Wc. Koskinen et Ea. Rochette, ATRAZINE SORPTION-DESORPTION IN FIELD-MOIST SOILS, International journal of environmental analytical chemistry, 65(1-4), 1996, pp. 223-230
Methods commonly used to obtain sorption coefficients require that the
soils be above field capacity moisture so that the aqueous phase cont
aining the pesticide to be quantified can be separated from the soil.
We have developed a system using supercritical CO, that can remove the
pesticide from soil solution of unsaturated soil without first requir
ing the separation of the solution from soil. Sorption coefficients in
creased with soil organic carbon and clay contents for three field-moi
st soils. Also, sorption significantly increased in a sand as moisture
content increased from 4.0 to 16% and in a silt loam as moisture incr
eased from 9.6 to 27%. Isosteric heats of sorption were easily determi
ned with the supercritical fluid system and ranged from -10 to -12 kca
l mol(-1) and were correlated to organic carbon and clay contents of t
he soils. Sorption coefficients in field-moist soils were much greater
than are typically obtained with the batch slurry system, while heats
of sorption were much more negative, indicating greater sorption at l
ow moisture contents.