首页> 外文会议>Annual Meeting of the Clay Minerals Society >DETERMINATION OF LAYER CHARGE OF SMECTITES IN BENTONITES: AN ASSESSMENT OF THE K-SATURATION METHOD
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DETERMINATION OF LAYER CHARGE OF SMECTITES IN BENTONITES: AN ASSESSMENT OF THE K-SATURATION METHOD

机译:膨润土中麦布粘岩层电荷的测定:K饱和法的评估

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摘要

Characterization of smectite layer charge is of economic and geologic importance, because layer charge strongly affects key smectite properties such as swelling, cation exchange capacity, and ion exchange selectivity. These properties are important for the various applications of bentonites. Smectites usually are structurally and compositionally heterogeneous, and this is reflected in the layer charge. We have proposed a method for determination of layer charge of smectites (Christidis & Eberl, 2003).
机译:蒙脱石层电荷的表征具有经济和地质重要性,因为层电荷强烈影响关键的蒙脱石特性,如溶胀,阳离子交换能力和离子交换选择性。这些属性对于膨润土的各种应用很重要。蒙脱石通常是在结构上和合成的非均相的,并且这反映在层电荷中。我们提出了一种确定蒙脱石层电荷的方法(Christidis&Eberl,2003)。

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