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ABSTRACT
Using an electrolytic respirometer, agricultural runoff from seven crop and tillage practices were studied to determine the 5-d biochemical oxygen demand (BOD5). Mean BOD5 concentrations for the practices ranged from 10 to 25 mg O2 L–1 as compared to 4 to 56 mg O2 L–1 for individual storm events. In general, there was no difference in BOD5 concentrations between conventional and no-till practices. Biochemical oxygen demand-time relationships were found to best fit a first-order reaction equation. The aqueous phase was the dominant source of BOD5, amounting to 64 ± 17% (1 SD) of the total BOD5 in runoff from notill soybeans, double-cropped with winter wheat (Triticum aestivum L.). However, additional data indicate that conventional tillage practices, producing higher sediment concentrations, may result in a greater proportion of the BOD associated with the sediment phase.
Key Words: water quality first-order reaction reaction rate constant lag phase suspended sediment
1 Contribution from the USDA-ARS, USDA Sedimentation Laboratory, Oxford, MS 38655.
2 Soil Scientist and Chemist, respectively.
Received for publication November 28, 1985.
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