Location: Agroecosystems Management ResearchTitle: Depth dependence of chisel plow tillage erosion) Author
Submitted to: Soil & Tillage Research
Publication Type: Peer reviewed journal
Publication Acceptance Date: 6/29/2012
Publication Date: 12/28/2012
Citation: Logsdon, S.D. 2012. Depth dependence of chisel plow tillage erosion. Soil & Tillage Research. 128:119-124. Interpretive Summary: Tillage tools loosen and move soil that can then be pulled downslope due to gravity. This results in soil loss from the tops of hills, whereas water erosion is most severe at the steepest, mid-slope position. This study showed that a twisted shank chisel plow did not loosen soil very deeply, so only soil near the surface got moved. This surface soil was moved as much as ten feet downslope. The rate of soil movement by the chisel plow was 102 lb/ft. Because the deeper soil did not get loosened, mainly the surface soil was eroded by the chisel plow. This information is primarily important for scientists who study tillage erosion and for those who provide soil management guidance to producers.
Technical Abstract: Tillage disturbs the soil vertically, and throws soil in the tillage direction. Tillage movement and disruption of soil is not uniform vertically or horizontally. Tracers have been used to document either the vertical or the horizontal disturbance by tillage, but few studies have examined both the vertical and horizontal tracer displacement by tillage. The objective is to document the vertical and the down- or up-slope movement of inert tracers by chisel plow. Colored limestone was applied at the soil surface (yellow) or at 10 cm depth (blue) before chisel plowing up or down the slope. Samples were collected vertically close to the tracer application and up or down slope. Tracers were separated from the soil for each vertical and horizontal increment, and bulk densities were determined for each increment. Surface applied tracers declined with depth, and most tracers were above 12 cm depth. Tracers applied at 10-cm depth ended up predominately at 4 to 10 cm depth. Surface applied tracers were moved down slope to greater than 3 m, and upslope to nearly 3 m distance. Tracers applied at 10-cm depth did not move up or down slope much distance, if any, beyond the application zone. The overall erosion flux rate was 104 kg m-1, near the low end of published fluxes. The results confirmed the importance of tillage erosion to soil redistribution, and that chisel plow primarily moves soil near the surface rather than the whole tillage depth.