The macropore and micropore domains of a soil system were considered to be hydraulically distinct. Drainage and solute transport through the soil were then characterized by mixed probability distributions. The components of the mixed probability distributions were used to represent the distinct proc
SW—Soil and Water: Two-component Analysis of Flow through Macroporous Soil
✍ Scribed by J.Y. Diiwu; R.P. Rudra; W.T. Dickinson; G.J. Wall
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 139 KB
- Volume
- 78
- Category
- Article
- ISSN
- 0021-8634
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✦ Synopsis
Subsurface hydrographs, obtained during rainfall simulation on 1 m by 1 m plots, were separated into macropore and micropore components by application of a dual-porosity concept and mass balance analysis. The corresponding solute concentrations in the two domains were also determined by mass balance analysis. Time-domain re#ectometry was then used to estimate similar out#ow hydrographs and breakthrough curves at an upper depth in the A horizon of the soil pro"le. The results show that the macropores contributed from 6 to 54% of total subsurface #ow and from 1 to 61% of total solute mass transported through the soil pro"le.
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