SUPERCRITICAL CARBON-DIOXIDE FOR DETERMINING ATRAZINE SORPTION BY FIELD-MOIST SOILS

Citation
Ea. Rochette et Wc. Koskinen, SUPERCRITICAL CARBON-DIOXIDE FOR DETERMINING ATRAZINE SORPTION BY FIELD-MOIST SOILS, Soil Science Society of America journal, 60(2), 1996, pp. 453-460
Citations number
36
Categorie Soggetti
Agriculture Soil Science
ISSN journal
03615995
Volume
60
Issue
2
Year of publication
1996
Pages
453 - 460
Database
ISI
SICI code
0361-5995(1996)60:2<453:SCFDAS>2.0.ZU;2-F
Abstract
Supercritical fluid extraction (SFE) with carbon dioxide (SF-CO2) has been used effectively as a method for the extraction of pesticides fro m soils. This study was intended to test its potential as a means of r emoving atrazine from soil water for quantification, to allow calculat ion of sorption coefficients (K(d)s) of atrazine in soils having water contents below field capacity. Low-density SF-CO2 removed atrazine fr om soil solutions without first requiring separation of the solution f rom the soil. The K(d)s obtained by the SF-CO2 method for the topsoil and the lower root zone samples were 1.21 +/- 0.04 and 1.14 +/- 0.03, respectively, while that of the vadose zone soil was 0.16 +/- 0.00. De sorption was rapid; equilibrium was reattained within 7 min. Desorptio n K(d)s for the topsoil and lower root zone soil were constant for suc cessive desorption equilibrations, through removal of approximately 25 % of the applied atrazine from the system. The SF-CO2 method can be us ed to determine the effect of changes in water content and temperature on sorption. It was found that little atrazine can be extracted by th e SF-CO2 method from desiccated soil though large amounts of water (16 %) caused a dramatic increase in the Kd values determined with SF-CO2. The soil solution concentration at 4% soil water content related line arly to the inverse of the temperature (T, K) and the isosteric heat ( Delta H-i) was determined to be - 55.2 +/- 1.7 kJ mol(-1). The SF-CO2 method is promising as a technique to characterize herbicide sorption- desorption from field-moist soils.