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Erosion from Alfalfa Established with Oat under Conservation Tillage

Dep. of Soil Science, 1525 Observatory Drive

J. D. Doll and D. J. Undersander

Dep. of Agronomy, Univ. of Wisconsin, Madison, WI 53706

* Corresponding author ( ncwollen{at}facstaff.wisc.edu).

ABSTRACT

Conservation tillage (CT) methods reduce soil erosion, but effects on establishing alfalfa (Medicago sativa L.) are not well known. Oat (Avena sativa L.) is often planted with alfalfa to reduce erosion during establishment, but results are not well documented. We hypothesized that the inclusion of oat during establishment would not be as effective as CT at reducing soil erosion. Moldboard plowing (MB) was compared with two CT practices of disking (DK) and no-till (NT), with alfalfa planted alone (SOLO) or with a companion oat crop (COMP). The study was conducted in 1992 and 1993 on Rozetta silt loam soils (fine-silty, mixed, mesic Typic Hapludalfs) following corn (Zea mays L.) each year. Simulated rainfall, 72 mm h^–1 for 1 h, was applied twice per growing season, at planting (1 wk) and during oat canopy development (4 wk). Runoff was reduced from 28 mm in MB plots to 13 mm in CT plots at planting in 1992. Four weeks after planting in 1993, runoff was reduced from 47 mm in SOLO to 44 mm in COMP. Averaged across all simulations, sediment concentration was 23.3 g L^–1 for MB and 3.2 g L^–1 for CT. The 2-yr mean soil loss dropped from 644 g m^–2 in MB to 94 g m^–2 in CT at planting. Mean treatment erosion was reduced 85% by canopy in 1992, a dry year. The wet 1993 growing season had several severe crusting rainstorms that induced large MB soil loss (2173 g m^–2) 4 wk after planting. Companion cropping reduced MB soil loss 46% (from 2827 to 1520 g m^–2) in 1993 and DK and NT further reduced soil loss to 235 and 123 g m^–2. Forage biomass was unaffected by treatment in 1992.

Received for publication January 10, 1994.

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