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Effect of Soil and Climate on Herbicide Dissipation

Published online by Cambridge University Press:  12 June 2017

O. C. Burnside ,
C. R. Fenster ,
G. A. Wicks  and
J. V. Drew
O. C. Burnside
Affiliation:
Department of Agronomy at Lincoln
C. R. Fenster
Affiliation:
Scotts Bluff Station at Mitchell
G. A. Wicks
Affiliation:
North Platte Station at North Platte
J. V. Drew
Affiliation:
Department of Agronomy at Lincoln, Nebraska
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Abstract

The persistence of five herbicides in six soils across Nebraska can be ranked from greatest to least as follows: 5-bromo-3-isopropyl-6-methyluracil (isocil) at 5 and 25 1b/A, 2-chloro-4,6-bis-(isopropylamino)-s-triazine (propazine) at 3 and 9 1b/A, 2-chloro-4-ethylamino-6-isopropylamino-s-triazine (atrazine) at 3 and 9 1b/A, trichlorobenzyl chloride (hereinafter referred to as TCBC) at 7 and 49 1b/A, and 3-(3,4-dichlorophenyl)-1-methoxyl-1-methylurea (linuron) at 3 and 9 1b/A. Soil texture differences (sandy loam, very fine sandy loam, silt loam, and silty clay loam) had a greater influence on herbicide residue carryover than did climatic differences across Nebraska during 1962 to 1968. Soil carryover of herbicide residues was greater in coarse rather than fine-textured soils and in the drier regions of western than in eastern Nebraska. Leaching of herbicides into the soil profile was an avenue of herbicide dissipation.

Type
Research Article
Information
Weed Science , Volume 17 , Issue 2 , April 1969 , pp. 241 - 245
Copyright
Copyright © 1969 Weed Science Society of America 

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References

Literature Cited

1. Birk, L. A. and Roadhouse, F. E. B. 1964. Penetration of and persistence in soil of the herbicide atrazine. Can. J. Plant Sci. 44:21–27.Google Scholar
2. Burnside, O. C., Fenster, C. R., and Wicks, G. A. 1963. Dissipation and leaching of monuron, simazine, and atrazine in Nebraska soils. Weeds 11:209–213.Google Scholar
3. Harris, C. I. 1966. Adsorption, movement, and phototoxicity of monuron and s-triazine herbicides in soil. Weeds 14:6–10.Google Scholar
4. Hartley, G. S. 1964. Herbicide behaviour in the soil, p. 111–161. In Audus, L. J. (ed.). The Physiology and Biochemistry of Herbicides. Academic Press, New York.Google Scholar
5. Hill, G. D., McGahen, J. W., Baker, H. M., Finnerty, D. W., and Bingeman, C. W. 1955. The fate of substituted urea herbicides in agricultural soils. Agron. J. 47:93–104.Google Scholar
6. Jordon, L. S., Day, B. E., and Clerx, W. A. 1964. Photodecomposition of triazines. Weeds 12:5–6.Google Scholar
7. Kearney, P. C., Sheets, T. J., and Smith, J. W. 1964. Volatility of seven s-triazines. Weeds 12:83–87.Google Scholar
8. Phillips, W. M. 1968. Persistence and movement of 2,3,6-TBA in soil. Weed Sci. 16:144–148.Google Scholar
9. Rodgers, E. G. 1968. Leaching of seven s-triazines. Weed Sci. 16:117–120.Google Scholar
10. Roeth, F. W., Lavy, T. L., and Burnside, O. C. 1969. Atrazine degradation in two soil profiles. Weed Sci. 17:202–205.Google Scholar
11. Talbert, Ronald E. and Hale Fletchall, O. 1964. Inactivation of simazine and atrazine in the field. Weeds 12:33–37.CrossRefGoogle Scholar
12. Upchurch, R. P., Keaton, J. A., and Selman, F. L. 1968. Soil sterilization properties of monuron, diuron, simazine, and isocil. Weed Sci. 16:358–364.Google Scholar
13. Upchurch, R. P. and Mason, D. D. 1962. The influence of soil organic matter on the phytotoxicity of herbicides. Weeds 10:9–14.Google Scholar
14. Upchurch, R. P. and Pierce, W. C. 1957. The leaching of monuron from Lakeland sand soil. Part I. The effect of amount, intensity, and frequency of simulated rainfall. Weeds 5:321–330.Google Scholar