Coupled hydrogeological and geochemical processes and structural controls on geothermal systems in Odisha, India

Geothermal springs in the Mahanadi region represent a low to moderate enthalpy geothermal system with potential for sustainable energy utilization. Integrated hydrogeochemical, geophysical, and geological investigations indicate that water–rock interaction, ion exchange, and structurally controlled fluid circulation govern the system evolution, with the fracture network acting as the primary control on regional fluid migration. Thermal waters are classified as Na–Cl and Ca–Mg–HCO₃ types, whereas non-thermal waters are Ca–HCO₃ type, reflecting limited mixing and meteoric recharge dominance. Elevated Na⁺/Cl⁻ ratios suggest that sodium enrichment in groundwater is mainly controlled by silicate weathering reactions, especially feldspar dissolution, reflecting dominant water–rock interaction processes with minimal marine influence. Key scaling phases include calcite, dolomite, gypsum, and anhydrite, with carbonate precipitation in near surface discharge zones driven by CO₂ degassing, induced supersaturation, leading to active scaling and mineral deposition. VLF-EM surveys delineate conductive fracture networks extending to depths, highlighting structurally controlled pathways for geothermal fluid migration. The estimated average reservoir temperature is $$\:\sim$$ 110 ± 5°C, with fluid circulation occurring at depths of approximately 1.37 ± 0.32 km along the North Khurda Fault and the Mahanadi Graben. Deep carbon gas upwelling further enhances fluid recharge along WNW–ESE trending fracture systems at the Atmalik (Deulajhari) thermal spring. Overall, the geothermal system is strongly structurally and fracture controlled, with regional fluid circulation governed primarily by fault networks, and is hydro-geochemically immature to moderately evolved, warranting further reservoir-scale characterization for sustainable exploitation. Harnessing geothermal energy in the region can effectively reduce CO₂ emissions, support India’s net-zero targets by 2070, and promote local economic development and energy resilience.

Authors

Institutions

Publication Details

Journal
Environmental Earth Sciences
Published
2026-06-29
DOI
https://doi.org/10.1007/s12665-026-13009-w
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Coupled hydrogeological and geochemical processes and structural controls on geothermal systems in Odisha, India

Susmita Goswami, Abhishek. Kumar Rai
Environmental Earth Sciences
Groundwater and Isotope Geochemistry
article

Coupled hydrogeological and geochemical processes and structural controls on geothermal systems in Odisha, India

Susmita Goswami, Abhishek. Kumar Rai
article en

Abstract

Geothermal springs in the Mahanadi region represent a low to moderate enthalpy geothermal system with potential for sustainable energy utilization. Integrated hydrogeochemical, geophysical, and geological investigations indicate that water–rock interaction, ion exchange, and structurally controlled fluid circulation govern the system evolution, with the fracture network acting as the primary control on regional fluid migration. Thermal waters are classified as Na–Cl and Ca–Mg–HCO₃ types, whereas non-thermal waters are Ca–HCO₃ type, reflecting limited mixing and meteoric recharge dominance. Elevated Na⁺/Cl⁻ ratios suggest that sodium enrichment in groundwater is mainly controlled by silicate weathering reactions, especially feldspar dissolution, reflecting dominant water–rock interaction processes with minimal marine influence. Key scaling phases include calcite, dolomite, gypsum, and anhydrite, with carbonate precipitation in near surface discharge zones driven by CO₂ degassing, induced supersaturation, leading to active scaling and mineral deposition. VLF-EM surveys delineate conductive fracture networks extending to depths, highlighting structurally controlled pathways for geothermal fluid migration. The estimated average reservoir temperature is $$\:\sim$$ 110 ± 5°C, with fluid circulation occurring at depths of approximately 1.37 ± 0.32 km along the North Khurda Fault and the Mahanadi Graben. Deep carbon gas upwelling further enhances fluid recharge along WNW–ESE trending fracture systems at the Atmalik (Deulajhari) thermal spring. Overall, the geothermal system is strongly structurally and fracture controlled, with regional fluid circulation governed primarily by fault networks, and is hydro-geochemically immature to moderately evolved, warranting further reservoir-scale characterization for sustainable exploitation. Harnessing geothermal energy in the region can effectively reduce CO₂ emissions, support India’s net-zero targets by 2070, and promote local economic development and energy resilience.

Environmental Earth SciencesVol. 85(13)
Indian Institute of Technology Kharagpur (IN)
Indian Institute of Technology Kharagpur
Openalex Percentile: Top 9%
Groundwater and Isotope Geochemistry
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.