Abstract
Although submarine ground-water discharge is recognised as being of physical and ecological significance, direct measurements are rare, and calculations are hampered by a lack of offshore data. Classification of the world's coast with respect to its potential, submarine ground-water contribution would help to focus attention on the most important areas and to extrapolate existing data. A classification may be based on relevant physical/climatological parameters (e.g. precipitation, soil type etc.), or geologic/geomorphic classes (e.g. karst, coastal plain, etc.), or on a collection of state parameters. State parameters for a coastal ground-water typology may include aquifer thickness, onshore hydraulic gradient, anisotropy and fractal dimension of the shoreline. Topographic gradient can serve as a surrogate for the hydraulic gradient. A fourth type of classification may be based on the distribution of salinity in the subterranean estuary but adequate subsurface data are not yet available.
| Original language | English |
|---|---|
| Pages (from-to) | 99-108 |
| Number of pages | 10 |
| Journal | Journal of Sea Research |
| Volume | 46 |
| Issue number | 2 |
| DOIs | |
| State | Published - 2001 |
Keywords
- Ground water
- Littoral zone
- Pore water
- Sediment-to-water exchange
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