Formation and Transport of the Sulfonic Acid Metabolites of Alachlor and Metolachlor in Soil

D. S. Aga* and E. M. Thurman
University of Nebraska at Kearney, Kearney, Nebraska 68849, and U.S. Geological Survey, 4821 Quail Crest Place, Lawrence, Kansas 66049
Environ. Sci. Technol., 2001, 35 (12), pp 2455–2460
DOI: 10.1021/es991264s
Publication Date (Web): April 27, 2001
Copyright © 2001 American Chemical Society
*

 Corresponding author phone:  (308)865-8802; fax:  (308)865-8157; e-mail:  agad@unk.edu.

,

 University of Nebraska at Kearney.

,

 U.S. Geological Survey.

Abstract

Alachlor and metolachlor are dechlorinated and transformed into their corresponding ethane sulfonic acid (ESA) metabolites in soil. In a field-disappearance study, it was shown that alachlor ESA was formed at a faster rate and at concentrations 2−4 times higher than metolachlor ESA, conforming with the observed longer disappearance half-life of metolachlor (15.5 d) in the field as compared to alachlor (8 d). Runoff data also showed higher concentrations of alachlor ESA as compared to metolachlor ESA, even though they were applied at the same levels. Data from soil cores showed transport of the ESA compounds in soil to as far down as 75−90 cm below the surface, at concentrations ranging from less than 0.5 μg/L to about 50 μg/L. In contrast, no parent herbicide was detected at these depths. This observation correlates with the higher log Koc values for alachlor (3.33) and metolachlor (3.01) relative to their corresponding ESA metabolites, alachlor ESA (2.26), and metolachlor ESA (2.29).

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History

  • Published In Issue June 15, 2001
  • Received for review November 9, 1999
    Revised manuscript received March 7, 2001
    Accepted March 16, 2001

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