JEQ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 28:1765-1777 (1999)
© 1999 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Baer, U.
Right arrow Articles by Calvet, R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Baer, U.
Right arrow Articles by Calvet, R.
Agricola
Right arrow Articles by Baer, U.
Right arrow Articles by Calvet, R.

Fate of Soil Applied Herbicides: Experimental Data and Prediction of Dissipation Kinetics

U. Baer and R. Calvet*

Unité de Science du Sol, INRA/INA-PG, Centre de Grignon, 78850 Thiverval-Grignon, France.

* Corresponding author (calvet{at}ecgn.grignon.inra.fr).

ABSTRACT

Dissipation kinetics of several soil-applied herbicides [atrazine (6-chloro-2 ethylamino-4 isopropyl-1,3,5-triazine-2,4 diamine), simazine (6-chloro-2,4-diethyl-1,3,5-triazine-2,4-diamine), diuron (3-(3,4-dichloro-phenyl)-1,1-dimethylurea), and sulcotrione (2-(2-chloro-4-mesyl-benzoyl)cyclohexane-1,3-dione)] are studied at three sites having different climatic, pedological, and agronomical characteristics. Field data were obtained during 2 yr, 1993 and 1994. Information was completed by laboratory measurements of adsorption, desorption, and disappearance kinetics obtained at two temperatures (15 and 28°C) and two soil water contents (50 and 90% soil water capacity). Adsorption and desorption conform to the Freundlich description, sulcotrione being the less adsorbed. Laboratory disappearance kinetics can be approximately described with a first-order law under some conditions. Calculated laboratory disappearance rate coefficients are used to simulate field dissipation kinetics in the 0- to 10-cm soil layer, taking into account the effects of soil temperature (Arrhenius formula) and water content (Walker relation). Observed field dissipation kinetics, which are not fully described by a first-order law, can be approximately simulated. Results are discussed from the points of view of agronomy and environment.


Received for publication March 9, 1998.


This article has been cited by other articles:


Home page
J. Environ. Qual.Home page
F. Flores-Cespedes, E. Gonzalez-Pradas, M. Fernandez-Perez, M. Villafranca-Sanchez, M. Socias-Viciana, and M.D. Urena-Amate
Effects of Dissolved Organic Carbon on Sorption and Mobility of Imidacloprid in Soil
J. Environ. Qual., May 1, 2002; 31(3): 880 - 888.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
X. Louchart, M. Voltz, P. Andrieux, and R. Moussa
Herbicide Transport to Surface Waters at Field and Watershed Scales in a Mediterranean Vineyard Area
J. Environ. Qual., May 1, 2001; 30(3): 982 - 991.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1999 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.