soil-to-grass transfer factors and grass-to-milk transfer coefficients were determined for 137Cs and stable Cs in soil, grass and milk samples collected in Aomori Prefecture, Japan. The concentrations of 137Cs in the soil and grass samples collected from 25 sampling sites were 13 ± 12 Bq x kg-1 and 2.0 ± 2.1 Bq x kg-1 dry wt., respectively. The geometric mean of soil-to-grass transfer factor of 137Cs was 0.13 and its 95% confidence interval was 0.017-0.98. The transfer factor of 137Cs was higher than that of stable Cs, and they had a positive correlation. The concentration of K in the soil affected both transfer factors. The concentration of 137Cs in milk samples collected from 16 sites was 76 ± 43 mBq x kg-1 fresh wt. and had a good correlation with that of stable Cs. The geometric mean of grass-to-milk transfer coefficient of 137Cs was 0.0027, assuming that a cow's total daily intake was 20 kg of dry grass. The transfer coefficient of 137Cs was positively correlated with that of stable Cs. (author)

  3. Uptake of 137Cs from coniferous forest soil by sheeps' fescue in pot experiment

    The uptake of the post-Chernobyl 137Cs fallout from forest soils with low nutrients, high organic matter content and acidic pH was examined in pot experiments. Results of sheep's fescue (Festuca ovina) two harvests (after growing period of 13 weeks) showed a considerable variations in 137Cs uptake. Transfer factor (TF) for 137Cs based upon soil-to-plant relationships was calculated: Bqkg-1 plant DW / Bqkg-1 soil DW. A considerable fluctuations in the values were also observed. The ranges were: from 0.03 to 3.43 with a mean of 0.35±0.43 for the first cut and from 0.03 to 2.28 with a mean of 0.36±0.42 for the second cut. This variation in the 137Cs uptake by sheep's fescue grass might be due to the influence of high soil OM% and soil pH in conjunction with soil moisture. The effect of potassium (K+), stable caesium (Cs+), and ammonium (NH4+) that were added as chlorides on 137Cs uptake by sheep's fescue were also tested in a pot experiment under the same conditions of previous set-up. Results of three harvests demonstrated that K+ reduced the uptake of 137Cs. In contrast an addition of both Cs+ and NH4+ seams to enhance the uptake of 137Cs by sheep fescue. (author)

  4. 137Cs in the Danish Wadden Sea: contrast between tidal flats and salt marshes

    The 137Cs activity of salt marsh and tidal flat sediments of the northern part of the European Wadden Sea was studied based on a comprehensive dataset of 210Pb dated cores. The 137Cs inventory of salt marsh sediments shows a major peak corresponding to the Chernobyl accident in 1986, and a minor peak located in the late 1960s interpreted as the combined effect of atmospheric testing of nuclear weapons. Emissions from the nuclear reprocessing plant Sellafield are not reflected as peaks in 137Cs activity, but may contribute to the rising 137Cs activity in the years prior to 1986. The 137Cs activity of tidal flat sediments differs from salt marsh sediment in two respects. First, the activity is much lower and, second, the major peak in the 1980s is located in the beginning instead of in the middle of the decade. The differences in 137Cs inventory between the two environments are interpreted to result from repeated cycles of deposition/resuspension and mixing on tidal flats. A simple model illustrating the consequence of mixings returns an apparent shift of major peaks in 137Cs activities backwards in time corresponding to the mixing depth divided by the deposition rate

  5. Concentration ratios for small mammals collected from the exposed sediments of a 137Cs contaminated reservoir

    137Cs concentration ratios were computed for small mammals collected from the dried sediments of a partially drained, contaminated reservoir. Soil 137Cs activity concentrations were heterogeneous on small and large spatial scales and had a geometric mean of 253 (range 23-2110) Bq/kg dry weight. Mean 137Cs activity concentrations in composite cotton rat Sigmodon hispidus and cotton mouse Peromyscus gossypinus samples averaged 2480 (range 556-6670) and 471 (range 96-1000) Bq/kg whole body dry weight, respectively. About 50% of the variance in cotton rat tissue 137Cs activity was explained by variation in soil 137Cs activity. Soil-to-animal dry weight concentration ratios averaged 6.0 for cotton rats and 1.2 for cotton mice and were generally similar to 137Cs concentration ratios for herbivorous, homeothermic animals from other contaminated ecosystems. In the RESRAD-BIOTA dose model, the default wet-weight concentration ratio for 137Cs in terrestrial animals is 110 resulting in an estimate of internal and external radiation doses to terrestrial biota that is 44 times more than the dose calculated with the actual measured wet-weight concentration ratio for cotton rats (1.6). These results show that site-specific concentration ratios can significantly affect the estimation of dose

  6. Uptake, retention and organic/tissue distribution of 137Cs by Japanese catfish (Silurus asotus linnaeus)

    Full text: This works describes the uptake, retention/biological elimination of 137Cs by Japanese Catfish (Silurus asotus linnaeus) under laboratory conditions. The fish were divided in to three groups viz. large, medium and small and reared in to the host water contaminated by 137Cs. The accumulated 137Cs concentration in the whole body of the fish was measured at certain intervals up to 60 days. A significant accumulation of 137Cs was found but a steady state accumulation of 137Cs was not achieved by the end of the experiment. The bioaccumulation factors and the distribution of the radionuclide in different organs/tissues of the fish were determined. To determine the effective half-life, the fish were transferred and reared into the non contaminated host water. The concentration of the radionuclide in the whole body of the fish was measured up to 66 days. Neglecting the small first compartment for a few days, the average effective half-life of 137Cs in the fish species was found to be ∼ 30 days for all size of fish. Accumulation of 137Cs in muscle/flesh of the fish was found to be ∼ 75% of whole body accumulation. (author)

  7. Evaluation of radioactive exposure from 137Cs in contaminated areas of Northern Ukraine.

    Handl, J; Beltz, D; Botsch, W; Harb, S; Jakob, D; Michel, R; Romantschuk, L D

    2003-04-01

    The paper gives averages of 137Cs deposition densities in soils from three areas in Northern Ukraine measured 12 to 15 y following the Chernobyl accident: in an area near Narodici (75 km west of the Chernobyl nuclear power plant in the so-called zone II) heavily contaminated by the Chernobyl fall-out and in areas around Korosten and Zhitomir showing contamination levels to be much lower. The three areas exhibited very different 137Cs deposition densities of 2.2 MBq m(-2), 400 kBq m(-2), and 5 kBq m(-2), respectively. During a 1-y observation, measurements of the 137Cs transfer in the food chain to humans and 137Cs whole body contents dependent on the 137Cs daily intake were carried out under realistic conditions of the rural inhabitants who lived in settlements within zone II. Detailed investigations of components of the daily diet showed that the high 137Cs contamination levels found in soils of zone II do not affect in any way low 137Cs concentrations of all important agricultural products harvested and consumed by villagers. With regard to consumption habits of the population of zone II, mushrooms and wild berries were found to contribute more than 95% of the 137Cs daily intake to the 137Cs whole body content of about 12 kBq (with maximum values up to 760 kBq) measured in a group of inhabitants of zone II during a period from July 1998 to July 1999. The median of the annual dose of these inhabitants from external and internal exposures was 1.2 mSv y(-1) with a geometric standard deviation of 2.6. Excluding extreme habits, the geometric mean of the total exposure was 1.0 mSv y(-1) with a geometric standard deviation of 1.3. PMID:12705449

  8. {sup 137}Cs in marine sediments of Admiralty Bay, King George Island, Antarctica

    Ferreira, Paulo Alves de Lima [Instituto Oceanográfico, Universidade de São Paulo (IO-USP), Pça. do Oceanográfico, 191, Butantã, SP, 05508 900 (Brazil); Ribeiro, Andreza Portella, E-mail: andrezpr@usp.br [Instituto Oceanográfico, Universidade de São Paulo (IO-USP), Pça. do Oceanográfico, 191, Butantã, SP, 05508 900 (Brazil); Mestrado de Gestão Ambiental e Sustentabilidade, Universidade Nove de Julho (UNINOVE), Avenida Francisco Matarazzo, 612, prédio C, andar térreo, Água Branca, São Paulo, SP, 05001 100 (Brazil); Nascimento, Mylene Giseli do; Martins, Cesar de Castro [Centro de Estudos do Mar, Universidade Federal do Paraná (CEM-UFPR), Av. Beira-mar, no number, Balneário Pontal do Sul, Pontal do Paraná, PR, 83255 971 (Brazil); Mahiques, Michel Michaelovitch de; Montone, Rosalinda Carmelo; Figueira, Rubens Cesar Lopes [Instituto Oceanográfico, Universidade de São Paulo (IO-USP), Pça. do Oceanográfico, 191, Butantã, SP, 05508 900 (Brazil)

    2013-01-15

    The radionuclide cesium-137 ({sup 137}Cs) is produced exclusively by anthropogenic processes and primarily by nuclear explosions. This study determined the reference inventory that is {sup 137}Cs associated with the element's original input, and utilized the levels of activity of this radionuclide previously measured in five sediment profiles collected from Admiralty Bay, Antarctica, to investigate the mobility of this element in the environment. {sup 137}Cs has a half-life of 30 years. Because of this, it is environmentally persistent and has been shown to accumulate in marine organisms. The mean reference inventory of this radionuclide in Admiralty Bay sediments, determined using high resolution gamma ray spectrometry, was 20.23 ± 8.94 Bq m{sup −2}, and within the ambient {sup 137}Cs activity range. A model of {sup 137}Cs diffusion–convection was applied to data collected from 1 cm intervals in sediment cores with the aim of providing insights with respect to this element's behavior in sediments. Model results showed a significant correlation between measured and modeled values using the concentrations of {sup 137}Cs, and estimated input into the system from the global fallout of past nuclear tests and expected values based on local sedimentation rates. Results highlight the importance of accounting for the vertical diffusion of {sup 137}Cs in marine sediments when used as a tracer for environmental processes and for assessing potential bioavailability. - Highlights: ► Cesium-137 ({sup 137}Cs) is produced exclusively by anthropogenic processes. ► A model of diffusion–convection simulated {sup 137}Cs environmental behavior. ► This is important for assessing the bioavailability of this toxic element. ► In Antarctica ice cover influenced the input to the sediments.

  9. 137Cs in marine sediments of Admiralty Bay, King George Island, Antarctica

    The radionuclide cesium-137 (137Cs) is produced exclusively by anthropogenic processes and primarily by nuclear explosions. This study determined the reference inventory that is 137Cs associated with the element's original input, and utilized the levels of activity of this radionuclide previously measured in five sediment profiles collected from Admiralty Bay, Antarctica, to investigate the mobility of this element in the environment. 137Cs has a half-life of 30 years. Because of this, it is environmentally persistent and has been shown to accumulate in marine organisms. The mean reference inventory of this radionuclide in Admiralty Bay sediments, determined using high resolution gamma ray spectrometry, was 20.23 ± 8.94 Bq m−2, and within the ambient 137Cs activity range. A model of 137Cs diffusion–convection was applied to data collected from 1 cm intervals in sediment cores with the aim of providing insights with respect to this element's behavior in sediments. Model results showed a significant correlation between measured and modeled values using the concentrations of 137Cs, and estimated input into the system from the global fallout of past nuclear tests and expected values based on local sedimentation rates. Results highlight the importance of accounting for the vertical diffusion of 137Cs in marine sediments when used as a tracer for environmental processes and for assessing potential bioavailability. - Highlights: ► Cesium-137 (137Cs) is produced exclusively by anthropogenic processes. ► A model of diffusion–convection simulated 137Cs environmental behavior. ► This is important for assessing the bioavailability of this toxic element. ► In Antarctica ice cover influenced the input to the sediments

  10. Distributions of 137Cs and 210Pb in moss collected from Belarus and Slovakia

    In the present work, moss samples collected in Slovakia and Belarus were assayed with respect to gamma-emitting radionuclides. The results for 137Cs and 210Pb are discussed. Moss was used for the first time in Belarus, as a biological indicator of radioactive environmental pollution in consequence of the Chernobyl accident in 1986. In Belarus, the maximum activity of 137Cs was observed in the Gomel region near Mazyr (6830 Bq/kg) and the minimum activity in the Vitebsyevsk Region near Luzhki-Yazno (5 Bq/kg). “Hot spots” were also observed near the towns Borisow and Yuratsishki. The results of measurements of 137Cs in moss samples collected in 2000, 2006 and 2009 in the same localities of Slovakia are presented and compared with the results of air monitoring of 137Cs carried out in Slovakia from 1977 until 2010. Measurements of the 210Pb concentration in moss samples collected over the territory of Slovakia showed, that the median value exceed 2.3 times median value of 210Pb obtained for Belarus moss. For that reason, the inhalation dose for man from 210Pb and 137Cs in Slovakia is more than twice as high as in Belarus, in spite of the initially very high 137Cs exposure in the latter country. -- Highlights: ► Belarus moss was used as a biological indicator of 137Cs and 210Pb. ► Comparison with concentration of 137Cs and 210Pb in moss from Slovakia. ► Moss samples reflect the original distribution of Chernobyl fallout in Belarus. ► Regular decrease of the annual average activity of 137Cs in surface air in Slovakia. ► Median concentration of 210Pb in moss from Belarus is 2.3 times lower than in Slovakia

  11. 137Cs in small forest lakes of Finland after the Chernobyl accident

    A joint monitoring study between the Radiation and Nuclear Safety Authority (STUK) and the Finnish Game and Fisheries Research Institute (FGFRI) on the radioactivity of forest lakes in Evo, Southern Finland, was started in summer 1987. Besides fish, lake water and other biota, such as zooplankton, larvae of various insects and aquatic plants, were analysed from these lakes. Soil samples from the lake catchments were also analysed in 1988 - 1989. In 1992, samples of bottom sediment were analysed from one lake for 137Cs. In addition, fish from the Finnish Acidification Research Project of FGFRI from several small forest lakes in 1986 - 1989 were analysed for 137Cs. The results obtained in the joint study of STUK and FGFRI are gathered in this report. The highest activity concentrations of 137Cs in fish were about 30 000 Bq / kg (w.w.) in 1987 in pike from Lake Iso Valkjaervi, which is a clear-water seepage lake having no natural inlet or outlet. Variation in the activity concentrations of 137Cs in fishes in small forest lakes in the area receiving the highest deposition in Finland has remained large since the Chernobyl deposition. Interspecific differences in 137Cs levels of fish were consistent with their trophic position in the food webs. Ten-fold interlake differences in 137Cs contents of lake water were noted within the same municipality in 1987. In the bottom sediment of Lake Iso Valkjaervi, 95% of 137Cs was present in the uppermost 10 cm and about 70% in the uppermost 3 cm in 1992. The total amount of 137Cs detected in the sediment profile was only a quarter of the average deposition in the municipality of Lammi measured by Arvela et al. (1990). Average values for 137Cs in soil in the catchments of five lakes as Becquerels per unit area were clearly higher than the average value for the deposited 137Cs in the municipality of Lammi determined by Arvela et al. (1990). An aquatic plant, the yellow iris, was the most effective 137Cs accumulator of all the organisms

  12. Behavior of 131I and 137Cs in environments released from the Fukushima nuclear disaster

    Ohta, T.; Mahara, Y.; Kubota, T.; Igarashi, T.

