Publication Date

1-1-1985

Series Number

42

Abstract

Throughflow troughs were installed to assess their effectiveness in quantifying shallow sub-surface flows on hillslopes. The majority of flow was found to occur from decayed root channels in clay sub-soils below the lowest gutter. The conclusion at this site is that shallow throughflow troughs installed on a small scale are not capable of quantifying all of the seepage occurring on hillslopes.

Keywords

Drainage, Measurement, Subsoil, Seepage

Disciplines

Hydrology | Soil Science

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