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Dep. of Agronomy, Ohio State Univ., Ohio Agricultural Research and Development Center, Wooster, OH 44691
USDA-ARS, North Appalachian Experimental Watershed, P.O. Box 478, Coshocton, OH 43812
*Corresponding author.
ABSTRACT
Flow in soil macropores has been implicated as a mechanism for accelerated movement of agrichemicals into groundwater under conservation tillage practices. Strontium bromide hexahydrate, atrazine (2-chloro-4-ethylamino-6-isopropylamino-1,3,5 triazine), and alachlor (2-chloro-2'-6'-diethyl-N-[methoxymethyl]-acetanilide) were surface applied to 18 undisturbed 0.3 by 0.3 by 0.3 m soil blocks collected from three Ohio soils subject to long-term no-till (NT) and moldboard plowing (MP). Two 30-mm rains were applied to the block surface, and leachate was collected from 64 cells at the bottom of each block. Leachate volume, amount of chemicals leached, and visible pore area on bottom surfaces were determined for each cell. Semivariograms of cell leachate volumes revealed that water flow in both NT and MP soils is spatially uncorrelated at a scale of 30 to 300 mm. Principal component analysis at the cell level demonstrated that water flow in both NT and MP blocks followed preferential pathways. The NT blocks transmitted larger water volumes and chemical amounts than MP blocks; however, differences were rarely significant. Principal component analysis of transport in individual blocks suggested that the tillage differences resulted from a higher proportion of strongly preferential pathways in NT blocks. Discriminant analysis yielded significant separation in the soil hydraulic behavior as influenced by tillage and demonstrated the interaction in this behavior between soil type and tillage treatment. It has become clearer that rainfall timing and intensity following chemical application may overshadow tillage effects on water and chemical transport in soils.
Joint contribution of OSU-OARDC and the USDA-ARS.
Received for publication January 31, 1992.
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