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In karst topography, there are three component of water recharge area that is from karst formation itself, non-karst area and entrance water from above karst formation. Karst formation have three groundwater systems and between them have connection. At the beginning water enter from the fissure and in this phase diffuse system is dominated and then when solution process developed it will make a result a conduit system and impact increasing count of flow. In this phase call mixed groundwater system. And the system will be developed until conduit system is dominated and it is occur on mature phase of karst.
In karst topography, there are three component of water recharge area that is from karst formation itself, non-karst area and entrance water from above karst formation. Karst formation have three groundwater systems and between them have connection. At the beginning water enter from the fissure and in this phase diffuse system is dominated and then when solution process developed it will make a result a conduit system and impact increasing count of flow. In this phase call mixed groundwater system. And the system will be developed until conduit system is dominated and it is occur on mature phase of karst.
White<ref name=White />derived karst aquifers into three conceptual models that is Diffuse-flow karst aquifers that is dominated by diffuse system and low dissolution activity, usually it occur in unsolvable limestone such as dolomite. Free flow karst aquifer it is occur on mixed flow system, in this model groundwater controlled by distribution and direction from each path, and confined-flow karst aquifers its occur usually on beneath rocks that have low permeability and very controlled by layer above the aquifers.
White<ref name=White />derived karst aquifers into three conceptual models that is Diffuse-flow karst aquifers that is dominated by diffuse system and low dissolution activity, usually it occur in unsolvable limestone such as [[dolomite]]. Free flow karst aquifer it is occur on mixed flow system, in this model groundwater controlled by distribution and direction from each path, and confined-flow karst aquifers its occur usually on beneath rocks that have low permeability and very controlled by layer above the aquifers.
==References==
==References==