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About Soil Physics - Ch5AA-1
1) Clay minerals form through the chemical weathering of rocks when they come into contact with water and carbon dioxide. Feldspar in particular weathers to form clay minerals like kaolinite. 2) Different clay minerals have distinct structures that give them varying properties. For example, montmorillonite can absorb water between its layers and swell, while kaolinite does not swell. 3) When water contacts clay particles, the negatively charged clay surfaces attract cations in solution. These cations, along with additional water molecules, form a diffuse double layer surrounding each clay particle. The properties of water in this layer differ from normal pore water.
Detailed Information
Author: | ['wijdan 3'] |
---|---|
Publication Year: | 2021 |
Pages: | 11 |
Language: | English |
Format: | |
Price: | FREE |
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