S. Baskaran et al., EFFECT OF DRYING OF SOILS ON THE ADSORPTION AND LEACHING OF PHOSPHATEAND 2,4-DICHLOROPHENOXYACETIC ACID, Australian Journal of Soil Research, 32(3), 1994, pp. 491-502
Surface samples of an allophanic (Patua silt loam) and a non-allophani
c (Tokomaru silt loam) soil were used to examine the effects of drying
on the adsorption and leaching of phosphate and 2,4-dichlorophenoxyac
etic acid (2,4-D). Phosphate and 2,4-D adsorption isotherms and adsorp
tion kinetics were determined for field-moist, air-dried and oven-drie
d soil samples using KH2PO4 and C-14 labelled 2,4-D. In a separate exp
eriment, the leaching of a pulse of phosphate or 2,4-D was examined us
ing soil columns. The Patua silt loam adsorbed 4-7 times more phosphat
e and 2,4-D than the Tokomaru silt loam. Compared with field-moist soi
l, both air-dried and oven-dried soil increased (2-5 times) the adsorp
tion of phosphate, and oven-dried soil decreased the adsorption of 2,4
-D. The adsorption kinetics indicated that there was no effect of dryi
ng on the rate of adsorption of either phosphate or 2,4-D. In column e
xperiments, there was less leaching of phosphate and 2,4-D from the Pa
tua soil than from the Tokomaru soil. In both soils, there was no effe
ct of drying on the leaching of phosphate, whereas oven-drying increas
ed the leaching of 2,4-D. Solubilization of organic matter during dryi
ng increased the accessibility of P to adsorption sites on the mineral
surface and thereby increased the adsorption, whereas the water-solub
le organic matter bound 2,4-D and thereby decreased the apparent adsor
ption onto soil and increased leaching.