## Abstract The effects of vegetation root distribution on nearβsurface water partitioning can be twoβfold. On the one hand, the roots facilitate deep percolation by rootβinduced macropore flow; on the other hand, they reduce the potential for deep percolation by rootβwaterβuptake processes. Whethe
EVAPOTRANSPIRATION AND SOIL MOISTURE DYNAMICS ON A SEMIARID PONDEROSA PINE HILLSLOPE
β Scribed by David Brandes; Bradford P Wilcox
- Book ID
- 111428485
- Publisher
- American Water Resources Association
- Year
- 2000
- Tongue
- English
- Weight
- 185 KB
- Volume
- 36
- Category
- Article
- ISSN
- 1093-474X
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Soil erosion on hillslopes occurs by processes of soil splash from raindrop impacts and sediment entrainment by surface water flows. This study investigates the process of soil erosion by surface water flow on a stony soil in a semiarid environment. A field experimental method was developed whereby
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