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Effect of soil moisture condition on the conversion rate of oxamyl.

By J.H. Smelt, A. Dekker and M. Leistra

Abstract

The decomposition of oxamyl in four soils under moist conditions was measured in incubation experiments at 15 deg C. Half-lives of oxamyl in soils with moisture tensions of approx. -9.8 X 103 Pa were 13 days in a clay loam, 14 days in a loamy sand, 34 days in a peaty sand and 39 days in a humic loamy sand. The rate of oxamyl decomposition in the clay loam decreased with decreasing soil moisture content down to values for below wilting point. Oxamyl decomposition in the humic loamy sand decreased with decreasing soil moisture content, but increased sharply in the very dry range. (Abstract retrieved from CAB Abstracts by CABI’s permission

Publisher: 'Wageningen University and Research'
Year: 1979
DOI identifier: 10.18174/njas.v27i3.17051
OAI identifier: oai:ojs.pkp.sfu.ca:article/17051

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