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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Bibliographic Details
Published in:Arabian journal of geosciences Vol. 14; no. 14
Main Authors: Al-Hajeri, Mubarak Matlak, Amer, Aimen
Format: Journal Article
Language:English
Published: Cham Springer International Publishing 01-07-2021
Springer Nature B.V
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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.
ISSN:1866-7511
1866-7538
DOI:10.1007/s12517-021-07321-x