Titlebook: Karst Hydrology; Concepts from the Ma William B. White,Elizabeth L. White Book 1989 Springer Science+Business Media New York 1989 Drainage.

Pelvic-Floor

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Water Budget and Physical Hydrology,flow regimes. The textbook version of the hydrologic cycle distributes precipitation as an input term into three components: evapotranspiration, surface runoff, and infiltration. Infiltration water remains in storage and then replenishes surface flow during periods of low precipitation. In a mature

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Flood Hydrology,face and groundwater systems is a floodwater zone. The floodwater zone is defined as the elevation between low stage of the regional water table and the highest flood level per year. The role of the seasonal rise and fall of base level allows the cave passages to drain, breakdown to fall, and sedime

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Chemical Hydrology, wall rock. As a result of this, the internal porosity distribution and flow regimes of carbonate aquifers are continuously changing on a time scale of tens of thousands to millions of years. This phenomenon can be contrasted with silicate rock aquifers where there is indeed an influence of the aqui

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Inelasticity

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Hydraulic Geometry of Cave Passages, comprises the spatial variations in the rates of solution of the bedrock caused by the distribution and geometry of joints and bedding planes, by the variations in solubility of the limestone, and by the distribution of such lithologic features as shale beds, dolomite beds, sandy layers, and chert

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壓倒性勝利

Geomorphic History of the Mammoth Cave System,s are extremely sensitive to environmental conditions while they are forming, and, in relict cave passages, physical weathering and similar disruptive agents are almost totally absent, allowing environmental clues to be preserved long after those on the surface have vanished. This is particularly tr