    2011-12-01

    The devastating tsunami that caused by the great earthquake (M = 9.0) off the coast of northeastern Honshu on 11 March 2011 destroyed large coastal areas of Tohoku and north Kanto, Japan. Radionuclides, including 131I, 134Cs, and 137Cs, were released into the atmosphere from the Fukushima Daiichi plants. Concentration of levels of 131I, 134Cs, and 137Cs in Ibaraki Prefecture, Japan, released from the Fukushima Daiichi plant were investigated in the soil and precipitation. The concentrations of 131I and 137Cs in the soil from the surface to 1 cm depth in Ibaraki Prefecture were 9360-13,400 Bq/kg and 720-3250 Bq/kg, respectively. The concentration of 137Cs at this soil observation site originating from the Fukushima plant was 8.4 to 21 times that found locally after the Nagasaki atomic bomb explosion. Most of the 134Cs and 137Cs from rainwater were trapped by the surface soil and sand to a depth of 1 cm, whereas only about 30% of the 131I was collected by the surface soil, suggesting that 131I would move deeper than 137Cs and 134Cs. The 131I in the rainwater was in the anion exchangeable form, and all of it could be collected by anion exchangeable mechanisms, whereas 30% of the 131I that had passed through the soil could not be trapped by the anion exchange resin, suggesting that the chemical form of this 30% was in a changeable, organic-bound form. The 131I, 134Cs, and 137Cs that were absorbed on soil were difficult to be dissolved into water. As the half-life of 131I is short and 137Cs is strongly adsorbed on the surface soil and sand, these radionuclides would be unlikely to reach the groundwater before completely decaying; contamination of groundwater with 131I and 137Cs supplied from rainwater to the surface soil is therefore exceedingly unlikely. As the 137Cs is likely to migrate only 0.6 cm in 10 years, people living in the Fukushima and Kanto areas will be exposed to radiation from 137Cs in the surface soil and sand. For protection, surface soils and sands

  13. The spread of 137Cs by resuspension of contaminated soil in the urban area of Goiania

    Measurements regarding the population exposure were performed in Goiania after the radiological accident as well as studies on resuspension and redeposition of 137Cs in urban areas, on the contribution of soil splash to the 137Cs uptake by leafy vegetables and on the transfer of 137Cs from soil to chicken meat and eggs. Periodical street dust sampling was used to follow-up the spreading of the radionuclide in the city. The results do not indicate a measurable spreading of this radionuclide throughout the city from the contaminated areas, but resuspension can lead to significant local contamination of agricultural products, equipment, structures, etc. (author)

  14. Effects of ash recycling on the migration rate of 137Cs in forest soils

    Large areas of the eastern parts of central Sweden received as a result of the Chernobyl fallout considerable amount of radioactive caesium (137Cs) . From a physical and chemical point of view potassium (K) and Cs are rather similar, and uptake Of 137Cs from the soil by the plants is restricted because of high of K availability. This leads to that most of the 137Cs the soil is the large storage, only a small portion of the available 137Cs is circulated in the vegetation. Since only minute part of the total pool of 137Cs of the ecosystem is stored in the above ground part of the vegetation, extraction of bio-fuels only marginally relive the system from 137Cs. Recycling of wood-ash could in the future become a common feature in Swedish forestry. However, the use of bio-fuel leads to an increased concentration of 137Cs in the produced wood-ash by c. 40 times. This question, how wood-ash recycling affects the radiation climate in the forest is an aspect on wood-ash recycling have been recognised during recent years. The Swedish Radiation Protection Authority (SSI) has stated that the highest radioactivity that could be spread onto the forests is 5 kBq/ha. The effect on the vegetation content of 137Cs is an intricate interaction between the properties of the ash and the soil. The form in which 137Cs and K is stored in the ash could affect the release. In addition, soil pH and differences in turnover time between the two constituents affects the content of 137Cs in the vegetation. In case large amounts of K are released the uptake of 137Cs be blocked. It has been demonstrated that addition of KCl reduced the concentrations of 137Cs fungal fruit bodies by two thirds a lower effect was found after addition of 3 tonnes wood-ash. In another investigation showed that the activity of 137Cs did not increase the activity in vegetation, and in one case also lowered the activity, this despite the fact that the wood-ash contained 137Cs. In the present study the objective was to

  15. Factors controlling the spatiotemporal variation of 137Cs in seabed sediment off the Fukushima coast: implications from numerical simulations

    We used numerical simulations to investigate major controls on spatiotemporal variations of 137Cs activities in seabed sediments off the Fukushima coast during the first year after the Fukushima Daiichi Nuclear Power Plant accident. The numerical model we used includes 137Cs transfer between bottom water and sediment by adsorption and desorption, and radioactive decay. The model successfully reproduced major features of the observed spatiotemporal variations of 137Cs activities in sediments. The spatial pattern of 137Cs in sediments, which mainly reflected the history of 137Cs activities in bottom water overlying the sediments and the sediment particle size distribution, became established during the first several months after the accident. The simulated temporal persistence of the 137Cs activity in the sediments was due to adsorption of 137Cs onto the sediment mineral fraction having a long desorption timescale of 137Cs. The simulated total 137Cs inventory in sediments integrated over the offshore area, where most of the monitoring stations were located, was on the order of 1013 Bq; this value is consistent with a previous estimate based on observed data. Taking into account 137Cs activities in sediments in both the coastal area and in the vicinity of the power plant, the simulated total inventory of 137Cs in sediments off the Fukushima coast increased to a value on the order of 1014 Bq. - Highlights: • Variations of 137Cs in seabed sediments off the Fukushima coast are investigated. • Sediments record the history of 137Cs activities in the overlying bottom water. • Distribution of sediment grain size affects 137Cs activities in sediments. • Estimated total inventory of 137Cs in the sediments is on the order of 1014 Bq

  16. 137CS-determination in game meat from some hunting areas in lower Austria

    In 1986, the contamination of some regions in Austria by 137Cs, due to the Chernobyl accident was relatively high. Among other 137Cs is taken up by people by the consumption of game. In an area of Lower Austria which is relatively heavily contaminated by Chernobyl fallout since 1986 the 137Cs-contamination of meat of game-animals was measured every year. Clear differences arose in the load of the single game species whose causes just like the temporal changes are discussed. The highest 137Cs activity concentration was with 5243 Bq/kg measured on a wild boar. With this activity concentration an annual effective dose of only 0,06 mSv can be estimated for an annual average consumption of one kilogram meat of wild boar. (orig.)

  17. A comparison of {sup 137}Cs radioactivity in localized evergreen and deciduous plant species

    Rangel, R.C.

    1996-05-01

    A vegetation study at the Comanche Peak Steam Electric Station (CPSES) near Glen Rose, Texas was conducted in 1991 and 1992. The CPSES is a commercial nuclear power plant owned and operated by Texas Utilities Electric of Dallas, Texas. The US Nuclear Regulatory Commission (USNRC) requires the CPSES to routinely sample broadleaf vegetation in place of milk samples. Few commercial dairies exist in the vicinity. Broadleaf tree species are scarce because the climate and local limestone geology have produced a dry rolling hill topography. An evergreen juniper is the dominant tree species. Few broadleaves during the winter season have hindered year-round sampling. This study compares the environmental {sup 137}Cs concentrations between broadleaf and evergreen foliage at CPSES. Soil {sup 137}Cs concentrations from each vegetation location were also compared to the foliage {sup 137}Cs concentrations. The study`s objective was to determine if the deciduous and evergreen vegetation {sup 137}Cs concentrations are statistically the same.

  18. Effect of application timing of potassium fertilizer on root uptake of 137Cs in brown rice

    We have already reported that potassium fertilizer is effective to reduce radiocesium in brown rice. In this study, we tried to find the most appropriate timing for potassium fertilizer application during the rice cultivation period in terms of 137Cs concentrations in brown rice. The concentration of 137Cs in brown rice cultivated without application of potassium fertilizer was 32 Bq kg-1, while that with application of basal fertilizer including potassium was 5 Bq kg-1. The concentration of 137Cs in brown rice was increased with the late application timing. Therefore, application of potassium fertilizer in the early growing period reduced the uptake of 137Cs by rice plant from contaminated soils effectively. (author)

  19. 137Cs in fishes of the cooling-pond after the decommissioning the ChNPP

    Content of 137Cs in fishes of the ChNPP cooling-pond was studied during 1999 - 2006. It is established, that in the main fishes species of the cooling-pond there was no essential decrease of content of 137Cs. In Abramis brama (L.), Blicca bjoerkna (L.) and Ictalurus punctatus (Raf.) the contents of 137Cs to 2006 has not decreased in comparison to 1999 - 2000. In Alburnus alburnus (L.) the content of 137Cs in 2006 authentically exceeds those in 2000. Probably, the given phenomenon is caused by the reorganization of trophic circuits due to the change of temperature and hydrological parameters of the cooling-pond ecosystem as the result of decommissioning of ChNPP

  20. Soil 137Cs activity in a tropical deciduous ecosystem under pasture conversion in Mexico

    Soil profiles of 137Cs were measured in a tropical deciduous ecosystem under pasture conversion on the Pacific Coast of Mexico. Soil samples were taken from unperturbed forest, and from pasture plots following forest conversion. The average total 137Cs areal activity of non-eroded forest sites indicated a base level of 5 315 ± 427 Bq m-2. On average, total areal activity on hill-tops was significantly higher (range 10-47%) in the forest than in the pastures. A significant correlation was found between the total 137Cs areal activity and soil organic matter content (r2 = 0.16). This correlation can be explained by a soil physical-protection hypothesis. The redistribution of 137Cs in the landscape is explained by soil erosion processes. (author)

  1. A case study of the transfer of 137Cs to the human fetus and nursing infant

    A four-months pregnant woman was contaminated during an accident involving 137Cs from a teletherapy source that occurred in Brazil in September 1987. In vivo monitoring and analysis of 137Cs concentration in excreta samples (both urine and faeces) of the mother was performed. In vivo monitoring of the infant was conducted after birth. After birth, for about 90 days, which corresponds to most of the period of measurement, the infant was exclusively fed by mother's milk, which was also measured. Estimates of parameters associated with the retention and distribution of 137Cs relating to the metabolism of mother and infant were made. The results provide useful information for age-specific models describing the metabolism of 137Cs. (author)

  2. Floodplain data: ecosystem characteristics and /sup 137/Cs concentrations in biota and soil. [ORNL

    Van Voris, P.; Dahlman, R.C.

    1976-11-01

    Radiocesium (/sup 137/Cs) distribution was determined in soil, roots, ground vegetation, overstory, litter, mammals, feces, and insects for a floodplain ecosystem contaminated by radioactive wastes from Manhattan Project operations in 1944. The 2-ha research site was located on the ERDA reservation, Oak Ridge, Tennessee, in a drained holding pond between Oak Ridge National Laboratory and White Oak Lake. Maximum /sup 137/Cs concentrations in soil occurred near the old retention pond dam (84,400 pCi/g) and at the upper portion of the floodplain boundary (70,500 pCi/g). This bimodal distribution pattern of /sup 137/Cs was evident for all samples collected. Large amounts of data have been collected since the summer of 1974. This report documents the data on ecosystem characteristics and /sup 137/Cs concentrations in biota and soil.

