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Claypans restrict infiltration, influence the lateral movement of soil water and agrichemicals, and limit crop production. In many areas of the Midwest, quantification and mapping of the variations in the depth to claypans are important components for research on water-quality and crop production. In an area of Mexico soils in central Missouri, a high correlation between the observed depth to claypans and the response of the EM38 meter was observed. Equations were developed to infer depths and chart the topography of the claypan. Compared with traditional methods of observing this subsurface layer, EM techniques are noninvasive, Less Labor intensive, more economical and can produce large quantities of data in a relatively short period of time.
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Doolittle et al. (1994) studied this question.
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