Abstract
The Permo-Triassic Kangan gasfield in southern Iran is composed of an aquifer, the Kangan Aquifer (KA), and an overlying gas reservoir. It is located in the Kangan and Dalan Formations and consists predominantly of limestone
and dolomite. The Kangan gasfield is exploited from 36 wells at depths from 2300 to 2860 m. The quality of the produced formation waters (PFW) varies from fresh to saline, with salinities of up to 60,000 mg/L. The present
study aims to identify the origin of the salinity of the PFWs. The concentration of major ions, Li, Sr and Br, as well as δ18O, δD, 87Sr/86Sr, δ37Cl and δ81Br isotope compositions of the KA water and PFW samples, a fresh and
a brine spring, and the Persian Gulf water were all measured. The suite of isotopic (δ37Cl and δ81Br) and hydrochemical data (Li, Cl and Br concentrations and CF index) in this study indicates that the salinity origin of
the PFWs is evaporated seawater, which could be either the KA water or the intergranular saturated brine in the Kangan Gas Reservoir (KGR), both derived from Permo-Triassic evaporated seawater. δ18O and 87Sr/86Sr
data exclude the KA water as the source of the saline PFW, leaving the intergranular brine of the KGR as the most likely source although further isotopic and geochemical tests are needed to verify this. This work also proposes, for the first time, the use of a Li/Cl versus Br/Cl diagramto distinguish between evaporate formationwater, water modified by halite dissolution and fresh water. It is recommended to apply these comprehensive methods to deep brine aquifers, especially related to gasfields.
and dolomite. The Kangan gasfield is exploited from 36 wells at depths from 2300 to 2860 m. The quality of the produced formation waters (PFW) varies from fresh to saline, with salinities of up to 60,000 mg/L. The present
study aims to identify the origin of the salinity of the PFWs. The concentration of major ions, Li, Sr and Br, as well as δ18O, δD, 87Sr/86Sr, δ37Cl and δ81Br isotope compositions of the KA water and PFW samples, a fresh and
a brine spring, and the Persian Gulf water were all measured. The suite of isotopic (δ37Cl and δ81Br) and hydrochemical data (Li, Cl and Br concentrations and CF index) in this study indicates that the salinity origin of
the PFWs is evaporated seawater, which could be either the KA water or the intergranular saturated brine in the Kangan Gas Reservoir (KGR), both derived from Permo-Triassic evaporated seawater. δ18O and 87Sr/86Sr
data exclude the KA water as the source of the saline PFW, leaving the intergranular brine of the KGR as the most likely source although further isotopic and geochemical tests are needed to verify this. This work also proposes, for the first time, the use of a Li/Cl versus Br/Cl diagramto distinguish between evaporate formationwater, water modified by halite dissolution and fresh water. It is recommended to apply these comprehensive methods to deep brine aquifers, especially related to gasfields.
Original language | English |
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Pages (from-to) | 62-75 |
Number of pages | 14 |
Journal | Chemical Geology |
Volume | 384 |
DOIs | |
Publication status | Published - 2014 |