  3. Influence of the Chernobyl fallout on 137Cs wine activities on the Rhone valley

    Influence of the Chernobyl fallout on 137CS wine activities on the Rhone valley. Some parts of the Rhone valley have been quite strongly, affected by the Chernobyl fallout, with 137Cs deposits sometimes higher than 20 000 Bq m-2. In those regions, most of agricultural surfaces are devoted to vineyards for famous vintages. This study shows that the consequences of the Chernobyl fallout in wine were visible but very weak. 137CS wine activities did not reached 1 Bq 1-1. Such limited consequences are linked to the date of the deposit, the first week of May 1986, at the beginning of vineyard plant foliar development. Since 1986, this activity has strongly decreased to be in 2000 close to those existing before the accident: some milli-becquerel per litre. 137Cs activities in soil, mainly contained within the 20 first centimeters, are weakly available for vineyard roots. (authors)

  4. Modelling the distribution of 90Sr and 137Cs in the Mediterranean Sea (MTPII-MATER)

    Within the frame of the MTPII-MATER project (MAST), the distribution of 90Sr and 137Cs in the Mediterranean Sea was modelled, as these radionuclides are useful tracers of water circulation. The Mediterranean Sea was divided into 81 boxes, corresponding to 21 regions, taking into account water mass circulation, bathymetry and data availability. Transfer rates were obtained from the MOM model run under MEDMEX conditions. The model was run with realistic inputs, which included weapons global fallout, Chernobyl 137Cs, nuclear industry and river runoff. It was observed that existing data are scarce, especially in the eastern Mediterranean. In general, model predictions agreed well with observations, showing maximum concentrations in surface waters and maxima due to global fallout (137Cs and 90Sr) and to the Chernobyl accident (137Cs only). (author)

  5. Floodplain data: ecosystem characteristics and 137Cs concentrations in biota and soil

    Radiocesium (137Cs) distribution was determined in soil, roots, ground vegetation, overstory, litter, mammals, feces, and insects for a floodplain ecosystem contaminated by radioactive wastes from Manhattan Project operations in 1944. The 2-ha research site was located on the ERDA reservation, Oak Ridge, Tennessee, in a drained holding pond between Oak Ridge National Laboratory and White Oak Lake. Maximum 137Cs concentrations in soil occurred near the old retention pond dam (84,400 pCi/g) and at the upper portion of the floodplain boundary (70,500 pCi/g). This bimodal distribution pattern of 137Cs was evident for all samples collected. Large amounts of data have been collected since the summer of 1974. This report documents the data on ecosystem characteristics and 137Cs concentrations in biota and soil

  6. A comparison of 137Cs radioactivity in localized evergreen and deciduous plant species

    A vegetation study at the Comanche Peak Steam Electric Station (CPSES) near Glen Rose, Texas was conducted in 1991 and 1992. The CPSES is a commercial nuclear power plant owned and operated by Texas Utilities Electric of Dallas, Texas. The US Nuclear Regulatory Commission (USNRC) requires the CPSES to routinely sample broadleaf vegetation in place of milk samples. Few commercial dairies exist in the vicinity. Broadleaf tree species are scarce because the climate and local limestone geology have produced a dry rolling hill topography. An evergreen juniper is the dominant tree species. Few broadleaves during the winter season have hindered year-round sampling. This study compares the environmental 137Cs concentrations between broadleaf and evergreen foliage at CPSES. Soil 137Cs concentrations from each vegetation location were also compared to the foliage 137Cs concentrations. The study's objective was to determine if the deciduous and evergreen vegetation 137Cs concentrations are statistically the same

  7. Body burden of fallout 137Cs in the inhabitants of Moscow in 1980-1983

    Several groups of people living in Moscow were measured for fallout 137Cs in 1980-1983. In vivo measurements of incorporated 137Cs were made with use of a whole-body counter. The minimum measurable activities of 137Cs were 37 and 17 Bq consequently for time of measurement 15 and 30 min. All persons measured were classified into four groups, personnel of whole-body counters laboratory, teenagers-sportsman, patients of a Moscow hospital (with heart and kidneys diseases) and normal adults-inhabitants of Moscow. The activity of 137Cs in the normal adults and patients was observed to decrease during the period of investigation. It was shown that by the end of 1983 the great majority of the results were similar and below the minimum measurable activity (for time of measurement 15 min)

  8. Plutonium as a chronomarker in Australian and New Zealand sediments: a comparison with (137)Cs.

    Hancock, G J; Leslie, C; Everett, S E; Tims, S G; Brunskill, G J; Haese, R

    2011-10-01

    The construction of high resolution chronologies of sediment profiles corresponding to the last 50-100 years usually entails the measurement of fallout radionuclides (210)Pb and (137)Cs. The anthropogenic radionuclide, (137)Cs, originating from atmospheric nuclear weapons testing can provide an important "first appearance" horizon of known age (1954-1955), providing much-needed validation for the sometimes uncertain interpretations associated with (210)Pb geochronology. However, while (137)Cs usually provides a strong signal in sediment in the northern hemisphere, total fallout of (137)Cs in the southern hemisphere was only 25% that of the north and the low activities of (137)Cs seen in Australian and New Zealand sediments can make its horizon of first appearance somewhat arguable. Low (137)Cs fallout also limited the size of the 1963-1964 fallout peak, a peak that is usually seen in northern hemisphere sediment profiles but is often difficult to discern south of the equator. This paper shows examples of the use of nuclear weapons fallout Pu as a chronomarker in sediment cores from Australia (3 sites) and New Zealand (1 site). The Pu profiles of five cores are examined and compared with the corresponding (137)Cs profiles and (210)Pb geochronologies. We find that Pu has significant advantages over (137)Cs, including greater measurement sensitivity using alpha spectrometry and mass spectrometric techniques compared to (137)Cs measurements by gamma spectrometry. Moreover, Pu provides additional chronomarkers associated with changes in the Pu isotopic composition of fallout during the 1950s and 1960s. In particular, the (238)Pu/(239+240)Pu activity ratio shows distinct shifts in the early 1950s and the mid to late 1960s, providing important known-age horizons in southern hemisphere sediments. For estuarine and near-shore sediments Pu sometimes has another significant advantage over (137)Cs due to its enrichment in bottom sediment relative to (137)Cs resulting from the

  9. Plutonium as a chronomarker in Australian and New Zealand sediments: a comparison with {sup 137}Cs

    Hancock, G.J., E-mail: gary.hancock@csiro.au [CSIRO Land and Water, Black Mountain Laboratories, GPO Box 1666, Canberra, ACT 2601 (Australia); Leslie, C. [CSIRO Land and Water, Black Mountain Laboratories, GPO Box 1666, Canberra, ACT 2601 (Australia); Everett, S.E.; Tims, S.G. [Department of Nuclear Physics, Research School of Physics and Engineering, The Australian National University, Building 57, Canberra, ACT 0200 (Australia); Brunskill, G.J. [84 Alligator Creek Road, Alligator Creek, Queensland 4816 (Australia); Haese, R. [Geoscience Australia, GPO Box 378, Canberra, ACT 2601 (Australia)

    2011-10-15

    The construction of high resolution chronologies of sediment profiles corresponding to the last 50-100 years usually entails the measurement of fallout radionuclides {sup 210}Pb and {sup 137}Cs. The anthropogenic radionuclide, {sup 137}Cs, originating from atmospheric nuclear weapons testing can provide an important 'first appearance' horizon of known age (1954-1955), providing much-needed validation for the sometimes uncertain interpretations associated with {sup 210}Pb geochronology. However, while {sup 137}Cs usually provides a strong signal in sediment in the northern hemisphere, total fallout of {sup 137}Cs in the southern hemisphere was only 25% that of the north and the low activities of {sup 137}Cs seen in Australian and New Zealand sediments can make its horizon of first appearance somewhat arguable. Low {sup 137}Cs fallout also limited the size of the 1963-1964 fallout peak, a peak that is usually seen in northern hemisphere sediment profiles but is often difficult to discern south of the equator. This paper shows examples of the use of nuclear weapons fallout Pu as a chronomarker in sediment cores from Australia (3 sites) and New Zealand (1 site). The Pu profiles of five cores are examined and compared with the corresponding {sup 137}Cs profiles and {sup 210}Pb geochronologies. We find that Pu has significant advantages over {sup 137}Cs, including greater measurement sensitivity using alpha spectrometry and mass spectrometric techniques compared to {sup 137}Cs measurements by gamma spectrometry. Moreover, Pu provides additional chronomarkers associated with changes in the Pu isotopic composition of fallout during the 1950s and 1960s. In particular, the {sup 238}Pu/{sup 239+240}Pu activity ratio shows distinct shifts in the early 1950s and the mid to late 1960s, providing important known-age horizons in southern hemisphere sediments. For estuarine and near-shore sediments Pu sometimes has another significant advantage over {sup 137}Cs due to its

  10. Long-term retention of (137)Cs in three forest soil types with different soil properties.

    Suchara, Ivan; Sucharová, Julie; Holá, Marie; Pilátová, Helena; Rulík, Petr

    2016-07-01

    Current (137)Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of (137)Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of (137)Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total (137)Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of (137)Cs in the soils was found to be in accordance with the estimated (137)Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of (137)Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of (137)Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current (137)Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher (137)Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing (137)Cs from the surrounding plots situated below neighbouring canopies. PMID:27085039

  11. Detritivores enhance the mobilization of {sup 137}Cs from leaf-litter

    Murakami, Masashi; Suzuki, Takahiro [Community Ecology Lab., Biology Course, Faculty of Science, Chiba University, Chiba, 263-8522 (Japan); Ishii, Nobuyoshi [National Institute of Radiological Sciences, Chiba, 263-8555 (Japan); Ohte, Nobuhito [Graduate School of Agricultural and Life Sciences, The University of Tokyo, Tokyo, 113-8657 (Japan)

    2014-07-01

    A large amount of radioactive material was released from the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident after the disastrous earthquake and subsequent tsunami of March 2011. Since most of the Japanese land area is covered by forest ecosystems, {sup 137}Cs was mostly deposited and accumulated on the land surface of forest. The fate of radioactive materials accumulated on the leaf litters should be conscientiously monitored to understand the future distribution and the spread to the surrounding landscapes. Because the accident took place on 11 March 2011, just before the bud-break of deciduous trees, the {sup 137}Cs are highly accumulated on the surface of leaf litter on the forest floor. This accumulated {sup 137}Cs had transferred to higher trophic organisms mainly through the detritus food chain. However, on the litter surface, {sup 137}Cs considered to be strongly and immediately fixed and highly immobilized. Decomposition processes in the forest floor can re-mobilise the nutritional elements which are contained within detritus and make them available for the organisms. In the present study, the feeding effect of detritivore soil arthropods on the mobilization of {sup 137}Cs from leaf litter was experimentally examined. Furthermore, the effect of detritivores on the plant uptake of {sup 137}Cs was examined by small-scale nursery experiment. Decomposition experiment in the small microcosms was performed using a larvae of Trypoxylus dichotomus, whichis a detritivores feeding on dead plant materials such as wood debris and leaf litters. Contaminated leaf litters were collected in a forest of the Kami-Oguni River catchment in the northern part of Fukushima Prefecture. The leaf litters at A0 layers which are highly contaminated by {sup 137}Cs were utilized for the experiment. The contaminated leaf litter was fed to the larvae for ten days. The litter with larvae excreta was washed by 2 M KCl and deionized water. The {sup 137}Cs concentration was measured

  12. Detritivores enhance the mobilization of 137Cs from leaf-litter

    A large amount of radioactive material was released from the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident after the disastrous earthquake and subsequent tsunami of March 2011. Since most of the Japanese land area is covered by forest ecosystems, 137Cs was mostly deposited and accumulated on the land surface of forest. The fate of radioactive materials accumulated on the leaf litters should be conscientiously monitored to understand the future distribution and the spread to the surrounding landscapes. Because the accident took place on 11 March 2011, just before the bud-break of deciduous trees, the 137Cs are highly accumulated on the surface of leaf litter on the forest floor. This accumulated 137Cs had transferred to higher trophic organisms mainly through the detritus food chain. However, on the litter surface, 137Cs considered to be strongly and immediately fixed and highly immobilized. Decomposition processes in the forest floor can re-mobilise the nutritional elements which are contained within detritus and make them available for the organisms. In the present study, the feeding effect of detritivore soil arthropods on the mobilization of 137Cs from leaf litter was experimentally examined. Furthermore, the effect of detritivores on the plant uptake of 137Cs was examined by small-scale nursery experiment. Decomposition experiment in the small microcosms was performed using a larvae of Trypoxylus dichotomus, whichis a detritivores feeding on dead plant materials such as wood debris and leaf litters. Contaminated leaf litters were collected in a forest of the Kami-Oguni River catchment in the northern part of Fukushima Prefecture. The leaf litters at A0 layers which are highly contaminated by 137Cs were utilized for the experiment. The contaminated leaf litter was fed to the larvae for ten days. The litter with larvae excreta was washed by 2 M KCl and deionized water. The 137Cs concentration was measured by germanium detectors (Seiko EG and G). As a

  13. Factors Effecting Adsorption of 137 Cs in Marine Sediment Samples in Marine Sediment Samples from the Upper Gulf of Thailand

    Contamination of 137Cs in sediment is a far more serious problem than in water because sediment is a main transport factor of 137Cs to the aquatic environmental. Most of 137Cs in water could be accumulated in sediment which has direct effect to benthos. This study focused on factors effecting the adsorption of 137Cs in marine sediment samples collected from four different estuary sites to assess the transfer direction of 137Cs from water to sediment that the study method by treat 137Cs into seawater and mixed with different sediment samples for 4 days. The result indicated that properties of marine sediment (cation exchange capacity (CEC), organic matter, clay content, texture, type of clay mineral and size of soil particle) had effects on 137Cs adsorption. CEC and clay content correlated positively with the accumulation of 137Cs in the marine sediment samples. On the other hand, organic matter in sediment correlated negatively with the accumulation of 137Cs in samples. The study of environmental effects (pH and potassium) found that the 137Cs adsorption decreased when concentration of potassium increased. The pH effect is still unclear in this study because the differentiation of pH levels (6, 7, 8.3) did not have effects on 137Cs adsorption in the samples.

