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. |