Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Rock-water interactions in the Fenton Hill, New Mexico, hot dry rock geothermal systems 1; Fluid mixing and chemical geothermometry

Journal Article · · Geothermics (International Journal of Geothermal Research and its Applications); (UK)
;  [1]; ;  [2]
  1. Dept. of Chemical Engineering, Massachusetts Inst. of Technology, Cambridge, MA (US)
  2. Earth and Space Sciences Div., Los Alamos National Lab., Los Alamos, NM (US)
The chemistry of fluids circulated through an artificially-stimulated, hot dry rock (HDR) fractured geothermal reservoir system in granitic rock is described in terms of mixing phenomena, geothermometry, and approach to saturation with reservoir rock minerals. Based on the similar dynamic behavior of Na{sup +}, K{sup +}, Li{sup +}, Cl{sup {minus}}, and B species and other isotopic evidence, the presence of a concentrated {ital in-situ} pore fluid was identified. Mixing and displacement of this {ital in situ} fluid with meteoric make-up water is responsible for the observed behavior of the major dissolved species in the circulated fluid of this HDR system.
OSTI ID:
5877209
Journal Information:
Geothermics (International Journal of Geothermal Research and its Applications); (UK), Journal Name: Geothermics (International Journal of Geothermal Research and its Applications); (UK) Vol. 18:5/6; ISSN GTMCA; ISSN 0375-6505
Country of Publication:
United States
Language:
English