Abstract

ABSTRACT IN an effort to characterize the amount of surface storage in depressions on naturally occurring and surface drained plots, three substantially different surface types were evaluated. Precise topographic information was used to calculate volume of surface storage and to estimate a characteristic depth of storage for each surface type. Average depth of macro relief storage was 5.0 mm for a level surface, 9.01 mm for a sloping surface, and 34.2 mm for a surface with a large depression. Superimposing wide beds and furrows on the surface gave small changes in storage volume, but inundation of the cropped bed surface could be avoided.

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