Divergent Thermal Damage Pathways in Coal-Measure Sandstone and Shale: Implications for High-Temperature Energy Subsurface Systems

High-temperature conditions significantly influence the physicochemical and mechanical characteristics of rocks, directly affecting deep geological applications, such as UCG, CCUS, and nuclear waste management. This research investigates the divergent thermomechanical response of sandstone and shale from the Barakar Formation, Jharia Basin, India, exposed from room temperature to 700 °C. A comprehensive multitechnique approach utilizing UCS, BTS, ultrasonic velocity, LPGA, He Pycnometer, and SEM was employed to analyze the interplay of porosity, microstructure, and mechanical integrity with temperature. We propose a three-zone paradigm for thermal degradation using the integrated data set, which mechanistically describes the nonlinear evolution of both rock types. Zone 1 is a conditioning stage characterized by minimal microcracking, mineral stability, and the loss of absorbed water. Due to intergranular tightness, sandstone temporarily gains strength, whereas shale loses strength due to clay mineral dehydration. The key damage-acceleration window, Zone 2, is characterized by organic matter pyrolysis, clay dehydroxylation, the α–β quartz transition, and the rapid formation of interconnected fracture networks. Both rocks experience significant strength loss, while shale disintegrates catastrophically. In Zone 3, high-temperature reorganization occurs due to partial sintering or recrystallization of certain minerals, expansion of fracture networks, and material degradation. Due to bond reprecipitation, sandstone exhibits a slight strength recovery, although shale’s structural integrity is still impaired. The zone-based paradigm offers a mechanistic understanding of the temperature thresholds governing bulk instability and pore–mineral interactions. The thermal design and risk assessment in UCG, geothermal operations, nuclear waste repositories, and fire-damaged rock engineering are directly impacted by these findings.

Authors

Institutions

Publication Details

Journal
Energy & Fuels
Published
2026-03-02
DOI
https://doi.org/10.1021/acs.energyfuels.5c06676
Primary Topic
Geothermal Energy Systems and Applications
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Divergent Thermal Damage Pathways in Coal-Measure Sandstone and Shale: Implications for High-Temperature Energy Subsurface Systems

Madhurima Mazumder, Arijit Sahoo, Ashutosh Tripathy, Shiqi Liu et al.
Energy & Fuels
Geothermal Energy Systems and Applications
article

Divergent Thermal Damage Pathways in Coal-Measure Sandstone and Shale: Implications for High-Temperature Energy Subsurface Systems

Madhurima Mazumder, Arijit Sahoo, Ashutosh Tripathy, Shiqi Liu, T. N. Singh
article en

Abstract

High-temperature conditions significantly influence the physicochemical and mechanical characteristics of rocks, directly affecting deep geological applications, such as UCG, CCUS, and nuclear waste management. This research investigates the divergent thermomechanical response of sandstone and shale from the Barakar Formation, Jharia Basin, India, exposed from room temperature to 700 °C. A comprehensive multitechnique approach utilizing UCS, BTS, ultrasonic velocity, LPGA, He Pycnometer, and SEM was employed to analyze the interplay of porosity, microstructure, and mechanical integrity with temperature. We propose a three-zone paradigm for thermal degradation using the integrated data set, which mechanistically describes the nonlinear evolution of both rock types. Zone 1 is a conditioning stage characterized by minimal microcracking, mineral stability, and the loss of absorbed water. Due to intergranular tightness, sandstone temporarily gains strength, whereas shale loses strength due to clay mineral dehydration. The key damage-acceleration window, Zone 2, is characterized by organic matter pyrolysis, clay dehydroxylation, the α–β quartz transition, and the rapid formation of interconnected fracture networks. Both rocks experience significant strength loss, while shale disintegrates catastrophically. In Zone 3, high-temperature reorganization occurs due to partial sintering or recrystallization of certain minerals, expansion of fracture networks, and material degradation. Due to bond reprecipitation, sandstone exhibits a slight strength recovery, although shale’s structural integrity is still impaired. The zone-based paradigm offers a mechanistic understanding of the temperature thresholds governing bulk instability and pore–mineral interactions. The thermal design and risk assessment in UCG, geothermal operations, nuclear waste repositories, and fire-damaged rock engineering are directly impacted by these findings.

Energy & FuelsVol. 40(10)
Indian Institute of Technology Dhanbad (IN), China University of Mining and Technology (CN)
Openalex Percentile: Top 41%
Geothermal Energy Systems and Applications
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.