Cleavage nature,electrokinetics,aggregation and dispersion of kaolinite  被引量:1

Cleavage nature,electrokinetics,aggregation and dispersion of kaolinite

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作  者:胡岳华 孙伟 刘晓文 王淀佐 

机构地区:[1]School of Minerals Processing and Bioengineering

出  处:《中国有色金属学会会刊:英文版》2003年第6期1430-1434,共5页Transactions of Nonferrous Metals Society of China

基  金:Project(G19990 64 90 1)supportedbytheNationalKeyFundamentalResearchandDevelopmentProgramofChina,project(59925412)supportedbytheChinaNationalScienceFundforDistinguishedYoungScholar

摘  要:Quantum chemical simulation calculation shows that kaolinite is cleaved to produce (001) and (001) basal planes. (001) plane is dominant by ([SiO4]) tetrahedral, which interacted easily with hydrogen ion or other positive ions by electrostatic forces or hydrogen bonding. (001) plane is dominant by ([AlO2(OH)4]), which interacted easily with high negativity group such as -O-, -N-, F- etc. The apparent zeta potential and surface points of zero charge(PZC) are different for hard and soft kaolinites depending on their crystallinity index (HI). The self-aggregation between edge and basal plane due to the electrostatic interactions may occur at acidic media. The dispersion of kaolinite particles at alkaline media may be attributed to the electrostatic repulsion between basal planes and/or edges. The aggregation or dispersion behavior is revealed by scan electron microscope and the transmittance measurements for the suspension of kaolinite particles.Quantum chemical simulation calculation shows that kaolinite is cleaved to produce (001) and (001) basal planes. (001) plane is dominant by ([SiO_4]) tetrahedral, which interacted easily with hydrogen ion or other positive ions by electrostatic forces or hydrogen bonding. (001) plane is dominant by ([AlO_2(OH)_4]), which interacted easily with high negativity group such as -O-, -N-, F- etc. The apparent zeta potential and surface points of zero charge(PZC) are different for hard and soft kaolinites depending on their crystallinity index (HI). The self-aggregation between edge and basal plane due to the electrostatic interactions may occur at acidic media. The dispersion of kaolinite particles at alkaline media may be attributed to the electrostatic repulsion between basal planes and/or edges. The aggregation or dispersion behavior is revealed by scan electron microscope and the transmittance measurements for the suspension of kaolinite particles.

关 键 词:高岭石 分散 自聚集 动电学 解理面 

分 类 号:P578.965[天文地球—矿物学] TQ04[天文地球—地质学]

 

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