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Microbial and Photolytic Dissipation of Imazaquin in Soil

Published online by Cambridge University Press:  12 June 2017

G. W. Basham
Affiliation:
Univ. Arkansas, Altheimer Lab., Rte. 11, Box 83, Fayetteville, AR 72703
T. L. Lavy
Affiliation:
Univ. Arkansas, Altheimer Lab., Rte. 11, Box 83, Fayetteville, AR 72703

Abstract

Microbial degradation of imazaquin {2-[4,5-dihydro-4-methyl-4-(1-methylethyl)-5-oxo-1H-imidazol-2-yl]-3-quinolinecarboxylic acid} was monitored by measuring 14CO2 evolution for 7 months under controlled laboratory conditions. Up to 10% of the 14C chain-labeled imazaquin that was applied to a Crowley silt loam was evolved as 14CO2 in 7 months. Less evolution of 14CO2 occurred on a Sharkey silty clay, a soil with higher clay and organic matter content, than on silt loam soils. The loss of 66 to 100% of the imazaquin applied to a Crowley silt loam incubated for 8 months at 18 C or 35 C, respectively, suggested that metabolic changes in addition to CO2 evolution were occurring. Rapid loss of imazaquin phytotoxicity occurred when soils were held at warm-moist (35 C and −33 kPa) conditions conducive to microbial growth. Imazaquin was more persistent in soils stored under cool, dry (18 C and −100 kPa) conditions. Imazaquin on a soil surface dissipated rapidly when exposed to ultraviolet light or sunlight. Photodecomposition could be a major mode of imazaquin dissipation if this herbicide is allowed to remain on the soil surface.

Type
Soil, Air, and Water
Copyright
Copyright © 1987 by the Weed Science Society of America 

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References

Literature Cited

1. Basham, G. W., Lavy, T. L., Oliver, L. R., and Scott, H. D. 1987. Imazaquin persistence in three Arkansas soils. Weed Sci. 35: 576582.Google Scholar
2. Braverman, M. P., Lavy, T. L., and Barnes, C. L. 1986. The degradation and bioactivity of metolachlor in the soil. Weed Sci. 34: 479484.Google Scholar
3. Brewer, F., Lavy, T. L., and Talbert, R. E. 1982. Effects of flooding on dinitroaniline persistence in soybean (Glycine max) — rice (Oryza sativa) rotations. Weed Sci. 30:531539.CrossRefGoogle Scholar
4. Crosby, D. G. and Tutass, H. O. 1966. Photodecomposition of 2,4-dichlorophenoxyacetic acid. J. Agric. Food Chem. 14:596599.Google Scholar
5. Gilmour, J. T., Clark, M. D., and Sigua, G. C. 1985. Estimating net nitrogen mineralization from carbon dioxide evolution. Soil Sci. Soc. Am. J. 49:13981402.Google Scholar
6. Goetz, A. J., Wehtje, G., Walker, R. H., and Hajek, B. 1986. Soil solution and mobility characterization of imazquin. Weed Sci. 34:788793.Google Scholar
7. Liang, T. T. and Lichtenstein, E. P. 1976. Effects of soil and leaf surfaces on photodecomposition of 14C-azinphosmethyl. J. Agric. Food Chem. 24:12051210.Google Scholar
8. Messersmith, C. C., Burnside, O. C., and Lavy, T. L. 1971. Biological and non-biological dissipation of trifluralin from soil. Weed Sci. 19:285290.Google Scholar
9. Ogram, A. V., Jessup, R. E., Ov, L. T., and Rao, P. S. C. 1985. Effects of sorption on biological degradation rates of 2,4-dichlorophenoxyacetic acid in soils. Appl Environ. Microbiol. 49:582587.CrossRefGoogle ScholarPubMed
10. Roeth, F. W., Lavy, T. L., and Burnside, O. C. 1969. Atrazine degradation in two soil profiles. Weed Sci. 17:202205.Google Scholar