Subsurface Lateral Flow in Texture-Contrast (Duplex) Soils and Catchments with Shallow Bedrock
Development-perched watertables and subsurface lateral flows in texture-contrast soils (duplex) are commonly believed to occur as a consequence of the hydraulic discontinuity between the A and B soil horizons. However, in catchments containing shallow bedrock, subsurface lateral flows result from a...
| Main Authors: | , , , |
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| Format: | Article |
| Sprog: | English |
| Udgivet: |
Wiley
2012-01-01
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| Serier: | Applied and Environmental Soil Science |
| Online adgang: | http://dx.doi.org/10.1155/2012/861358 |