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- W1506733223 endingPage "321" @default.
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- W1506733223 abstract "The hydrogeology of islands has an important control on their diagenesis. Large-scale circulation within carbonate platforms may be driven by hydraulic head, geothermal effects, and so-called Kohout circulation, and similar effects are reported on a smaller scale in many oceanic islands. In these, as a result of the high permeability of Pleistocene sequences, hydrology is commonly separated into two or more layered systems giving the dual-aquifer concept common among reef islands. Rainfall is an important first-order control on the volume and characteristics to the freshwater body. In small islands, the base of the freshwater body is effectively truncated as a result of the relatively rapid flow of saltwater beneath. The tidal lag within islands decreases with distance from the shore but is primarily a response to local variations in permeability. The compositions of meteoric waters vary as a result of their passage through rocks. They may be oversaturated or undersaturated with respect to calcite and aragonite, but simultaneously saturated with respect to dolomite, particularly when they are mixing with seawater. Thus, locally, groundwaters may be responsible for dissolution, neomorphism, or dolomitization of the rocks through which they pass." @default.
- W1506733223 created "2016-06-24" @default.
- W1506733223 creator A5023388557 @default.
- W1506733223 creator A5085840786 @default.
- W1506733223 date "2009-01-01" @default.
- W1506733223 modified "2023-09-26" @default.
- W1506733223 title "Chapter Seven Reef Hydrogeology" @default.
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