## Abstract Water flow through a melting snow pack modifies its structure and stability and affects the release of water and nutrients into soils and surface waters. Field and laboratory observations indicate a large spatial variability on various scales of the liquid water content and flow, a domi
β¦ LIBER β¦
Effect of fracture roughness on solute transport
β Scribed by Wook Yeo
- Publisher
- The Geological Society of Korea
- Year
- 2001
- Tongue
- English
- Weight
- 266 KB
- Volume
- 5
- Category
- Article
- ISSN
- 1226-4806
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