A standardized quantitative approach was developed toreliably elucidate the effect of increasing
soil moisture onpesticide mineralization. The mineralization of threeaerobically degradable and chemically different
14C-labeled pesticides (isoproturon, benazolin-ethyl, andglyphosate) was studied under controlled conditions inthe laboratory at an identical
soil density of 1.3 g cm
-3. Theagricultural
soils used are characterized by (i) largevariations in
soil texture (sand content 4-88%) and organicmatter content (0.97-2.70% org. C), (ii) fairly diverse
soil-
water retention curves, and (iii) differing pH values. Wequantified the effect of
soil moisture on mineralization ofpesticides and found that (i) at
soil water potential
-20MPa minimal pesticide mineralization occurred; (ii) alinear correlation (
P < 0.0001) exists between increasing
soil moisture (within a
soil water potential range of -20 and-0.015 MPa), and increased relative pesticide mineralization;(iii) optimum pesticide mineralization was obtained at a
soil water potential of -0.015 MPa, and (iv) when
soil moistureapproximated
water holding capacity, pesticide mineralization was considerably reduced. As both selected pesticidesand
soils varied to a large degree, we propose that thecorrelation observed in this study may be also valid in thecase of aerobic degradation of other native and artificialorganic compounds in
soils.