  14. Toxicity of injected 137CsCl in Beagle dogs. XI

    Studies of the metabolism, dosimetry and effects of intravenously administered 137CsCl in the Beagle dog are being conducted to aid in assessing the biologic consequences of exposure to 137Cs that might occur in the event of certain nuclear accidents. Effects of the chronic, relatively uniform whole-body exposure produced by 137Cs are being compared with other diverse radiation dose patterns resulting from inhalation of radioactive aerosols. Sixty-six dogs were entered into the study: six with a mean initial 137Cs body burden of 3780 μCi/kg and five groups of 12 dogs each with mean initial 137Cs body burdens of 2820, 1940, 1420, 970 and 0 μCi/kg. Twenty-two of the dogs injected with 137CsCl have died: 11 with cumulative whole-body doses of 860 to 1400 rads died from 19 to 81 days after injection with severe bone marrow damage and resultant pancytopenia; four with cumulative whole-body doses of 690 to 1900 rads have died between 2471 and 3386 days post injection with neurofibrosarcoma of the liver, dermal mast cell tumor, hemangiosarcoma of the right atrium, and squamous cell carcinoma of the maxillary sinus and soft palate; seven with cumulative doses of 840 to 2200 rads from 693 to 3529 days after injection with shock, aspiration pneumonia, severe arthritis, renal amyloidosis, congestive heart failure, leiomyoma of bladder and urethra, and brain and spinal cord edema. Four control dogs have died: one at 647 days with auto-immune hemolytic anemia, one at 2442 days with renal amyloidosis, one at 3088 days with disseminated complex mammary adenocarcinoma and one at 3265 days with chronic interstitial nephritis. Serial observations are continuing on the 32 137CsCl injected dogs and eight control dogs. The 137CsCl injected dogs now alive have cumulative whole-body doses of 550 to 1500 rads from 3508 to 3762 days after injection

  15. 137 Cs soil contamination of Techa river flood plain near village Muslyumovo

    The results of measuring soil contamination with 137 Cs in 16-km zone of the Techa river flood plain near the Muslyumovo village of the Chelyabinsk region are presented. The measurements are performed in 1995-1996. Maps for the 137 Cs buildup distribution in soils of the half-kilometer areas along the river branch are plotted. Total amount and area of contaminated flood plain are estimated for these zones

  16. Accumulation of 137Cs in Brazilian soils and its transfer to plants under different climatic conditions

    The spatial distribution and behaviour of the global fallout 137Cs in the tropical, subtropical and equatorial soil-plant systems were investigated at several upland sites in Brazil selected according to their climate characteristics, and to the agricultural importance. To determine the 137Cs deposition density, undisturbed soil profiles were taken from 23 environments situated between the latitudes of 02oN and 30oS. Sampling sites located along to the equator exhibited 137Cs deposition densities with an average value of 219 Bq m-2. Extremely low deposition densities of 1.3 Bq m-2 were found in the Amazon region. In contrast, the southern part of Brazil, located between latitudes of 20oS and 34oS, exhibited considerably higher deposition densities ranging from 140 Bq m-2 to 1620 Bq m-2. To examine the 137Cs soil-to-plant transfer in the Brazilian agricultural products, 29 mainly tropical plant species, and corresponding soil samples were collected at 43 sampling locations in nine federal states of Brazil. Values of the 137Cs concentration factor plant/soil exhibited a large range from 0.020 (beans) to 6.2 (cassava). Samples of some plant species originated from different collecting areas showed different concentration factors. The 137Cs content of some plants collected was not measurable due to a very low 137Cs concentration level found in the upper layers of the incremental soils. Globally, the soil-to-plant transfer of 137Cs can be described by a logarithmic normal distribution with a geometric mean of 0.3 and a geometric standard deviation of 3.9

  17. 137Cs and 90Sr aerosol-carriers origination when welding radioactively contaminated metal structures

    The results of research of main parameters of welding process influence to 137Cs and 90Sr radionuclides transition regularity in a welding aerosol are demonstrated. The 137Cs specific activity in welding aerosol decreases according to power law with lessening of surface activity of plates being welded on, and depends on content of electrode cover and does not depend on welding heat input. Respirable fraction activity of welding aerosol exceeds at 20 - 30 % the welding aerosol activity as a whole.

  18. Inventory and vertical migration of 137Cs in Spanish mainland soils

    In this study the total activity of 137Cs deposited per unit area over the Spanish peninsular territory was analysed using a 150 x 150 km2 mesh grid, with samples taken from 29 points. The deposited activities ranged between 251 and 6074 Bq/m2. A linear relationship was obtained between these values and the mean annual rainfall at each sampling point which allowed a map to be drawn, using GIS software, which shows the distribution of total deposited 137Cs activity across the Spanish mainland. At twelve of these sampling points the vertical migration profile of 137Cs was obtained. These profiles are separated into two groups with different behaviour, one of which includes clay and loam soils and the other containing sandy soils. For both groups of profiles the parameters of the convective-diffusive model, which describes the vertical migration of 137Cs in the soil, v (apparent convection velocity) and D (apparent diffusion coefficient) were calculated. - Highlights: → Measured the 137Cs activity in Spanish mainland, being within a range of [251, 6074] Bq/m2, with a mean value of 1726 Bq/m2. → Establishment of the 137Cs background by means of a 137Cs inventory map showing its distribution in the Spanish mainland. → 137Cs shows two different behaviour tendencies in soil depending on it. → The parameters which govern the applied model have been obtained for the analysed profiles. → Analysed those parameters, the two tendencies have been reflected in the obtained values.

  19. 90Sr and 137Cs in higher aquatic plants of the Chernobyl NPP exclusion zone

    The content of 90Sr and 137Cs radionuclides in higher aquatic plants of water object within Chernobyl NPP exclusion zone has been analysed. Biodiversity of phytocenose was studied and species-indicators of radioactive contamination were revealed. The seasonal dynamics of radionuclide content in macrophytes was studied and the role of main aquatic plant clumps in processes of 90Sr and 137Cs distribution in abiotic component of biohydrocenose was demonstrated

  20. [90Sr and 137Cs in higher aquatic plants of the Chernobyl nuclear plant exlusion zone

    Gudkov, D I; Derevets, V V; Kuz'menko, M I; Nazarov, A B

    2001-01-01

    The content of radionuclides 90Sr and 137Cs in higher aquatic plants of water objects within Chernobyl NPP exclusion zone has been analysed. Biodiversity of phytocenose was studied and species-indicators of radioactive contamination were revealed. The seasonal dynamics of radionuclide content in macrophytes was studied and the role of main aquatic plant clumps in processes of 137Cs and 90Sr distribution in abiotic component of biohydrocenose was demonstrated. PMID:11402559

  1. Toxicity of injected 137CsCl in beagle dogs. IX

    Studies on the metabolism, dosimetry and effects of intravenously administered 137CsCl in the Beagle dog are being conducted to aid in assessing the biologic consequences of exposure to 137Cs such as occurs in the event of certain nuclear accidents. Effects of the chronic, relatively uniform whole-body exposure produced by 137Cs are being compared with other diverse radiation dose patterns resulting from inhalation of radioactive aerosols. Sixty-six dogs were entered into the study: six with a mean initial 137Cs body burden of 3780 μCi/kg and five groups of 12 dogs each with mean initial 137Cs body burdens of 2820, 1940, 1420, 970 and 0 μCi/kg. Seventeen of the dogs injected with 137CsCl have died: 11 at 19 to 81 days after injection and cumulative whole-body doses of 860 to 1400 rads died with severe bone marrow damage and resultant pancytopenia; two at 2471 and 2707 days after injection and cumulative doses of 690 and 1800 rads with a neurofibrosarcoma of the liver and a mast cell tumor of the skin; four at 693 to 2148 days after injection and cumulative doses of 840 to 2000 rads with shock, aspiration pneumonia, severe arthritis and renal amyloidosis. Two control dogs died; one at 647 days with auto-immune hemolytic anemia and one at 2442 days with renal amyloidosis. Serial observations are continuing on the 37 137CsCl dogs and 10 control dogs. The 137CsCl dogs now alive have cumulative whole-body doses of 550 to 2200 rads at 2777 to 3031 days after injection

  2. Toxicity of injected 137CsCl in beagle dogs. X

    Studies on the metabolism, dosimetry and effects of intravenously administered 137CsCl in the Beagle dog are being conducted to aid in assessing the biologic consequences of exposure to 137Cs such as occurs in the event of certain nuclear accidents. Effects of the chronic, relatively uniform whole-body exposure produced by 137Cs are being compared with other diverse radiation dose patterns resulting from inhalation of radioactive aerosols. Sixty-six dogs were entered into the study: six with a mean initial 137Cs body burden of 3780 μCi/kg and five groups of 12 dogs each with mean initial 137Cs body burdens of 2820, 1940, 1420, 970 and 0 μCi/kg. Eighteen of the dogs injected with 137CsCl have died: 11 from 19 to 81 days after injection and cumulative whole-body doses of 860 to 1400 rads died with severe bone marrow damage and resultant pancytopenia; two at 2471 days and at 2707 days after injection and cumulative doses of 690 and 1800 rads with a neurofibrosarcoma of the liver and a mast cell tumor of the skin; five from 693 to 3162 days after injection and cumulative doses of 840 to 2000 rads with shock, aspiration pneumonia, severe arthritis, renal amyloidosis and congestive heart failure. Three control dogs died; one at 647 days with auto-immune hemolytic anemia, one at 2442 days with renal amyloidosis and one at 3088 days with disseminated complex mammary adenocarcinoma. Serial observations are continuing on the 36 137CsCl dogs and nine control dogs. The 137CsCl dogs now alive have cumulative whole-body doses of 550 to 2200 rads from 2777 to 3031 days after injection

  3. 137Cs: A Widely Used and Validated Medium Term Soil Tracer

    Radioactive Caesium-137 (137Cs) is found globally in the environment due to fallout after nuclear weapon testing in the fifties and sixties, and nuclear accidents in the more recent past. The properties and particular features of 137Cs (half-life of about 30 years), such as its strong adsorption to soil particles, make it an exceptional and the most widely used soil tracer for studying soil movement processes. The 137Cs method that possesses a number of major advantages over traditional approaches to document erosion and deposition rates, provides estimates of soil redistribution averaged over a period of several decades. It has been employed to study soil redistribution under different agro-ecological conditions in many different areas of the world. 137Cs has been also used in soil erosion investigations over a wide range of geographic scales, extending from experimental plots, through fields of a few hectares to small watersheds of several km2. This method has been validated by many international peer-reviewed studies that compared erosion rates obtained with 137Cs, other tracers, direct measurements at various scales and/or traditional soil erosion modelling. Significant progress has been made in harmonizing protocols for application of 137Cs-based soil erosion research through cooperation of specialist teams and coordination by the International Atomic Energy Agency (IAEA). The development, refinement and calibration of the 137Cs method have provided a universal and mature tool to quantify soil redistribution rates in a range of natural and agro-ecosystems, and have paved the way for a wider application of the technique, particularly in assessing the effectiveness of soil conservation technologies in controlling or mitigating soil erosion and associated degradation processes. This paper explains the fundamental principles of the use of fallout radionuclides for soil erosion assessments based on the example of 137Cs. (author)

  4. Modelling of 137Cs behaviour in the soil-plant system following the application of ameliorants

    A set of countermeasures aimed at reducing 137Cs uptake by plant products includes agrochemical measures based on changes in the soil properties after the application of ameliorants. The dynamic models for studying the effect of the application of potassium fertilizers and dolomite powder on 137Cs accumulation in plants are presented. Conceptual approaches to the development of models are based on the identification of mechanisms governing a complex of physico-chemical processes in soil after the use of ameliorants. The following assumptions were used in the development of models: - dynamics of 137Cs distribution in each soil layer depends on the sorption processes characterized by different time to achieve quasi-equilibrium (exchangeable uptake and fixation by clay minerals) as well as on vertical migration process; - change in 137Cs content in soil solution results from the radionuclide sorption on selective and nonselective exchange sites; - uptake of extra amounts of K+ and Ca2+ in soil solution produces effect on processes of 137Cs exchangeable sorption and initiate specific processes responsible for 137Cs fixation in the crystal lattice of clay minerals; - Ca2+ and K+ cations have a competing effect on 137Cs uptake by plants from soil solution, which along with the fixation processes, causes lower accumulation of this radionuclide by plants during the application of ameliorants. The developed models were parameterized for soils of the coniferous forest located in the Bryansk region in area suffered from the radioactive fallout after the Chernobyl accident. Effects of ameliorants and time of their application on 137Cs behaviour in the soil-plant system are assessed. The contribution of soil chemical and biological processes to the decrease in the radionuclide uptake by plants is estimated. (author)

  5. Study of relation between 137Cs soil-to-plant transfer factor and basic soil properties

    Experiments are reviewed in which along with the determination of the 137Cs soil-to-plant transfer factors, the basic properties of soils were determined. The basic properties of soils were completely determined only in a small number of experimental studies. In the said experiments, a multi-parameter regression analysis was used to find a regression equation suitable for reliable forecast of 137Cs content in plants according to the properties of soils. (author). 7 tabs., 34 refs

  6. Peculiarities of 137Cs translocation in higher plants under environmental and laboratory conditions

    Accumulation of technogenic 137Cs in higher plant roots and above-ground part and comparison of 137Cs and 40K transfer from roots to the above-ground part of plant as well as distribution within above-ground part of plant under environmental conditions were investigated. Parallely, the results of the investigations of 137Cs accumulation in the roots and shoots of test-organism Lepidium sativum L. in the model hydroponic system aqueous solution-solid phase-plant were analyzed. Peculiarities of transfer of this radionuclide from roots to shoots during the entire plant growing period under experimental conditions were determined. 137Cs activity in the tested plants of meadow ecotop was on an average 6-fold lower than in the plants of swamp and 10-fold lower than in the plants of forest ecotop. Differences in 137Cs and 40K transfer from roots to the above-ground part of plant and their distribution in plants indicate particular biological metabolism of these radionuclides in plants. Increased levels of 137Cs in soil practically did not affect the 40K transfer from roots to the above-ground part of plants. The results of investigations under natural and laboratory conditions show that increasing contamination of growth medium with 137Cs caused higher accumulation of this radionuclide in roots but its transfer from roots to the above-ground part of plant decreased or changed insignificantly. 137Cs transfer from roots to above-ground part under natural (Artemisia vulgaris) and laboratory (Lepidium sativum) conditions was rather similar. (authors)

