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Preparation of Mg-#alpha# SiAlON powder by carbothermal reduction-nitridation of talc and halloysite  

International Nuclear Information System (INIS)

Carbothermal reduction-nitridation (CRN) of talc (Mg_3(Si_2O_5)_2(OH)_2) and halloysite (Al_2Si_2O_5(OH)_4) clay provides a useful route for preparing low-cost Mg-#alpha# sialon powder. In this study, the chosen molecular ratios of talc to halloysite were 0.1:1, 0.2:1, 1.5:1.0 and 2.0:1. The CRN reaction was conducted at 1450 to 1520 deg C and 2 to 6h holding time using carbon black as a reducing agent in flowing N_2 (gas). The results showed the synthesized powder was composed of #alpha#-sialon, #beta#-sialon and small amounts of SiC, 15R and AlN phases that greatly depended on the ratio of talc to halloysite, the reaction temperature and holding time. The highest content of Mg-#alpha# sialon, as much as 90wt%, was achieved at 1480 deg C for a holding time of 4h at a talc to halloysite ratio of 1.5:1.0. SiC was considered as an intermediate compound. We also discuss the evaporation loss of Mg caused by ...

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Use of clays as liners in solar ponds  

Energy Technology Data Exchange (ETDEWEB)

An alternative to synthetic materials for use in solar pond liners is to select clayey soils as hydraulic barriers. This option reduces the cost of construction and the risk of contamination of subsoil and groundwater by hot brines. This paper deals with the physical, chemical and hydraulic properties of different soils tested mainly as compacted clay liners. The underdeveloped nations have the option to use this type of liner, but before doing so several tests are recommended, including those for soil and water composition, permeability, plasticity and X-ray diffraction analysis. In this investigation the following samples are analyzed: native clayey soils with illite, montmorillonite and halloysite, treated and non-treated bentonites in powder and granulated form, a mixture of zeolite and sodium bentonite, and industrial minerals composed largely of halloysite, kaolinite and attapulgite selected clays. Neutral salt aqueous solutions (NaCl and ...

2009-06-15

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The effect of oxide additives on the synthesis and sintering of x-Sialon  

International Nuclear Information System (INIS)

The effect is reported of seven inorganic oxide additives on both the formation mechanism and the densification of X-Sialon prepared by a silicothermal process. The oxides were added to the starting mixture of halloysite clay, alumina and elemental silicon at a level of 1 wt% of the calculated final product, and fired in nitrogen at 1200-1500 deg C. The formation of X-Sialon was monitored by thermal analysis, powder XRD and 2"7"Al and "2"9Si solid state MAS NMR The effects of the additives are temperature dependent and influence the various stages of the reaction by differing degrees. The oxides which best promote the formation of crystalline X-Sialon (Y_2O_3, CaO and MgO) are also those which facilitate the conversion of initially-formed Si_3N_4 to SiO_2N_2 and SiO_3N units. Densification is most enhanced by Y_2O_3 CaO and CeO_2; MgO exerts its maximum effect on sintering at lower temperatures. Copyright (1998) Australasian Ceramic Society

1998-09-28

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Natural gels: crystal-chemistry of short range ordered components in Al, Fe, and Si systems  

Energy Technology Data Exchange (ETDEWEB)

In this review, the most important inorganic natural gels are presented: opal, aluminosilicate (allophanes) and hydrous iron oxides and silicates. It is demonstrated that natural gels are ordered at the atomic scale. In allophanes, Al is distributed between octahedral and tetrahedral sites. The amount of Al increases as Al/Si ratio decreases. Si-rich allophane have a local structure around Al and Si very different of that is known in kaolinite or halloysite. Transformation of Si-rich allophanes to crystallized minerals implies dissolution-recrystallization processes. On the contrary, in iron silicate with Fe/Si = 0.72, Si and Fe environments are close to those found in nontronite. The gel transformation to Fe-smectite may occur by long range ordering during ageing. In ferric silicate gels, the similarity of local structure around Fe in poorly ordered precursors and what is known in crystallized minerals suggests a solid transformation during ageing. This difference ...

1997-07-01