Changes

==Karst Aquifers==

==Karst Aquifers==

[[File:UDip_Karst_Fig_3.png|thumb|300px|{{figure number|3}}Conduit flow system and Diffuse flow system (<ref name=White>White, W. B., 1988, Geomorphology and hydrology of karst terrains: New York, Oxford University Press</ref>]]

[[File:UDip_Karst_Fig_3.png|thumb|300px|{{figure number|3}}Conduit flow system and Diffuse flow system<ref name=White>White, W. B., 1988, Geomorphology and hydrology of karst terrains: New York, Oxford University Press</ref>]]

Karst aquifers can describe as a geological formation that could store and flow ground water in moderate count in certain gradient.<ref>Acworth, R. I., 2001, Physical and chemical properties of a DNAPL contaminated sone in a sand aquifer: Quarterly Journal Engineering Geology and Hydrogeology, v. 34, p. 85–98</ref> So it means that karst formation could call as aquifers. Karst aquifers are characterized by a network of conduits and caves the conduits and caves drain the pore space between the limestone grains (intergranular or primary porosity) and the fractures (secondary porosity) formed by joints, bedding planes, and faults.

Karst aquifers can describe as a geological formation that could store and flow ground water in moderate count in certain gradient.<ref>Acworth, R. I., 2001, Physical and chemical properties of a DNAPL contaminated sone in a sand aquifer: Quarterly Journal Engineering Geology and Hydrogeology, v. 34, p. 85–98</ref> So it means that karst formation could call as aquifers. Karst aquifers are characterized by a network of conduits and caves the conduits and caves drain the pore space between the limestone grains (intergranular or primary porosity) and the fractures (secondary porosity) formed by joints, bedding planes, and faults.