Abstract
Erosion of the productive surface soil from a landscape reduces crop production and alters chemical and physical properties of the soil, especially the thickness of the effective rooting depth and surface horizon thickness. Fast and reliable tools are needed to detect and map the thickness of soil horizons of eroded landscapes to allow for proper management of eroded soil for optimum agricultural production and environmental protection. A truck-mounted, constant-rate profile cone penetrometer was used to determine the horizon thickness and thus map the distribution of various erosion levels of an eroded Dubuque silt loam soil, in southwest Wisconsin, USA. The penetrometer was pushed into the ground with the hydraulic cylinder of a soil probe mounted on a 0.7 ton truck, to a depth of approximately 1.3 m. Data were collected continuously with a datalogger connected to a load cell and a string potentiometer depth gage. The 30° tip of the penetrometer was constructed following the American Society of Agricultural Engineers (ASAE) guidelines. Data collected with the penetrometer correlate well with previously constructed maps of soil erosion distribution for the study site constructed by soil borings using morphological observations, where depth to clay residuum (2Bt2 horizon) was used to determine erosion severity. Depth to clay residuum averaged 0.95, 0.74, and 0.45 m for the slight, moderate, and severe erosion levels, respectively. Of the total study area, approximately 44, 31, and 25 % consisted of slight, moderate, and severe erosion levels, respectively. Three-dimensional (3D) maps of the site were developed using data from the penetrometer. Development of limited invasive tools and methods for mapping eroded soil can aid in land management.
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Arriaga, F.J., Lowery, B., Reinert, D.J., McSweeney, K. (2016). Cone Penetrometers as a Tool for Distinguishing Soil Profiles and Mapping Soil Erosion. In: Hartemink, A., Minasny, B. (eds) Digital Soil Morphometrics. Progress in Soil Science. Springer, Cham. https://doi.org/10.1007/978-3-319-28295-4_25
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DOI: https://doi.org/10.1007/978-3-319-28295-4_25
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