  7. Phytoremediation of 137Cs from low level nuclear waste using Catharanthus roseus

    Remediation of radionuclides has been carried out using the phytoremediation technology. The green plants have been screened for the uptake potential of radionuclide and found that Catharanthus roseus has the high potential for radionuclides in particular 137Cs. Low level nuclear waste (LLNW) collected from effluent treatment plant, BARC has been characterized for physico-chemical and the presence of traces of radionuclides. LLNW was spiked with 3.7 x 104 kBqL-1 activity level of 137Cs. The plants of C. roseus were grown in (i) LLNW, (ii) 137Cs spiked LLNW and (iii) with the control. The radio activities were measured in the solution at the intervals of 0, 1, 2, 3, 6, 8 and 15 days in triplicate set of the experiment. The plants were harvested after the growth. The depletion of 137Cs in LLNW was found to be 19, 21, 24, 38, 60 and 76% at intervals of 1, 2, 3, 6, 8 and 15 days, respectively. The bio-accumulation of 137Cs has been measured in the roots and shoots of the harvested plants. The activity of 137Cs was found higher in shoots (998 kBq g-1 dw) as compared to the roots (735 kBq g-1 dw). The uptake of radionuclide-137Cs, bio-accumulation in the shoot via the active transport from the root, shows the high efficiency and potentiality of C. roseus for the remediation of radionuclide. The bio-accumulation of 137Cs in the shoot will remediate the radionuclide contamination from LLNW. C. roseus can also be made applicable for effective remediation of radionuclides present in the LLNW. (author)

  8. 137Cs in puddle sediments as timescale tracer in urban environment

    The 137Cs-based chronological approach is suggested to identify the age of urban landscapes and the chronology of pollution of soil in residential areas. Three main pivot points constitute the basis of the chronological approach: beginning of the Atomic Era in 1945, the maximum input in 1963 and the Chernobyl accident in 1986. Application of 137Cs as a timescale tracer was tested on the example of Ekaterinburg, a city in the Middle Urals region of Russia. The sampling of recent urban sediments of micro water bodies (puddles) was carried out in 210 locations in 2007–2010. The concentrations of Pb, Zn, Cu, Ni, Co, Mn and Fe, and activity concentrations of 137Cs were measured. It was found that the 137Cs concentrations in the puddle sediments correlated with the age of surrounding buildings determined by the year of construction. The correlations between the concentrations of metals and 137Cs in the puddle sediments identified the major pollutants of the urban area, assessing their background concentrations and obtaining the average annual inputs. - Highlights: • The approach to assess age of landscape and chronology of heavy metal pollution of urban environment is suggested. • Technogenic isotope 137Cs is used as a timescale tracer. • The puddle sediments reflect the recent pollution of urban soil. • The approach allows identifying the pollutants, assessing their background values, and obtaining the average annual input of pollutants

  9. Distribution of {sup 137}Cs in water leachates of forest humus

    Passeck, U.; Zech, W. [Bayreuth Univ. (Germany); Lindner, G. [Fachhochschule Coburg (Germany)

    1995-12-31

    The distribution of {sup 137}Cs in water extracts of organic layers of forest soils was investigated using an ultrafiltration method. Samples were taken from two sites in the Bavarian Alps. The different horizons of the organic layers were extracted by column elution with water and 50 mmol/litre CsCl solution. Water extracts were fractionated using membranes with the molecular weight cutoff of 500, 1000 and 3000 Dalton to determine the molecular weight distribution of dissolved organic carbon (DOC). The activity of {sup 137}Cs associated with the different DOC-fractions was measured by direct gammaspectrometry. Cesium-137 in the fraction smaller than 500 Dalton was defined as `ionic`. The results indicated a change of the binding sites depending on the degree of decomposition and humification in the profile. Organic bound {sup 137}Cs was identified in all extracts. High mobilities of DOC and {sup 137}Cs were observed in the same horizons, fractionation showed then low-molecular-weight DOC and {sup 137}Cs mainly in ionic form. In horizons with high-molecular-weight DOC the portion of organic bound {sup 137}Cs ranged up to 40%. (author).

  10. The feature and distribution of 137Cs in the forest soil

    The 137Cs concentration in an undisturbed upper layer of naked land in Fukuoka Prefecture decreased exponentially from 1969 to 1999 with the apparent half-life of 7 years. The ratio of 137Cs concentration in the lower layer of the soil to that in the upper layer was about 1/5. The concentration of 137Cs, 40K, and stable Cs and the soil profile consisting of loss on ignition, pH, and electric conductivity were determined in the 48 samples collected in the forests and the neighboring naked land from 1991 to 1998. The 137Cs concentration in the forest soils ranged from 1 to 424 Bq/kg dry wt, 131 Bq/kg dry wt on average, although 137Cs was hardly detected in the naked soil around the forest. There was no regional difference in the distribution of the 137Cs concentration, and it varied with pH and electric conductivity in the soil. Further, it tended to be higher in the deciduous woodland than in the evergreen woodland. (author)

  11. 137Cs and 40K in the flesh of Pacific albacore, 1964-1974

    Concentrations of 137Cs in the flesh of albacore tuna caught off the California coast during the last 10 yr decreased by a considerably smaller factor than did corresponding values reported for atmospheric fallout. Between 1965 and 1974, average tissue concentrations decreased steadily from 90 to approx. 40pCi/wet kg, which suggests an effective half-time for 137Cs in the upper layer of the eastern North Pacific of about 1 decade. Values for natural 40K, which was measured at the same time, averaged 3300pCi/wet kg. The 1965 mean concentrations of 137Cs in albacore from four widely separated fisheries in the Northern Hemisphere agreed within a factor of two, ranging from 50 to 90pCi/wet kg. In contrast, specimens from South Pacific fishery based at American Samoa averaged only 14pCi/wet kg. Surface seawater collected around Tutuila Island averaged 0.085pCi/l. 137Cs, in good agreement with measurements made a year later over a much wider area of the South Pacific. No larger variations in flesh concentrations of 137Cs or 40K were observed as a function of tuna size, species, portion of the body sampled or cooking. Thus, radioanalysis of canned tuna may be an efficient method of following major changes in 137Cs contamination of upper layers of the world ocean. (author)

  12. The 137Cs accumulation by forest-derived products in the Gomel region

    This paper reports basic features of the 137Cs uptake by forest-derived products in the Gomel region. Even with the soil contamination density of 37 kBq m−2 the radionuclide contents in 20–30% of mushrooms and berries were found to be higher than the admissible levels. The 137Cs contamination density of soil, site type and meteorological parameters were observed as the major factors which govern the radiocaesium uptake by mushrooms and berries. The 137Cs contents in forest-derived products were found to increase directly with the soil contamination density. Bilberries (Vaccinium myrtillus) growing on different site types differed significantly in the 137Cs content. It was also determined that statistically significant differences in the 137Cs radioactivity of forest foods growing on different natural sites were governed by the factor designated in the current study by “territorial”. The differences are to be accounted for both by forms of the Chernobyl fallout and by the natural and climatic conditions determining variations in the availability of radionuclides in the soil. In dry years the 137Cs concentrations in some mushroom species were higher than in normal years

  13. Influence on the mouse immune system of chronic ingestion of {sup 137}Cs

    Bertho, Jean-Marc; Faure, Marie-Cecile; Louiba, Sonia; Tourlonias, Elie; Stefani, Johanna; Siffert, Baptiste; Paquet, Francois; Dublineau, Isabelle, E-mail: Jean-marc.bertho@irsn.fr [IRSN, Laboratoire de Radiotoxicologie Experimentale, Fontenay aux Roses (France)

    2011-03-01

    The aim of this work was to determine the possible occurrence of damage to the immune system during the course of chronic ingestion of {sup 137}Cs. BALB/C mice were used, with {sup 137}Cs intake via drinking water at a concentration of 20 kBq l{sup -1}. Adults received {sup 137}Cs before mating and offspring were sacrificed at various ages between birth and 20 weeks. Phenotypic analysis of circulating blood cells and thymocytes did not show any significant modification of immune cell populations in animals ingesting {sup 137}Cs as compared with control animals, with the exception of a slight increase in Treg percentage at the age of 12 weeks. Functional tests, including proliferative response to mitogens such as phytohaemagglutinin, response to alloantigens in mixed lymphocyte reaction and immunoglobulin response to vaccine antigens such as tetanus toxin and keyhole limpet haemocyanin did not show any significant functional modification of the immune system in {sup 137}Cs-ingesting animals as compared with control animals. Overall, our results suggest that chronic ingestion of a low concentration of {sup 137}Cs in drinking water in the long term does not have any biologically relevant effect on the immune system.

  14. A survey of 90Sr and 137Cs activity levels of retail foods in Japan

    A comprehensive survey was conducted on 90Sr and 137Cs activity levels in retail foods purchased from retail markets all over Japan during the period 1989-1994, and the annual effective dose equivalent due to dietary ingestion was estimated. The concentrations of 90Sr and 137Cs in the food samples were determined using γ-ray spectrometry and the radiochemical method. The following were clarified by this study: (1) The 90Sr and 137Cs activity concentration levels were below 1 Bq kg-1 for almost all food samples except for the dried foods. (2) The activity concentration levels of 90Sr and 137Cs in foods of animal origin were different from those of plant origin. Generally, the former had higher 137Cs and lower 90Sr activity concentrations than the latter. (3) The mean and maximum values of the annual effective dose equivalent from a dietary intake of 90Sr and 137Cs by the consumption of retail foods were estimated to be as low as 1·3 and 4·1 μSv, respectively. (Copyright (c) 1998 Elsevier Science B.V., Amsterdam. All rights reserved.)

  15. Monitoring 137Cs and 134Cs at marine coasts in Indonesia between 2011 and 2013

    Highlights: • In response to the Japan Fukushima Daiichi nuclear accident. • The monitoring have been carried out in some Indonesia coasts. • 137Cs in the eastern and western Indonesia coasts originated from global fallout. - Abstract: Environmental samples (seawater, sediments and biota) were collected along the eastern and western Indonesian coasts between 2011 and 2013 to anticipate the possible impacts of the Fukushima radioactive releases in Indonesia. On the eastern coasts (south and north Sulawesi), the 137Cs concentrations in the seawater and sediments were 0.12–0.32 Bq m−3 and 0.10–1.03 Bq kg−1, respectively. On the western coasts (West Sumatra, Bangka Island, North Java, South Java and Madura island), the 137Cs concentrations in the seawater and sediments were 0.12–0.66 Bq m−3 and 0.19–1.64 Bq kg−1, respectively. In general, the 137Cs concentrations in the fish from several Indonesian coasts were 137Cs concentrations in mollusk, crab and prawn were 10.65–38.78, 4.02 and 6.16 mBq kg−1, respectively. 134Cs was not detected in the seawater, sediments or biota. Thus, it was concluded that 137Cs on the eastern and western Indonesian coasts originated from global fallout

  16. Sampling soils for 137Cs using various field-sampling volumes

    The sediments from a liquid effluent receiving area at the Los Alamos National Laboratory and soils from intensive study area in the fallout pathway of Trinity were sampled for 137Cs using 25-, 500-, 2500-, and 12 500-cm3 field sampling volumes. A highly replicated sampling program was used to determine mean concentrations and inventories of 137Cs at each site, as well as estimates of spatial, aliquoting, and counting variance components of the radionuclide data. The sampling methods were also analyzed as a function of soil size fractions collected in each field sampling volume and of the total cost of the program for a given variation in the radionuclide survey results. Coefficients of variation (CV) of 137Cs inventory estimates ranged from 0.063 to 0.14 for Mortandad Canyon sediments, where CV values for Trinity soils were observed from 0.38 to 0.57. Spatial variance components of 137Cs concentration data were usually found to be larger than either the aliquoting or counting variance estimates and were inversely related to field sampling volume at the Trinity intensive site. Subsequent optimization studies of the sampling schemes demonstrated that each aliquot should be counted once, and that only 2 to 4 aliquots out of an many as 30 collected need be assayed for 137Cs. The optimization studies showed that as sample costs increased to 45 man-hours of labor per sample, the variance of the mean 137Cs concentration decreased dramatically, but decreased very little with additional labor

  17. Effect of 137Cs on spring wheat and transfer in soil-wheat systems

    The study emphasized on the effect of 137Cs on spring wheat and transfer factors in soil-wheat system. The results show that the spring wheat grown normally under the experimental conditions and no adverse effects appeared; the absorption trends of 137Cs by spring wheat were in the order of Dayawan soil > Qinshan soil > Beijing soil; the specific radioactivity of 137Cs in wheat increased in the magnitude order varying with the radioactivity of 137Cs applied in the soils and the relationship was significant difference in positive; the transfer factor (TF) of 137Cs in the soil-plant systems varied with the characteristic of soil and the range was within n x 10-2- n x 100 in the same activity of contamination; in the same soil-plant system the TF value increased varying with the radioactivity of 137Cs contamination in the range of 2.2 x 10-2 - 5.4 x 10-2 for Beijing soil plant system, 1.04 - 2.09 for Dayawan soil-plant system and 0.51 - 1.21 for Qinshan soil-plant system

  18. Influence on the mouse immune system of chronic ingestion of 137Cs

    The aim of this work was to determine the possible occurrence of damage to the immune system during the course of chronic ingestion of 137Cs. BALB/C mice were used, with 137Cs intake via drinking water at a concentration of 20 kBq l-1. Adults received 137Cs before mating and offspring were sacrificed at various ages between birth and 20 weeks. Phenotypic analysis of circulating blood cells and thymocytes did not show any significant modification of immune cell populations in animals ingesting 137Cs as compared with control animals, with the exception of a slight increase in Treg percentage at the age of 12 weeks. Functional tests, including proliferative response to mitogens such as phytohaemagglutinin, response to alloantigens in mixed lymphocyte reaction and immunoglobulin response to vaccine antigens such as tetanus toxin and keyhole limpet haemocyanin did not show any significant functional modification of the immune system in 137Cs-ingesting animals as compared with control animals. Overall, our results suggest that chronic ingestion of a low concentration of 137Cs in drinking water in the long term does not have any biologically relevant effect on the immune system.

