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Fresh Water and Karst Topography. Hydrologic cycle On a global basis: Water from atmosphere to earth (Precipitation) Water from earth to atmosphere (Evaporation.

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Presentation on theme: "Fresh Water and Karst Topography. Hydrologic cycle On a global basis: Water from atmosphere to earth (Precipitation) Water from earth to atmosphere (Evaporation."— Presentation transcript:

1 Fresh Water and Karst Topography

2 Hydrologic cycle On a global basis: Water from atmosphere to earth (Precipitation) Water from earth to atmosphere (Evaporation and Transpiration) =

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4 Surface Water lakesstreams overland flow Ground water soil pores in rocks regolithsediments

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7 Ground water Water stored beneath the surface, in rock, regolith, soil, sediments Water stored beneath the surface, in rock, regolith, soil, sediments –Flows to surface water –Is recharged (fed) by surface streams

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9 Water percolates downward from soil as gravitational water through aerated zone; reaches water table, which is the top of the saturated zone

10 aquifer: rock or sediment that holds a body of free-flowing ground water

11 Ground water utilization: well pumping causes cone of depression;

12 may cause water table drawdown

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14 Water table and climate

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16 Karst Topography movement of ground water through limestone produces karst landscapes. Characteristics: Sinkholes Sinkholes Caves Caves Springs Springs Lack of surface water Lack of surface water

17 Requirements: (Not all limestone regions are karst regions)  “pure” limestone –(>80% calcium carbonate) abundant rainfall abundant rainfall complex joint patterns in limestone complex joint patterns in limestone

18 Carbonation process: 1. carbon dioxide + water carbonic acid 2. carbonic + calciumcalcium acid carbonatebicarbonate acid carbonatebicarbonate in limestone soluble

19 Soluble product of the reaction is carried away in groundwater Soluble product of the reaction is carried away in groundwater As groundwater seeps through joints, rock is gradually dissolved; beginning of cavern formation As groundwater seeps through joints, rock is gradually dissolved; beginning of cavern formation

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23 Tube passage

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25 As rock dissolves, surface loses underlying support and subsides or collapses: SINKHOLE develops

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29 Travertine Calcite that has precipitated out of groundwater as a mineral deposit carbonation in reverse : calcium calcite + CO 2 + H 2 O bicarbonate travertine

30 Some types of travertine: soda straws soda straws draperies draperies stalactites stalactites stalagmites stalagmites columns columns

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