Temperature-induced microstructural evolution and fractal characteristics of high-enthalpy Chumathang granite for enhanced geothermal energy

Journal Article (2025)
Author(s)

Mrityunjay Singh (GFZ Helmholtz-Zentrum für Geoforschung)

Sachchida nand Pandey (Indian Institute of Technology Bombay)

Debanjan Chandra (TU Delft - Civil Engineering & Geosciences)

Nishant Singh (Indian Institute of Technology Bombay)

Adarsh Tripathi (Indian Institute of Technology Roorkee)

Sunil Kumar Yadav (Indian Institute of Technology Roorkee)

Ingo Sass (GFZ Helmholtz-Zentrum für Geoforschung, Technische Universität Darmstadt)

Ajeet Kumar Srivastav (Visvesvaraya National Institute of Technology, Nagpur)

Sandip Kumar Saha (Indian Institute of Technology Bombay)

Research Group
Applied Geophysics and Petrophysics
DOI related publication
https://doi.org/10.1038/s41598-025-00683-2 Final published version
More Info
expand_more
Publication Year
2025
Language
English
Research Group
Applied Geophysics and Petrophysics
Journal title
Scientific Reports
Issue number
1
Volume number
15
Article number
18549
Downloads counter
202
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

Micro-structural attributes of Chumathang granite from Leh, India, were experimentally determined in the temperature range from 25 to 600 °C for enhanced geothermal systems (EGS). P-wave velocity, thermal crack generation, and pore attributes were analyzed using a combination of pulse ultrasonic velocity study, 3D X-ray tomography and low-pressure gas adsorption experiments, respectively. Results indicate that thermal crack development is driven by mineral composition and differential thermal expansion, with a significant increase in the thermal damage factor between 450 ∘C and 600 ∘C, accompanied by visible cracks at 600 ∘C. Surface area and pore volume decreased up to 300 ∘C due to mineral dissolution, then slightly increased up to 600 ∘C due to microfracture formation. Pore size distribution showed a dominance of coarser mesopores, and fractal dimensions decreased with temperature, reflecting simpler pore geometries. These findings enhance the understanding of granite’s microstructural changes under thermal stress, informing the optimization of EGS heat extraction efficiency.

Files

S41598-025-00683-2-1.pdf
(pdf | 3.29 Mb)
License info not available