  19. Deposition of atmospheric (137)Cs in Japan associated with the Asian dust event of March 2002.

    Fujiwara, Hideshi; Fukuyama, Taijiro; Shirato, Yasuhito; Ohkuro, Toshiya; Taniyama, Ichiro; Zhang, Tong-Hui

    2007-10-01

    Considerable deposition of (137)Cs was observed in the northwestern coastal area of Japan in March 2002. Since there were no nuclear explosions or serious nuclear accidents in the early 2000s, transport of previously contaminated dust appears to be the only plausible explanation for this event. In March 2002, there was a massive sandstorm on the East Asian continent, and the dust raised by the storm was transported across the sea to Japan. This dust originated in Mongolia and northeastern China, in an area distant from the Chinese nuclear test site at Lop Nor or any other known possible sources of (137)Cs. Our radioactivity measurements showed (137)Cs enrichment in the surface layer of grassland soils in the area of the sandstorm, which we attributed to accumulation as a result of past nuclear testing. We suggest that the grassland is a potential source of (137)Cs-bearing soil particles. Since the late 1990s, this area has experienced drought conditions, resulting in a considerable reduction of vegetation cover. We attribute the prodigious release of (137)Cs-bearing soil particles into the atmosphere during the sandstorm and the subsequent deposition of (137)Cs in Japan to this change. PMID:17604085

  20. A new approach to analysis of relationships between 137Cs activity concentrations in forest soil horizons

    The measurements results of 137Cs activity concentrations in forest soil profiles are discussed. In studies some simplifications were considered. First of them concerns disregarding of soil subtype in data analysis. However initially this parameter was considered in data analysis, it was finally ignored. The second assumption drops information about specific soil horizon. Description of 137Cs accumulation is based on relationships between its relative activity concentrations in soil layers. The model formulation was based on the results of exploratory data analysis of the relative 137Cs activity concentrations. In studies the methods designed for compositional data analysis were used. The results of analysis showed that the relationships between the relative activity concentrations of 137Cs in soil layers, due to their nature, might be divided into two groups. The first of them concerns layers located close to soil surface. The relative activity concentrations of 137Cs in these layers are proportional to each other, and distribution mechanism of cesium within them has the characteristics of the process leading to thermodynamic equilibrium. The second group is related to layers that are located deeper. The calculation results suggest lack of thermodynamic equilibrium between these layers and layers situated above. Utilization of a linear model for description of changes in relative activity concentrations of 137Cs in deeper layers supposes that these changes occur much slower than in layers lying above. (author)

  1. Dietary 137Cs and 90Sr in Finland in 1960 - 2000

    Domestic animal products dominated dietary intake of 137 Cs in 1960 2000. Freshwater fish and vegetable products of agricultural origin were almost equal contributors of 137 Cs to the diet. Wild foods received from forests, assessed using a simple approach, were also non-negligible sources of 137 Cs. Marine and brackish-water fishes, although of low activity concentration of 137 Cs compared to freshwater fishes, added to the ingestion dose through a higher consumption rate. Sources of dietary 137 Cs during the period of atmospheric nuclear fallout from weapon tests differed from the post-Chernobyl time. Agricultural produce then seemed to dominate the 137 Cs received via the Finnish diet more than after the Chernobyl accident. Subsequent growth periods of considerable stratospheric fallout made the pathways from vegetation to human diet important in the 1960s. Strontium 90 is mobile in soils for long periods of time. However, it has not been a significant dietary nuclide for Finns during the history of environmental radioactive contamination. In the years of maximum deposition rates in early 1960s the doses exceeded more than tenfold the doses in the following decades, and also the doses received after the Chernobyl accident (Rajama and Rantavaara 1982). The wild foods from forests are not likely to contribute to ingestion of 90 Sr essentially more than similar types of agricultural and garden products replacing wild foods in the diets of non-pickers and non-hunters. (AU)

  2. Accumulation of 137Cs after potassium fertilization in plant organs of Salix viminalis L. and in combusted ash

    The effect of potassium (K) application at a common rate on 137Cs uptake and distribution within basket willow (Salix viminalis L.) and 137Cs activity in willow ash was studied in a three-year field experiment on a sandy soil. Experimental plots fertilized with 60 kg N and 48 kg K per ha were compared with a control with similar N but no K fertilization. There was no significant difference in 137Cs activity concentrations in plants growing on plots with or without fertilizer K. Higher concentrations of 137Cs activity were found in roots and leaves of willow than in stems and cuttings. The highest 137Cs activity concentration was detected in the fine roots (size 0-1 mm). The transfer factor (TFg) of 137Cs in different plant organs varied between 0.1 x 10-3 and 2.6 x 10-3 m2 kg-1. After combustion, 137Cs activity concentrations in ash produced from wood chips from K-fertilized plots were significantly lower than those in ash originating from plots without K fertilization. Fly ash had higher 137Cs concentrations than bottom ash and all ash samples had 137Cs concentrations that were well below the 10 000 Bq kg-1 Swedish limit for spreading on land. -- Highlights: → We studied effect of potassium on 137Cs uptake by basket willow (Salix viminalis). → No significant difference in 137Cs activity in plants was found. → Higher 137Cs activity was found in roots and leaves than in stems and cuttings. → Highest 137Cs activity was detected in fine roots (size 0-1 mm). → Transfer factors of 137Cs in plant organs were 0.1 x 10-3 and 2.6 x 10-3 m2 kg-1.

  3. Deposition, transfer and migration of 137Cs and 90Sr in Swedish agricultural environments, and use of 137Cs for erosion studies

    Intensive atmospheric tests of nuclear bombs in the late 1950s and early 1960s resulted in fallout on Sweden of 3 kBq/m2137Cs and 2 kBq/m290Sr. To determine how soil characteristics influence radionuclide transfer to red clover, pot experiments with 137Cs and 90Sr were made with 178 Swedish mineral soils; significant negative correlations were obtained the with levels of P, K and Ca. To quantify impact in field conditions, experiments with artificial depositions on microplots were started in 1961. Transfer to barley on 12 topsoils combined with sandy and clay subsoils, and to grass on two contrasting pastures, was followed over two decades. The subsoil type was found to be important. Fallout of 137Cs from the Chernobyl accident, up to 200 kBq/m2 in some areas of Sweden, was studied between 1986 and 1994. As in the microplot experiments, transfer of 137Cs to grass was higher than to arable crops. Transfer rates were high in the first year(s), and then decreased differently from year to year, as shown by a new Tar (i.e. annual reduction rate in nuclide transfer) concept. The use of Chernobyl fallout to investigate soil redistribution on arable fields is briefly discussed; a frame-scrape soil-sampling procedure is proposed to improve the accuracy and precision of the 137Cs technique for evaluation of soil erosion. (author)

  4. Effective half-lives of 137Cs in giant butterbur and field horsetail, and the distribution differences of potassium and 137Cs in aboveground tissue parts

    Concentrations of 137Cs and 40K in different tissues of edible wild herbaceous plants, that is, leaf blade and petiole for giant butterbur (Petasites japonicas (Siebold et Zucc.) Maxim.), and leaf, stem and strobilus for fertile shoot of field horsetail (Equisetum arvense L.) were measured in 2012–2014 to clarify the effect in Japan from the Fukushima Daiichi Nuclear Power Plant accident. The concentrations of 137Cs decreased with time with effective half-lives of ca. 450 d and 360 d for giant butterbur and field horsetail, respectively. The ANOVA test revealed that 40K and 137Cs distributions in leaf blade and petiole for giant butterbur and leaf and stem for field horsetail were different. Therefore, other plants, leaf and stem for Japanese knotweed (Fallopia japonica (Houtt.) Ronse Decr.) and Canada goldenrod (Solidago canadensis L.), and leaf blade and petiole for gingko (Ginkgo biloba L.) and Someiyoshino cherry (Cerasus × yedoensis (Matsum.) A.V.Vassil. ‘Somei-yoshino’) were collected from the same sampling field and their 137Cs and 40K concentrations were compared to those in the giant butterbur and field horsetail parts. For 137Cs, concentrations in leaf blade and leaf parts were 1.1–6.0 times higher than those in petiole and stem parts for all six plants. On the other hand, 40K concentrations in leaf blade and leaf parts were 0.40–0.97 of those observed in petiole and stem parts. Discrimination ratios of 40K/137Cs of leaf blade to petiole or leaf to stem were then calculated and they ranged from 0.09 to 0.57. These results suggested that Cs and K did not behave similarly in these plants. Thus, to understand the radiocesium fate in plants, K measurement results should not be used as an analog for Cs behavior although Cs is known to have a similar chemical reactivity to that of K. - Highlights: • 137Cs amounts in leaf blade and leaf were higher than those in petiole and stem in plants. • 40K amounts in leaf blade and leaf were lower than

  5. Activity concentrations of 137Cs in meat of broiler chicken after single and continuous application

    Previously we examined the transfer, distribution and half-live of radiocaesium in broiler chicken after the application of artificially contaminated feed mixture or wheat wheat contaminated from the Chernobyl accident. Our results pointed to a different dynamics of radiocaesium in breast meat compared to leg meat in the chicken after short-time application (3 oral applications in 1 day). The aim of the present study was to find if the results are similar also after single and repeated (long-time) applications of an artificially contaminated feed mixture. Two experiments were carried out with broiler chickens (White Leghorn hybrid, race ISA VEDETTE). In experiment 1, one artificially contaminated oral dose of 5160 Bq of 137Cs (activity concentration 1664 Bq/g) was administered to 18-day-old chickens. In experiment 2, artificially contaminated oral doses of 500 Bq of 137Cs (activity concentration 161.3 Bq/g) were administered to 14-day-old chickens twice a day (at 8:00 and 20:00 h.) for 10 days. In either experiment, four chickens were slaughtered for activity determination in meat (breast and leg muscles) 6, 12, 24, 48 and 96 hours and 2, 4, 8, 10 days, respectively, after the first application of 137Cs. The uptake of the single oral 137Cs was rapid and the maximum 137Cs activity concentrations were found in breast meat (0.783 Bq/g) 24 hours and in leg meat (1.005 Bq/g) 6 hours after 137Cs application. From the 24th hour of the experiment, radiocaesium activity concentrations in breast and leg meat decreased with the biological half-life (T1/2b) of 84 and 66 hours, respectively. During a 10-day application of continuous doses of 137Cs, the Cs activity concentrations increased and were 3.988 Bq/g in breast meat and 5.610 Bq/g in leg meat on day 2, and 7.427 Bq/g and 7.698 Bq/g, respectively, on day 10. Immediately after the administration of radiocaesium was stopped, the 137Cs activity concentrations decreased rapidly with T1/2b = 4.5 and 3.8 days in breast and leg

  6. Distribution of {sup 137}Cs in three representative soils of Pernambuco state, Brazil;Distribuicao de {sup 137}Cs em tres solos representativos do estado de Pernambuco

    Antunes, Patrik Diogo, E-mail: pdantunes@yahoo.com.b [Universidade Federal Rural de Pernambuco (UFRPE), Recife, PE (Brazil). Dept. de Ciencias do Solo; Sampaio, Everardo Valadares de Sa Barretto; Ferreira Junior, Antonio Luiz Goncalves; Salcedo, Ignacio Hernan, E-mail: esampaio@ufpe.b, E-mail: antonio.ferreira@ariano.nlink.com.b, E-mail: salcedo@ufpe.b [Universidade Federal Rural de Pernambuco (UFRPE), Recife, PE (Brazil). Dept. de Energia Nuclear; Galindo, Izabel Cristina Luna, E-mail: iclgalindo@uol.com.b [Universidade Federal Rural de Pernambuco (UFRPE), Recife, PE (Brazil). Dept. de Agronomia

    2010-05-15

    Contents of {sup 137}Cs have been used to quantify soil loss or accumulations, based on values of reference sites with little soil disturbance in the last decades. In Northeastern Brazil no such sites have been evaluated yet. Three areas with flat topography, native vegetation and undisturbed soil were selected in of Goiania, Araripina and Sertania counties, state of Pernambuco. Four points in each area were marked at a distance of 20 to 50 m away from each other and soil samples were collected in 3 cm depth intervals, down to 30 cm. The {sup 137}Cs activities were determined using gamma spectrometry with a hyper pure germanium detector. Average contents of {sup 137}Cs (Bq m{sup -2}) were 71.6 +- 6.3 in Goiania, 64.0 +- 13.8 in Araripina and 95.5 +- 9.8 in Sertania. Values in this range have been reported in Paraiba and Bahia, and higher ones in the Southeastern region, confirming the reduction of stocks in areas closer to the equator. The highest activities occurred in the surface layers, ranging from 0.5 to 1.6 Bq kg{sup -1}, and decreased linearly with depth until the detection limits: 18 cm in Araripina, 15 cm in Goiania, and 9 cm in Sertania. In Goiania, the activity was highest (2.06 +- 1.0 Bq kg{sup -1}) in an organic horizon above a inorganic horizon. The high activities and stock and lower depth in Sertania could be explained by the predominance of 2:1 clay minerals versus 1:1 clay minerals in the other areas. {sup 137}Cs activities were positively correlated with water and KCl pH values and negatively correlated with Al concentrations. The results confirm that, in the reference areas, {sup 137}Cs activities are highest in the surface layers, decreasing regularly down the soil profile. (author)

