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Factors Influencing Microbial Degradation of 14C-Glyphosate to 14CO2 in Soil

Published online by Cambridge University Press:  12 June 2017

Loren J. Moshier
Affiliation:
Dep. Crop and Soil Sci., Michigan State Univ., East Lansing, MI 48824
Donald Penner
Affiliation:
Dep. Crop and Soil Sci., Michigan State Univ., East Lansing, MI 48824

Abstract

14C-glyphosate [N-(phosphonomethyl)glycine] degradation to 14CO2 was examined in a Spinks sandy loam, Collamer silt loam, and a Norfolk loamy sand. After 32 days, 40, 9.5, and 3% of the 14C-glyphosate was recovered as 14CO2 in the three soils, respectively. The degradation was primarily microbial. Phosphate additions stimulated 14C-glyphosate degradation to a limited extent in the Collamer silt loam but not in the Norfolk loamy sand. Additions of Fe+++ and Al+++ ions reduced degradation in the Spinks sandy loam. It is postulated that formation of colloidal Fe and Al precipitates in modified soils with concomitant adsorption of 14C-glyphosate is responsible for decreased availability of 14C-glyphosate to microorganisms. Mn++ additions were found to increase degradation. Spinks soil and carbon substrate amendments failed to substantially increase degradation rates in both soils with low degradation rates.

Type
Research Article
Copyright
Copyright © 1978 by the Weed Science Society of America 

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