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Ion Exchange Properties of Lateritic Soil from Calicut Kerala


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1 Department of Civil Engineering, Indian Institute of Technology, Kanpur 208016, India
     

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The lateritic soils developed over Precambrian crystalline rocks near Calicut have relatively high Cation Exchange Capacity. At the same time, the soils are highly efficient for phosphate uptake. Both of these properties are traced to the presence of halloysite of intermediate hydration in the soils. Experimental results have been interpreted in terms of the structure of soil minerals.
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  • Ion Exchange Properties of Lateritic Soil from Calicut Kerala

Abstract Views: 165  |  PDF Views: 4

Authors

B. C. Raymahashay
Department of Civil Engineering, Indian Institute of Technology, Kanpur 208016, India
P. R. Bhavana
Department of Civil Engineering, Indian Institute of Technology, Kanpur 208016, India
K. S. Rao
Department of Civil Engineering, Indian Institute of Technology, Kanpur 208016, India
V. K. Mehta
Department of Civil Engineering, Indian Institute of Technology, Kanpur 208016, India

Abstract


The lateritic soils developed over Precambrian crystalline rocks near Calicut have relatively high Cation Exchange Capacity. At the same time, the soils are highly efficient for phosphate uptake. Both of these properties are traced to the presence of halloysite of intermediate hydration in the soils. Experimental results have been interpreted in terms of the structure of soil minerals.