  7. Patterns of 137Cs accumulation in bullhead catfish inhabiting an abandoned reactor reservoir

    The author assayed muscle 137Cs concentrations of bullhead catfish (Ameiurus natalis) in order to determine factors contributing to the bioconcentration of this fission product. Bullhead catfish (N = 173) were obtained from the Pond B reservoir, Savannah River Site, SC. Muscle 137Cs concentration did not differ between sexes (ANOVA, P = 0.631). Age of fish (1--6 yr) appeared to explain variation in 137Cs concentration (P = 0.005), but not when mass of fish was included as a model covariate (P = 0.086). Least-square means, adjusted for the covariate, suggested that 1 and 2 yr old fish (71.09 and 81.38 mean pCi/g, respectively) differed from 3, 4, 5, and 6 yr old fish (94.94, 92.34, 97.27, 90.25 mean pCi/g, respectively). Therefore, the effects of age and mass were evaluated by partitioning the data into young (1--2 yr) and older (3, 4, 5, and 6 yr) age classes. When adjusted for mass, age (young vs. old) significantly accounted for differences in 137Cs concentration (78.98 vs. 94.33 mean pCi/g; P = 0.005). Within older fish, neither age (P = 0.870) or mass (P = 0.361) significantly influenced 137Cs concentration. The effect of age within young fish was nonsignificant (P = 0.971) in contrast to the influence of mass (P = 0.044). This suggests that the contribution of 'size' (mass) to 137Cs body burden is related to early growth and that these fish reach an asymptotic 'steady-state' 137Cs concentration by 3 years of age

  8. Sediment and 137Cs behaviors in the Ogaki Dam Reservoir during a heavy rainfall event

    We performed a simulation of sediment and 137Cs behaviors in the Ogaki Dam Reservoir, one of the main irrigation reservoirs in the Fukushima prefecture, Japan, during a heavy rainfall event occurred in 2013. The one-dimensional river and reservoir simulation scheme TODAM, Time-dependent One-dimensional Degradation and Migration, was applied for calculating the time dependent migration of sediment and 137Cs in dissolved and sediment-sorbed forms in the reservoir. Continuous observational data achieved in the upper rivers were used as the input boundary conditions for the simulation. The simulation results were compared with the continuous data achieved in the lower river and we confirmed the predicted values of sediment and 137Cs in sediment-sorbed form at the exit of reservoir satisfactorily reproduced the observational data. We also performed sediment and 137Cs behavioral simulation by changing the water level of the reservoir, because such a dam operation could control the quantities of sediment and 137Cs discharge from and/or deposition in the reservoir. The simulation clarified that the reservoir played an important role to delay and buffer the movement of radioactive cesium in heavy rainfall events and the buffer effect of the reservoir depended on particle sizes of suspended sediment and the water level. It was also understood that silt deposition was the main source of the bed contamination (except for the initial fallout impact), while clay was the main carrier of 137Cs to the lower river at a later stage of rainfall events. - Highlights: • We simulated sediment and 137Cs behavior in a reservoir in the Fukushima area. • The simulation reproduced the measured values during a heavy rainfall event. • It clarified the reservoir buffers contamination movement in heavy rainfall events

  9. {sup 137}Cs and {sup 9}Sr uptake by sunflower cultivated under hydroponic conditions

    Soudek, Petr [Department of Plant Tissue Cultures, Institute of Organic Chemistry and Biochemistry, Academy of Sciences of the Czech Republic, Flemingovo nam. 2, CZ-166 10 Prague 6 (Czech Republic); Valenova, Sarka [Department of Plant Tissue Cultures, Institute of Organic Chemistry and Biochemistry, Academy of Sciences of the Czech Republic, Flemingovo nam. 2, CZ-166 10 Prague 6 (Czech Republic); Vavrikova, Zuzana [Department of Plant Tissue Cultures, Institute of Organic Chemistry and Biochemistry, Academy of Sciences of the Czech Republic, Flemingovo nam. 2, CZ-166 10 Prague 6 (Czech Republic); Vanek, Tomas [Department of Plant Tissue Cultures, Institute of Organic Chemistry and Biochemistry, Academy of Sciences of the Czech Republic, Flemingovo nam. 2, CZ-166 10 Prague 6 (Czech Republic)]. E-mail: vanek@uochb.cas.cz

    2006-07-01

    The {sup 9}Sr and {sup 137}Cs uptake by the plant Helianthus annuus L. was studied during cultivation in a hydroponic medium. The accumulation of radioactivity in plants was measured after 2, 4, 8, 16 and 32 days of cultivation. About 12% of {sup 137}Cs and 20% of {sup 9}Sr accumulated during the experiments. We did not find any differences between the uptake of radioactive and stable caesium and strontium isotopes. Radioactivity distribution within the plant was determined by autoradiography. {sup 137}Cs was present mainly in nodal segments, leaf veins and young leaves. High activity of {sup 9}Sr was localized in leaf veins, stem, central root and stomata. The influence of stable elements or analogues on the transfer behaviour was investigated. The percentage of non-active caesium and strontium concentration in plants decreased with the increasing initial concentration of Cs or Sr in the medium. The percentage of {sup 9}Sr activity in plants decreased with increasing initial activity of the nuclide in the medium, but the activity of {sup 137}Cs in plants increased. The influence of K{sup +} and NH{sub 4} {sup +} on the uptake of {sup 137}Cs and the influence of Ca{sup 2+} on the uptake of {sup 9}Sr was tested. The highest accumulation of {sup 137}Cs (24-27% of the initial activity of {sup 137}Cs) was found in the presence of 10 mM potassium and 12 mM ammonium ions. Accumulation of about 22% of initial activity of {sup 9}Sr was determined in plants grown on the medium with 8 mM calcium ions.

  10. Precipitation scavenging of 7Be and 137Cs radionuclides in air

    Atmospheric depositional fluxes of the naturally occurring 7Be of cosmogenic origin and 137Cs from fallout of the Chernobyl accident were measured over a 6-year period (January 1987-December 1992) at Thessaloniki, Greece (40o38'N, 22o58'E). Total precipitation accumulation during 1987-1992 varied between 33.7 cm and 65.2 cm, reflecting a relatively dry (precipitation-free) climate. The activity concentrations of 7Be and 137Cs in rainwater depended on the precipitation rate, being higher for low precipitation rates and lesser for high precipitation rates. 137Cs was removed by rain and snow more efficiently than 7Be. Snowfall was more efficient than rainfall in removing the radionuclides from the atmosphere. The annual bulk depositional fluxes of 7Be varied between 477 and 1133 Bq m-2 y-1 and this variability was attributed to the amount of precipitation and the variations of the atmospheric concentrations of 7Be. The annual bulk depositional fluxes of 137Cs showed a significant decrease over time from 1987 to 1992, resulting in a removal half-life of 1.33 years. The presence of 137Cs in air, and therefore in rainwater and snow, long after the Chernobyl accident (26 April 1986) was mainly due to the resuspension process. The normalized depositional fluxes of both radionuclides showed maximal values during the spring season where the maximum amount of precipitation occurred. The relatively high positive correlation between 7Be and 137Cs normalized depositional fluxes indicates that the scavenging process of local precipitation controlled the fluxes of both radionuclides. The dry depositional flux of 7Be was less than 9.37% of total (wet and dry) depositional flux. The fraction of dry-to-total depositional flux of 137Cs was much higher than that of 7Be, due to the resuspended soil

  11. 137Cs and 9Sr uptake by sunflower cultivated under hydroponic conditions

    The 9Sr and 137Cs uptake by the plant Helianthus annuus L. was studied during cultivation in a hydroponic medium. The accumulation of radioactivity in plants was measured after 2, 4, 8, 16 and 32 days of cultivation. About 12% of 137Cs and 20% of 9Sr accumulated during the experiments. We did not find any differences between the uptake of radioactive and stable caesium and strontium isotopes. Radioactivity distribution within the plant was determined by autoradiography. 137Cs was present mainly in nodal segments, leaf veins and young leaves. High activity of 9Sr was localized in leaf veins, stem, central root and stomata. The influence of stable elements or analogues on the transfer behaviour was investigated. The percentage of non-active caesium and strontium concentration in plants decreased with the increasing initial concentration of Cs or Sr in the medium. The percentage of 9Sr activity in plants decreased with increasing initial activity of the nuclide in the medium, but the activity of 137Cs in plants increased. The influence of K+ and NH4+ on the uptake of 137Cs and the influence of Ca2+ on the uptake of 9Sr was tested. The highest accumulation of 137Cs (24-27% of the initial activity of 137Cs) was found in the presence of 10 mM potassium and 12 mM ammonium ions. Accumulation of about 22% of initial activity of 9Sr was determined in plants grown on the medium with 8 mM calcium ions

  12. ESTIMATION OF SOIL EROSION IN A RESERVOIR WATERSHED USING 137CS FALLOUT RADIONUCLIDE

    Y. J. CHIU; A. M. BORGHUIS; H. Y. LEE; K. T. CHANG; J. H. CHAO

    2007-01-01

    Sedimentation from soil erosion is a critical reservoir watershed management issue. Due to the difficulty of field investigations, empirical formulas are commonly used to estimate the soil erosion rate. However, these estimations are often far from accurate. An effective alternative to estimating soil erosion is to analyze the spatial variation of 137Cs inventory in the soil. 137Cs can be adsorbed by the soil and is widely assumed to change its distribution only when disturbed by rainfall and human activities. Thus, 137Cs distributed in soils can be a useful environmental tracer to estimate soil erosion. In this study, the net soil loss estimate is 108,346 t/yr and the gross erosion and net erosion rates are 10.1 and 9 t/ha yr respectively. The sediment delivery ratio is therefore estimated to be 0.9 based on the two erosion rates. Because of the steep hillsides in the watershed, only 10% of the sediment yield stayed in the deposition sites and 90% was transported to the river as the sediment output. Soil erosion estimates from spatial variations of the 137Cs activity in the Baishi river watershed showed satisfactory accuracy when compared to sediment yield data. Using soil 137Cs concentrations is therefore a feasible method for estimating soil loss or deposition in Taiwan. Data sampling, analysis and result of this approach are given in this paper.

  13. Spatial distribution of fallout 137Cs in coastal marine water of Tamil Nadu coast

    Very little information on the fallout 137Cs activity exists for the Bay of Bengal. Normally the volume of sea water required for detecting fall out level of 137Cs in coastal marine environment ranges from 100 litres to 1000 litres. The studies on distribution of 137Cs in surface seawater of Tamil Nadu in Bay of Bengal were carried out in April 2009. On the eastern coastal lines of Bay of Bengal in Tamil Nadu, seven offshore locations were selected namely Chennai, Pondicherry, Karaikal, Rameshwaram, Tuticorin, Nagercoil and Kanyakumari. In situ preconcentration method was adopted and the experiments were carried out using motor boats well equipped to carry the instruments and provide power supply to operate the pump. 1000 litres of seawater was passed each time through CFCN filters at all the locations at a flow rate of 8 litres per minute. The activity concentrations of 137Cs was in the range of 0.90 to 2.2 Bq/m3. These data represents reference values for coastal environment of Tamil Nadu and will be used to estimate radionuclide inventory in Indian marine environment, particularly of East Coast. The 137Cs activity indicates that there are no new inputs of these radionuclides into the area. (author)

  14. Influence of urea and of chlorocholine chloride on accumulation of 137Cs in spring wheat crops

    The influence of leaf feeding with nitrogen in urea solution and application of chlorocholine chloride (CCC) on the uptake of 137Cs by spring wheat from the investigated soil samples and through leaves was studied in pot experiments. Spray application of nitrogenous fertilizer in urea solution with additional use of growth retardant were found to have brought about an increased accumulation in the grain of 137Cs taken up by the plants from the contaminated soil. It was found that the 2-4 times more 137 Cs accumulated in the wheat grain from the leaves contaminated in the flowering stage in the comparison with that found in the grain of plants contaminated in the propagation stage. The application of leaf feeding with urea and chlorocholine exerted no influence on the accumulation of 137Cs in grain if the plants had been contaminated superficially in their earlier development stages. Contamination with 137Cs sprayed upon the plants after application of chlorocholine chloride appeared to pass to the spring wheat crops more readily. (author)

  15. Total beta activity, 137Cs and 90Sr in surface air in northern Finland in 1963

    Air filter samples collected at Sodankylae(67 22' N, 26 39' E) were analyzed to determine concentrations of 137Cs and 90Sr in surface air in northern Finland in 1963. Previously, activity concentrations of Pu isotopes have been determined from the same filters. Activity concentrations of 137Cs and 90Sr in surface air were 3-13800 ± 2700 μBq/m3 and 3-5340 ± 290 μBq/m3, respectively. Air concentrations of 137Cs and 90Sr varied seasonally with a maximum in spring due to the springtime enhanced transportation of air masses with radioactive aerosols from the stratosphere to the troposphere. Activity ratios 90Sr/239+240Pu and 90Sr/137Cs were 6.9 ± 0.8-75 ± 5 and 0.08 ± 0.03-1.46 ± 0.51, respectively. The median value for the 90Sr/137Cs ratio (0.508) indicates contamination from global nuclear test fallout. An air mass back trajectory analysis suggests that no direct transport of radioactivity from the Novaya Zemlya test site to northern Finland occurred in 1963. (orig.)

