Return
Heat transfer characteristics of an oceanic crust thermal reservoir under seawater cyclic thermal shock: optimization for geothermal energy extraction
M
J
C
H
DOI:10.1016/j.renene.2026.126266.png)
Abstract
En 中文
• Thermal properties of HDR drop sharply after seawater thermal shock. • A 300 °C threshold shifts heat transfer to a fracture-controlled regime. • Dense fracture networks form local thermal barriers, causing rapid temp changes. • Thermo-chemical-mechanical coupling accelerates rock degradation and cracking.
Journal
IF:
9.1
Papers:
2.6W
Citations:
12.1W
