Farshad Alijani , Narges Bayat , Hamid Reza Nassery , Gesine D. Lorenz , Florian Heine , Matthew I. Leybourne
{"title":"伊朗西南部地下水水化学及烃污染岩溶含水层成因研究","authors":"Farshad Alijani , Narges Bayat , Hamid Reza Nassery , Gesine D. Lorenz , Florian Heine , Matthew I. Leybourne","doi":"10.1016/j.ejrh.2025.102379","DOIUrl":null,"url":null,"abstract":"<div><h3>Study region</h3><div>Khuzestan, Ilam, Lorestan, and Chaharmahal and Bakhtiari provinces in southwest of Iran.</div></div><div><h3>Study focus</h3><div>In this study, conventional geochemical, stable isotopes of H<sub>2</sub>O (δ<sup>2</sup>H, δ<sup>18</sup>O), SO<sub>4</sub> (δ<sup>34</sup>S, δ<sup>18</sup>O), and dissolved inorganic carbon (δ<sup>13</sup>C<sub>DIC</sub>) were employed on the samples collected in February 2021, August 2021, and February 2022 from SW Iran. By the use of hydrogeochemical diagrams, sulfuric samples (SS), non-sulfuric samples (NSS), and oil field water (OFW) samples in karst aquifers have been distinguished.</div></div><div><h3>New hydrological insights for the region</h3><div>The findings reveal that: (1) the major chemical composition of the SS, NSS, and OFW samples consist of CaSO<sub>4</sub>, CaHCO<sub>3</sub>, and NaCl types, respectively; (2) the δ<sup>2</sup>H<sub>H2O</sub> values range between −17.37 and −15.86 ‰ V-SMOW and the δ<sup>18</sup>O<sub>H2O</sub> values range between −4.49 and −4.18 ‰ V-SMOW for the SS and NSS, indicating that they originated from local rainwater; (3) the δ<sup>34</sup>S<sub>SO4</sub> and δ<sup>18</sup>O<sub>SO4</sub> values of dissolved sulfate of SS, NSS, and OFW indicate that the sulfate resulted from interactions between water and rocks, particularly evaporitic rocks such as gypsum and anhydrite; and (4) the δ<sup>13</sup>C<sub>DIC</sub> values vary extensively, ranging from −16 ‰ to + 7 ‰ V-PDB. Higher δ<sup>13</sup>C<sub>DIC</sub> signatures are consistent with biogeochemical processes (i.e., methanogenesis) or exchange with marine carbonates. (5) The concentration of total petroleum hydrocarbons (TPH) ranged from 26.3 to 19,670 μg/L in the groundwater samples.Toluene was the most abundant species of BTEX in all samples.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"59 ","pages":"Article 102379"},"PeriodicalIF":4.7000,"publicationDate":"2025-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Insights into groundwater hydrochemistry and origin of the hydrocarbon contaminated karst aquifers, SW Iran\",\"authors\":\"Farshad Alijani , Narges Bayat , Hamid Reza Nassery , Gesine D. Lorenz , Florian Heine , Matthew I. Leybourne\",\"doi\":\"10.1016/j.ejrh.2025.102379\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><h3>Study region</h3><div>Khuzestan, Ilam, Lorestan, and Chaharmahal and Bakhtiari provinces in southwest of Iran.</div></div><div><h3>Study focus</h3><div>In this study, conventional geochemical, stable isotopes of H<sub>2</sub>O (δ<sup>2</sup>H, δ<sup>18</sup>O), SO<sub>4</sub> (δ<sup>34</sup>S, δ<sup>18</sup>O), and dissolved inorganic carbon (δ<sup>13</sup>C<sub>DIC</sub>) were employed on the samples collected in February 2021, August 2021, and February 2022 from SW Iran. By the use of hydrogeochemical diagrams, sulfuric samples (SS), non-sulfuric samples (NSS), and oil field water (OFW) samples in karst aquifers have been distinguished.</div></div><div><h3>New hydrological insights for the region</h3><div>The findings reveal that: (1) the major chemical composition of the SS, NSS, and OFW samples consist of CaSO<sub>4</sub>, CaHCO<sub>3</sub>, and NaCl types, respectively; (2) the δ<sup>2</sup>H<sub>H2O</sub> values range between −17.37 and −15.86 ‰ V-SMOW and the δ<sup>18</sup>O<sub>H2O</sub> values range between −4.49 and −4.18 ‰ V-SMOW for the SS and NSS, indicating that they originated from local rainwater; (3) the δ<sup>34</sup>S<sub>SO4</sub> and δ<sup>18</sup>O<sub>SO4</sub> values of dissolved sulfate of SS, NSS, and OFW indicate that the sulfate resulted from interactions between water and rocks, particularly evaporitic rocks such as gypsum and anhydrite; and (4) the δ<sup>13</sup>C<sub>DIC</sub> values vary extensively, ranging from −16 ‰ to + 7 ‰ V-PDB. 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Insights into groundwater hydrochemistry and origin of the hydrocarbon contaminated karst aquifers, SW Iran
Study region
Khuzestan, Ilam, Lorestan, and Chaharmahal and Bakhtiari provinces in southwest of Iran.
Study focus
In this study, conventional geochemical, stable isotopes of H2O (δ2H, δ18O), SO4 (δ34S, δ18O), and dissolved inorganic carbon (δ13CDIC) were employed on the samples collected in February 2021, August 2021, and February 2022 from SW Iran. By the use of hydrogeochemical diagrams, sulfuric samples (SS), non-sulfuric samples (NSS), and oil field water (OFW) samples in karst aquifers have been distinguished.
New hydrological insights for the region
The findings reveal that: (1) the major chemical composition of the SS, NSS, and OFW samples consist of CaSO4, CaHCO3, and NaCl types, respectively; (2) the δ2HH2O values range between −17.37 and −15.86 ‰ V-SMOW and the δ18OH2O values range between −4.49 and −4.18 ‰ V-SMOW for the SS and NSS, indicating that they originated from local rainwater; (3) the δ34SSO4 and δ18OSO4 values of dissolved sulfate of SS, NSS, and OFW indicate that the sulfate resulted from interactions between water and rocks, particularly evaporitic rocks such as gypsum and anhydrite; and (4) the δ13CDIC values vary extensively, ranging from −16 ‰ to + 7 ‰ V-PDB. Higher δ13CDIC signatures are consistent with biogeochemical processes (i.e., methanogenesis) or exchange with marine carbonates. (5) The concentration of total petroleum hydrocarbons (TPH) ranged from 26.3 to 19,670 μg/L in the groundwater samples.Toluene was the most abundant species of BTEX in all samples.
期刊介绍:
Journal of Hydrology: Regional Studies publishes original research papers enhancing the science of hydrology and aiming at region-specific problems, past and future conditions, analysis, review and solutions. The journal particularly welcomes research papers that deliver new insights into region-specific hydrological processes and responses to changing conditions, as well as contributions that incorporate interdisciplinarity and translational science.