  16. Isolation of 137-Cs in tuna fish by ammonium phosphomolybdate (AMP)

    The isolation of 137-Cs in tuna fish (Neithunnus macroptenus) has been carried out using AMP. The energy of 137-Cs was measure using NaI(T1) detector connected to a Multi Channel Analyzer (MCA). In standard solution of 137-Cs with activity 160.74 and 80.37 pCi, the addition of 120 mg AMP and 7 hours of absorption time, caused 97% of 137-Cs in the solution was absorbed. The destruction of tuna fish was carried out using two methods namely by wet destruction with sulfuric acid, nitrit acid and hydrogen peroxid mixture and by wet destruction with hydrogen peroxide. The applications of this technique of tuna fish was carried out by spiking 137-Cs standard into the fish before being destructed. The recovery obtained from wet destruction with H2O2 was about 80%, while from destruction with acid mixtures and H2O2 was only about 47%. (authors). 3 refs, 3 tabs

  17. Specific activity and concentration model applied to 137Cs movement in a eutrophic lake

    A linear systems-analysis model which simulates time-dependent dynamics of specific activity and concentration of radiocesium in lake ecosystems was applied to a shallow, eutrophic lake that had received a pulse input of 137Cs. Best estimates of transfer coefficients for abiotic compartments (sediment, interstitial water and lake water) and the macrophyte compartment which controlled the mass balance of cesium in water were determined by ''tuning'' our initial estimates of the transfer coefficients to observed data on 137Cs concentrations and contents of these compartments. In most cases, the optimized transfer coefficients for the abiotic compartments were not greatly different from our independently derived initial estimates, and the simulations for optimized coefficients were close to those based on initial estimates. The 137Cs concentrations in water as predicted by the optimized transfer coefficients were then used to calculate 137Cs kinetics in biota other than macrophytes. In general, model simulations were close to concentrations observed in the biota. The agreement between 137Cs concentrations and simulations in bottom invertebrates supported our assumption that bottom sediments are not a major source of Cs to the biota. Our specific activity and concentration model was compared to the radionuclide content model, the model used in terrestrial ecosystems. For biotic components of aquatic ecosystems, values of α/sub ij/, the transfer coefficients of our model, are easily estimated from turnover rates of radiocesium in individual organisms in the laboratory

  18. Assessment of the transfer of 137Cs in three types of vegetables consumed in Hong Kong

    A dynamic food chain model has been built for the modeling of the transfer of 137Cs in three types of vegetables consumed in Hong Kong, namely, white flowering cabbage (Brassica chinensis), head lettuce (Lactuca sativa) and celery (Apium graveolens). Some parameters have been estimated from the experimental data obtained in this work. The experimental data include the transfer factors of 137Cs from soil to the different vegetable species which are determined through high resolution gamma spectrometry, maximum crop biomasses for the vegetable species, the dry-to-fresh ratios for the vegetable species, the bulk density of soil layers and the average concentration of 137Cs in air. The derived parameters include the deposition rate and the root uptake rate, information for tillage, the logistic growth model and radionuclide concentrations in vegetables. The dynamic food chain model is solved by the Birchall-James algorithm to give the 137Cs concentration in subsurface soil, from the 0.1-25 cm soil layer, and the 137Cs concentration in harvested and unwashed vegetables. As validation of the model and parameters, the concentrations obtained experimentally and from the model are compared and are found to be in good agreement

  19. Temporal change in fallout 137Cs in terrestrial and aquatic systems: a whole ecosystem approach

    During the years after a nuclear accident, the bioavailability and environmental mobility of radiocesium declines markedly, resulting in large changes in contamination of foodstuffs, vegetation, and surface waters. Predicting such changes is crucial to the determination of potential doses to affected populations and therefore to the implementation of radiological countermeasures. We have analyzed 77 data sets of radiocesium (137Cs) activity concentrations in milk, vegetation, and surface waters after the Chernobyl accident. Our results show that the rate of decline in 137Cs during the years after Chernobyl is remarkably consistent in all three ecosystem components, having a mean effective half-life, Teff ≈ 2 years. By comparing changes in 137Cs availability with rates of diffusion of 40K (a close analogue) into the lattice of an illitic clay (1) we have, for the first time, directly linked changes in the environmental availability of 137Cs to fixation processes at a mechanistic level. These changes are consistent with declines in the exchangeable fraction of 137Cs in soils (2, 3)

  20. 137Cs-uptake into wheat (Triticum vulgare) plants from five representative soils of Bangladesh.

    Monira, B; Ullah, S M; Mollah, A S; Chowdhury, N

    2005-05-01

    A pot experiment was conducted to study the uptake of 137Cs by wheat grown in five representative soils of Bangladesh having different soil characteristics. Artificial application of 137Cs increased the activity in soils up to 45.9 Bq/kg soil, measured at the end of the harvest of wheat crop. Different plant parts had different ability to accumulate 137Cs. Grains had the least activity and transfer factor, while the highest activity and lowest transfer factor were measured in roots, which restricted translocation of 137Cs to wheat straw. The result showed that the transfer factors (mean value) varied from 0.05 to 0.114 in wheat straw, 0.066-0.133 in roots and 0.011-0.043 in wheat grains. The activity and transfer factor of radioactive cesium in wheat plants were found to be greatly influenced by soil properties, i.e. clay content, K, organic matter, CEC, pH, exchangeable ions, etc. Cation exchange capacity and calcium in soils influenced positively, while clay minerals, exchangeable K and organic matter, negatively affected the 137Cs activity concentrations in wheat plants. PMID:15931978

  1. 137 Cs content of some honey products in the period 1993-1998

    In this work, the 137 Cs content in some honey products collected from Arges and Sibiu zones in the period 1993-1998 is determined. The gamma ray measurements were carried out for 18-28 hours by means of a HPGe (EG/G ORTEC) detector of 30% relative efficiency and 2.1 KeV resolution for the 60 Co 1332.5 KeV gamma ray. The samples were placed in a lead container with 10 cm thick walls. The IAEA-321 reference material with certified specific activities for 137 Cs was used to check the analysis quality. The results were expressed in Bq/kg and Bq/l as appropriate. Comparisons with the measurements performed previously were done. The 137 Cs content of the analyzed samples depends on product, type and collecting time. The activity levels in honey increased in 1994, as compared to 1993 and 1995-1997, to 0.8 Bq/kg. The 137 Cs concentration in propolis is 5-10 times higher than that in honey. Compared to '80 period, the 137 Cs concentration in honey products is diminished. (authors)

  2. 137Cs availability for soil to understory transfer in different types of forest ecosystems

    A quantitative analysis of 137Cs bioavailability in forest soils in the long term after the Chernobyl NPP accident based on a 3-year (1996-1998) investigation is presented. Five forest sites with different trees, composition and properties of soil were studied to identify factors determining radiocaesium transfer to different understory species. The following parameters were investigated: 137Cs activity concentrations and its speciation in various horizons of forest soil, accumulation of this radionuclide by different species of understory vegetation and distribution of root biomass in the soil profile. It has been shown that one decade after the deposition maximum 137Cs activity in soil of the experimental sites considered is located in different soil layers dependent on moisture regime, characteristics of litter and soil properties. A linear dependence between aggregated transfer factors for different species and groups of species of understory vegetation and exchangeable and available fractions of radiocaesium in soil was found. The vertical distribution of 137Cs activity, percentage of exchangeable radiocaesium in each horizon of litter and soil, as well as distribution of root systems (mycelia) over the soil profile are key factors governing variations in the availability of 137Cs for transfer to all forest understory components

  3. Migration of 137Cs in the soil of sloping semi-natural ecosystems in Northern Greece

    In the present study, the 137Cs concentration in the soil of sloping semi-natural ecosystems at four different regions of Western Macedonia in Greece was measured 10 years after the Chernobyl accident. These regions were highly polluted due to the deposition of radionuclides escaped during the accident. The concentrations of 137Cs measured were found to differ significantly among the four regions. The rates of both horizontal and vertical migration in the soil were also evaluated. The vertical migration velocity of 137Cs was found to range from 0.1 to 0.3 cm per year, in the most contaminated areas. Consequently, 10 years following the Chernobyl accident, the bulk of 137Cs deposited over the surface of the studied areas in Greece was found to be restricted in the upper 5 cm layer of soil. Regarding the horizontal migration, in most of the sampling sites, we did not detect any displacement or trend to movement of radiocaesium on the surface from the upper to the lower levels of the slopes. Instead, we recorded decreased concentrations of 137Cs with the decrease of altitude

  4. 137Cs contamination of the Techa river flood plain near the village of Muslumovo

    The results of a radiometric survey of the Techa river flood plain near the village of Muslumovo in the Chelyabinsk region of Russia are presented. The observed territory extended 16.6 km along the riverbed, with a total area of 2.5 km2. The collimated scintillation detector technique was applied to in situ field measurements of 137Cs deposition on the soil. Maps of 137Cs deposition and soil penetration depth were developed on the basis of approximately 5000 measurements. The total 137Cs deposition within the surveyed territory has been estimated at 6.6 TBq. The means of the total 137Cs soil depositions at half-kilometer sites on the flood plain and its distribution along the river have also been calculated. A maximum 137Cs contamination above 7.5 MBq/m2 is associated with a bank height up to 1 m above the usual water level. The data identify zones of intensive radionuclide sedimentation and transit zones

  5. Peculiarities of 137Cs accumulation by macromycetes in dry bors of Ukrainian Polessye

    The main ecological peculiarities of dry bor in Ukrainian Polessye were given. Research were carried out in Central Polessie of Ukraine during 1997 - 1999. Results were obtained due to spectrometric measurement of specific activity of 137Cs in fruit bodies of mushrooms and in the soil. Species composition of macromycetes was divided on homogeneous groups on intensity of 137Cs accumulation. Amanita porphyria, A. muscaria and Tricholoma portentosum belong to the group of weak 137Cs accumulation from the soil (TF = 15 - 20); Amanita pantherina, A. phalloides, Cantharellus cibarius, Boletus edulis, Tricholoma flavovirens and Laccaria laccata - to the group of moderate radionuclide accumulation (TF = 30 - 55). The group of strong 137Cs accumulation (TF = 100 - 180) consists of Suillus variegates, S. bovines and Hydnum imbricatum; and group of very strong accumulation (TF 200 - 280) - of Xerocomus badius, Lactarius rufus, Russula xerampelina, Cortinarius varius and Paxillus involutus. Cortinarius sanguineus (with TF 400) is an accumulator of 137 Cs. Comparative evaluation of dry bor was given from the point of view of purchase of edible macromycetes in it

  6. GIS supported calculations of 137Cs deposition in Sweden based on precipitation data

    137Cs deposition maps were made using Kriging interpolation in a Geographical Information System (GIS). Quarterly values of 137Cs deposition density per unit precipitation (Bq/m2/mm) at three reference sites and quarterly precipitation at 62 weather stations distributed over Sweden were used in the calculations of Nuclear Weapons Fallout (NWF). The deposition density of 137Cs, resulting from the Chernobyl accident, was calculated for western Sweden using precipitation data from 46 stations. The lowest levels of NWF 137Cs deposition density were noted in the northeastern and eastern Sweden and the highest levels in the western parts of Sweden. The Chernobyl 137Cs deposition density is highest along the coast in the selected area and the lowest in the southeastern part and along the middle. The sum of the calculated deposition density from NWF and Chernobyl in western Sweden was compared to accumulated activities in soil samples at 27 locations. Comparisons between the predicted values of this study show a good agreement with measured values

  7. Migration of 137Cs from air to soil and plants in the Gulsvik area, Norway after the Chernobyl reactor accident

    The migration of 137Cs from air to soil and vegetation after the Chernobyl accident has been studied using the concentrations measured in the Gulsvik area in Norway. The major part of the 137Cs deposition seems to be in the soil. An uptake of 137Cs from soil to plants through their root system is not a rapid process. Only a few percent of the deposition can be traced in plants. This seems to suggest that as far as 137Cs is concerned, an effect of the Chernobyl releases is not an acute but a long-term phenomenon. The 137Cs accumulation in soils is rather high, but doses not result in 137Cs levels in plants and diet higher than acceptable in Norway

  8. Simulation study on 137Cs distribution in the each component of irrigation-farmed gray-brown desert soil humus

    The components and characters of humus in irrigation-farmed gray-brown desert soil were studied and gel filtration method is used at indoor experiment to study the bond properties of the foreign source 137Cs and soil humus' components. Results show that the bonding rate of 137Cs was the highest in clay mineral, 78.37% of total. 21.63% of 137Cs was accumulated in the humus, the bonding rate of 137Cs with humic acid, fulvic acid, and humin were 5.78%, 6.60% and 9.25%, respectively. The humic acid and 137Cs formed four low weight complex molecules, their average molecular weights are > 700, 392, 168 and 137Cs can not only be bonded into the stable organic-inorganic composite, but also into humus-metal ion complex with very high stability. (authors)

  9. Post-depositional redistribution and gradual accumulation of 137Cs in a riparian wetland ecosystem in Sweden

    After the Chernobyl accident, high activity concentrations of 137Cs (>1 MBq m-2) were detected in a riparian swamp in the central-eastern part of Sweden. The objective of this study was to clarify the redistribution processes behind the accumulation of 137Cs in the wetland. A mass balance budget of 137Cs was calculated based on soil and sediment samples and reports in the literature. Results showed that accumulation occurred over several years. Of all the 137Cs activity discharged between 1986 and 2002 from the upstream lake, 29% was estimated to be retained in the wetland. In 2003, measurements showed that 17 kBq m-2 sedimented on the stream banks of the wetland. Continuing overbank sedimentation by spring flooding prolongs the time that the wetland will contain high activity concentrations of 137Cs. Consequently, organisms living in wetlands serving as sinks for 137Cs may become exposed over long time periods to high activity concentrations

  10. The uptake of 90Sr, 137Cs and 144Ce by leaves of spring wheat and rape

    The distribution and accumulation of 90Sr, 137Cs, 144Ce through the leaf surface into the plant have been studied. The results show that the uptake rate of 137Cs by crop plant is about 53%, while the uptake rate for 90Sr and 144Ce is about 0.4%. However 90Sr is absorbed in significant amount from soil whereas 137Cs is absorbed in negligible amount