1990•International Journal of Environmental & Analytical ChemistryRequires access

Movement of Phosphamidon in Soil Columns

K. Gowri Bala Kumari, R. P. Singh, S. K. Saxena

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Abstract

Adsorption and movement of phosphamidon, a systemic non-ionic insecticide, was studied using two different types of Indian soil, clay loam and silt loam, of alluvial origin. Equilibrium adsorption coefficient, K, values determined by batch slurry technique were in the order: clay loam>silt loam. The distribution coefficient, Kd , for both soils in batch adsorption as well as in columns was also calculated. The phosphamidon movement measured in soil columns during water infiltration was in the order: silt loam > clay loam. This order was anticipated from the K and Kd values. A larger amount of water was needed for leaching the phosphamidon to 60 inches in clay loam than in silt loam soil.

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Adsorption and movement of phosphamidon, a systemic non-ionic insecticide, was studied using two different types of Indian soil, clay loam and silt loam, of alluvial origin. Equilibrium adsorption coefficient, K, values determined by batch slurry technique were in the order: clay loam>silt loam. The distribution coefficient, Kd , for both soils in batch adsorption as well as in columns was also calculated. The phosphamidon movement measured in soil columns during water infiltration was in the order: silt loam > clay loam. This order was anticipated from the K and Kd values. A larger amount of water was needed for leaching the phosphamidon to 60 inches in clay loam than in silt loam soil.

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Available abstract

Adsorption and movement of phosphamidon, a systemic non-ionic insecticide, was studied using two different types of Indian soil, clay loam and silt loam, of alluvial origin. Equilibrium adsorption coefficient, K, values determined by batch slurry technique were in the order: clay loam>silt loam. The distribution coefficient, Kd , for both soils in batch adsorption as well as in columns was also calculated. The phosphamidon movement measured in soil columns during water infiltration was in the order: silt loam > clay loam. This order was anticipated from the K and Kd values. A larger amount of water was needed for leaching the phosphamidon to 60 inches in clay loam than in silt loam soil.

Key concepts: Loam, Soil water, Phosphamidon, Leaching (pedology), Soil science, Chemistry, Silt, Adsorption

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