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Quickly, the cations are distributed around the negatively charged surface of the clay fragments, with the greatest thickness near the surface and reduced thickness with raising range from the surface area. The cations form a favorably charged layer and the dual layer is developed with a negatively charged surface area of the clay particles. The dual layer influences the setups of the clay particles, as well as therefore, the physical as well as mechanical residential properties of the soil are likewise influenced. The interaction of these pressures manages the engineering behavior of soils to a terrific extent. http://www.driftpedia.com/wiki/index.php/Try_This_Out |
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