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Flurtamone Adsorption and Mobility in Three Georgia Soils

Published online by Cambridge University Press:  12 June 2017

Thomas C. Mueller  and
Philip A. Banks
Thomas C. Mueller
Affiliation:
Univ. Georgia, Athens, GA 30602
Philip A. Banks
Affiliation:
Univ. Georgia, Athens, GA 30602
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Abstract

Flurtamone and atrazine adsorption to soil was examined using a batch equilibrium method. Flurtamone mobility in packed soil columns under saturated flow conditions was also evaluated. Adsorption was greater for flurtamone than atrazine in the three soils, and the order of adsorption to soil for both herbicides was Greenville sandy clay loam > Cecil loam > Dothan loamy sand. Greater adsorption of each herbicide corresponded to soils with greater organic matter and clay content. The 14C–flurtamone movement under saturated flow conditions in 28–cm soil–packed columns was limited to 16 cm, with no flurtamone leaching from any soil column after the addition of two pore volumes of water. Seventy–five percent of the applied 14C–flurtamone remained in the 0– to 4–cm soil depth in the Greenville sandy clay loam, with less than 5 percent moving to a depth > 4 cm. Flurtamone movement was greater in the Cecil loam and the Dothan loamy sand, with movement in each soil to a depth of 16 and 12 cm, respectively.

Keywords

Flurtamone, 5-(methylamino)-2-phenyl-4-[3-(trifluoromethyl)phenyl]-3-(2H)-furanoneatrazine, 6-chloro-N-ethyl-N′-(1-methylethyl)-1,3,5-triazine-2,4-diamineRE-40885atrazineleachingorganic matterclay contentisotherm
Type
Soil, Air, and Water
Information
Weed Science , Volume 39 , Issue 2 , June 1991 , pp. 275 - 279
Copyright
Copyright © 1991 Weed Science Society of America 

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