Chemical evolution of a gas-capped deep aquifer, southwest of Iran

The Kangan Aquifer (KA) is located below a gas reservoir in the crest of the Kangan Anticline, southwest of Iran. This aquifer is composed of Permo-Triassic limestone, dolomite, sandstone, anhydrite and shale. It is characterized by a total dissolved solid of about 332,000 mg/L and Na–Ca–Cl-type wat...

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Veröffentlicht in:	Environmental earth sciences 2014-04, Vol.71 (7), p.3171-3180
Hauptverfasser:	Bagheri, Rahim, Nadri, Arash, Raeisi, Ezzat, Shariati, Ali, Mirbagheri, Mahmud, Bahadori, Farahtaj
Format:	Artikel
Sprache:	eng
Schlagworte:	Aquifers Bacteria Biogeosciences Brine calcium Chemical evolution Diagenesis Dissolved solids Dolomite Earth and Environmental Science Earth Sciences Earth, ocean, space Environmental Science and Engineering Evaporation Exact sciences and technology Geochemistry Geology Hydrogeology Hydrology. Hydrogeology Hydrology/Water Resources ion exchange Ions Limestone Magnesium Manganese Original Article Reservoirs Rocks Sandstone Sea water Seawater sodium Strontium Terrestrial Pollution Trace elements Triassic
Online-Zugang:	Volltext
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