Karstsystem
Karstsystem refers to a landscape and groundwater system that develops in soluble rocks such as limestone, dolostone, and gypsum. It is defined by surface dissolution features like sinkholes (dolines), disappearing streams, and by extensive underground drainage through caves and conduits. In a karstsystem, much of the groundwater moves through fractures and enlarged cavities rather than through pore spaces, giving high permeability but irregular storage.
Formation and structure: Karst develops as rainwater, slightly acidic from dissolved carbon dioxide, percolates through the
Hydrology and ecology: Karstsystems can transmit large volumes of water rapidly and are highly heterogeneous, making
Classification and significance: Types depend on rock type—limestone karst, dolostone karst, and gypsum karst—each with characteristic