How To Use Kaolinite In A Sentence
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Three types of soils, residual soils, kaolinite and bentonite, were used in the study.
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These include clay minerals such as kaolinite and talc, micas, montmorillonites, and the remainder of the asbestos minerals including chrysotile (white asbestos).
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Gold is associated with extensive zones of vuggy silica, quartz-alunite and quartz-dickite-kaolinite alteration.
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Clay minerals are mainly illite and chlorite, with only traces of smectite, vermiculite and kaolinite.
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Barite, sphalerite, and calcite are the most abundant vein minerals; pyrite, kaolinite, chalcopyrite, galena, and wurtzite are less common.
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The clay is composed of illite and kaolinite, with minor amounts of chlorite and smectite.
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It consists largely of the minerals gibbsite Al (OH) 3, boehmite γ-AlO (OH), and diaspore α-AlO (OH), together with the iron oxides goethite and hematite, the clay mineral kaolinite and small amounts of anatase TiO2.
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Common clays are usually mixtures of clay minerals such as illite, smectite, and kaolinite, together with fine silica and other minor constituents.
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Common cements include clay minerals such as kaolinite, montmorillonite, or illite; quartz or chalcedony; iron oxides such as haematite; or calcite.
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Montmorillonite and vermicullite are the clays with the highest CEC, illite has less, and kaolinite and sesquioxides have a very low CEC.
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The limestone-dolomite breccia is characterized by abundant palygorskite, minor sepiolite, rare kaolinite and near absence of smectite.
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It consists largely of the minerals gibbsite Al (OH) 3, boehmite γ-AlO (OH), and diaspore α-AlO (OH), together with the iron oxides goethite and hematite, the clay mineral kaolinite and small amounts of anatase TiO2.
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In the presence of kaolinite and illite, aggregate sizes were smaller and sinking rates lower than in the presence of smectite and quartz.
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The region is characterized by permafrost, and smectite and kaolinite are the common authigenic clay minerals in the soils.
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The clay is composed of illite and kaolinite, with minor amounts of chlorite and smectite.
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Although each mound had substantial amounts of quartz and kaolinite, minerals that reflected differences in mound material included magnetite, gypsum, hornblende, hematite, goethite, and feldspars.
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Mineralogically, clay may contain a variety of components such as kaolinite, vermiculite, illite, chlorite and montmorillonite.
Chapter 5
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The Thorium versus Potassium cross-plot confirms illite as being the main clay and kaolinite as the secondary clay mineral.
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Attachment of quartz and kaolinite to the surface of lobster eggs demonstrates experimentally for the first time that soft tissues could fossilize in pre-existing minerals.
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The Thorium versus Potassium cross-plot confirms illite as being the main clay and kaolinite as the secondary clay mineral.
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In this case the surrounding sediment matrix is dominated by detrital quartz and illite along with various other clay minerals (e.g. kaolinite and chlorite).
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It consists largely of the minerals gibbsite Al (OH) 3, boehmite γ-AlO (OH), and diaspore α-AlO (OH), together with the iron oxides goethite and hematite, the clay mineral kaolinite and small amounts of anatase TiO2.
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Barite, sphalerite, and calcite are the most abundant vein minerals; pyrite, kaolinite, chalcopyrite, galena, and wurtzite are less common.
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Experiment research conducted on calcination of kaolinite from coal measure regarding the influential factors on whiteness of the final product.
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Although each mound had substantial amounts of quartz and kaolinite, minerals that reflected differences in mound material included magnetite, gypsum, hornblende, hematite, goethite, and feldspars.
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Vein minerals are barite, calcite, chalcopyrite, kaolinite, pyrite, sphalerite, and wurtzite.
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Vein minerals are barite, calcite, chalcopyrite, kaolinite, pyrite, sphalerite, and wurtzite.
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Sandstones with this component contain authigenic hematite intergrown with kaolinite and illite and replacing muscovite.
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One red tubular pipe was recognized as Kansas pipestone, which, while normally consisting dominantly of quartz and pyrophyllite, can have traces of both kaolinite and, commonly, muscovite.
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Common clays are usually mixtures of clay minerals such as illite, smectite, and kaolinite, together with fine silica and other minor constituents.
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In addition, the influence of structural property of kaolinite to wave velocities and dynamic mechanical parameters are analysed.
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The effect of four small-molecule organic regulator to three single minerals such as diaspore, pyrophyllite and kaolinite was investigated using sodium oleate as collector.
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There are, in fact, several distinct types of clay, the principal ones being: kaolinite, which is relatively stable, illite, which is of average stability, and montmorillonite, which is highly sensitive to water (causing swelling, etc).
Chapter 4
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Clay minerals are mainly illite and chlorite, with only traces of smectite, vermiculite and kaolinite.
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The predominant clay mineral constituents in lake muds from both regions include smectite, illite-smectites and lesser kaolinite.
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The effect of four small-molecule organic regulator to three single minerals such as diaspore, pyrophyllite and kaolinite was investigated using sodium oleate as collector.
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The Thorium versus Potassium cross-plot confirms illite as being the main clay and kaolinite as the secondary clay mineral.
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Kaolinite clays are mainly composed of the clay mineral kaolin.
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The Thorium versus Potassium cross-plot confirms illite as being the main clay and kaolinite as the secondary clay mineral.
