The origin of hydrogen sulphide found in abnormally saline groundwaters in Kuwait City, Kuwait
The paper presents a qualitative assessment water geochemistry study to understand the deep non-anthropogenic origin of dissolved H 2 S in anomalously abnormal saline groundwaters in Kuwait City. The groundwater samples show geographical variation in water chemistry, salinity, CO 2 and H 2 S concent...
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Published in: | Arabian journal of geosciences Vol. 14; no. 14 |
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Main Authors: | , |
Format: | Journal Article |
Language: | English |
Published: |
Cham
Springer International Publishing
01-07-2021
Springer Nature B.V |
Subjects: | |
Online Access: | Get full text |
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Summary: | The paper presents a qualitative assessment water geochemistry study to understand the deep non-anthropogenic origin of dissolved H
2
S in anomalously abnormal saline groundwaters in Kuwait City. The groundwater samples show geographical variation in water chemistry, salinity, CO
2
and H
2
S concentrations and δ
34
S isotope data. The variation was found to be controlled by the proximity to the abandoned Medina Field. Three geographical areas in Kuwait City with different groundwater properties were identified: Area-A with very high H
2
S concentration (> 100 mg/l); Area-B with moderate H
2
S concentration (50–100 mg/l) and Area-C with low H
2
S concentration (< 50 mg/l). The δ
34
S isotope data of dissolved H
2
S in the groundwater samples showed a range of −8.9 to −12.9‰. The variation of δ
34
S values indicate the origin of H
2
S sourced from mixing of low-temperature sulphate reduction (BSR) with high-temperature thermochemical sulphate reduction (TSR) fluids migrated up-fault from deeper and hotter oil reservoirs through reactivated NE-SW deep-seated faults during recent tectonic events. |
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ISSN: | 1866-7511 1866-7538 |
DOI: | 10.1007/s12517-021-07321-x |