Carbonate aquifers typically have complex groundwater flow patterns that result from depositional heterogeneities and postlithification fracturing and karstification. Various sources of information may be used to build a conceptual understanding of flow in the system, including drilling data, well t
โฆ LIBER โฆ
A parsimonious model for simulating flow in a karst aquifer
โ Scribed by Michael E Barrett; Randall J Charbeneau
- Book ID
- 117139471
- Publisher
- Elsevier Science
- Year
- 1997
- Tongue
- English
- Weight
- 791 KB
- Volume
- 196
- Category
- Article
- ISSN
- 0022-1694
No coin nor oath required. For personal study only.
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## Abstract In China, 9ยท5% of the landmass is karst terrain and of that 47,000 km^2^ is located in semiarid regions. In these regions the karst aquifers feed many large karst springs within basins of thousands of square kilometres. Spring discharges reflect the fluctuation of ground water level and