CORRECTION FACTORS IN THE DETERMINATION OF MEAN VELOCITY OF OVERLAND FLOW
The velocity of overland flow has been conventionally measured using tracers, but it is difficult to measure the mean flow velocity directly because the centroid of the tracer plume is not easily identified. Consequently, previous investigators have measured the velocity of the leading edge of the p...
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Veröffentlicht in: | Earth surface processes and landforms 1996-06, Vol.21 (6), p.509-515 |
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Sprache: | eng |
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