Results 131 to 140 of about 1,254 (182)
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ANION ADSORPTION BY GOETHITE AND GIBBSITE
Journal of Soil Science, 1972Summary The relationship between adsorption and pH, termed the adsorption envelope, varies with the p K a, of the conjugate acid of the anion, for several adsorbents in presence of an excess of specifically adsorbed anions.
F. J. HINGSTON +2 more
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Morphological characterisation of gibbsite and alumina
Powder Technology, 2002By combining visualisation by scanning electron microscopy (SEM), optical microscopy (OM) with aniline as an immersion liquid and semiautomated image analysis procedures, the external and internal structures of different types of gibbsite and alumina particles have been characterised.
Belaroui, K. +2 more
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Halloysite and Gibbsite Formation in Hawaii
Clays and clay minerals (National Conference on Clays and Clay Minerals), 1960AbstractDesilication and removal of bases from the basalitic rocks of the Hawaiian Islands produces large amounts of halloysite and gibbsite, together with variable quantities of allophane and nontronite, iron and titanium oxides, and amorphous mineral and gel material.The nature and relative abundance of intermediate and end products of weathering ...
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ANION ADSORPTION BY GOETHITE AND GIBBSITE
Journal of Soil Science, 1974Summary The desorption of specifically adsorbed (ligand exchanged) anions, such as phosphate, selenite, and fluoride, from the surface of gibbsite and goethite has been studied by repeatedly washing the adsorption complex with solutions of constant pH and ionic strength but containing no specifically adsorbable ...
F. J. HINGSTON +2 more
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Gibbsite in the weathered dartmoor granite
Geoderma, 1971Abstract Gibbsite encountered in the weathered Dartmoor granite is an initial product of the weathering process; its occurrence is not indicative of an earlier humid tropical environment.
C.P. Green, M.J. Eden
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Atomic force microscopy of gibbsite
Applied Surface Science, 1998Atomic force microscopy has been used to image the surface structure of a range of gibbsite (Al(OH)3) crystals. A variety of microtopographies has been imaged on the (001) plane, and sub-nanometer detail has been observed on flat areas that is commensurate with the known bulk structure of the solid.
Lloyd, S. +3 more
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THE MICROMORPHOLOGY OF GIBBSITE FORMS IN SOILS
Journal of Soil Science, 1977Summary Using optical and scanning electron microscopy various forms of gibbsite are described in some tropical soils. In a lateritic soil from Zaire gibbsite occurs on argillans, in randomly oriented crystal sheets, as nodular aggregates infilling vughs and on ped faces.
H. ESWARAN, G. STOOPS, C. SYS
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Autoprecipitation of Gibbsite and Boehmite
2016When thick bauxite slurry was heated up to 160°C, boehmite precipitation was observed and caused scale formation on the surface of heat exchangers in digestion step.
T. Harato, T. Ishida, K. Yamada
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The removal of silicate from gibbsite
Hydrometallurgy, 1993Abstract Desorption of silicate from the surface of gibbsite was studied under typical Bayer process conditions. Desorption of silicate declined with aging and with increasing temperature. Successive extractions increased the desorption of silicate, although desorption was more pronounced in the first extraction than in subsequent extractions.
Kofi Adu-Wusu, William R. Wilcox
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Soil Science Society of America Journal, 1967
Abstract In order to help determine if the equilibria reached by soil mineral mixtures is that predicted on the basis of single minerals, two kaolinite samples were equilibrated individually and also with gibbsite of known stability. One set of samples was equilibrated from undersaturation, the other from supersaturation. Samples were
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Abstract In order to help determine if the equilibria reached by soil mineral mixtures is that predicted on the basis of single minerals, two kaolinite samples were equilibrated individually and also with gibbsite of known stability. One set of samples was equilibrated from undersaturation, the other from supersaturation. Samples were
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