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Title: Seismic velocity and attenuation structure of the Geysers geothermal field, California

Journal Article · · Geothermics (International Journal of Geothermal Research and its Applications); (United Kingdom)
; ;  [1]
  1. Lawrence Livermore National Lab., CA (United States)

The Geysers geothermal field is located in northern California and is one of the world's largest producers of electricity from geothermal energy. A key resource management issue at this field is the distribution of fluid in the matrix of the reservoir rock. In this paper, the authors interpret seismic compressional-wave velocity and quality quotient (Q) data at The Geysers in terms of the geologic structure and fluid saturation in the reservoir. Their data consist of waveforms from approximately 300 earthquakes. Using compressional-wave arrival times, they invert for earthquake location, origin time, and velocity within a three-dimensional grid. Using the pulse width of the compressional wave, they invert for the pulse width contribution associated with the source and the one-dimensional Q structure. They find that the velocity structure correlates with known mapped geologic units. The dry steam reservoir, which is known from steam well drilling, is mostly correlated with low velocity. The correlation is best for those areas where the steam pressure has been reduced by production. The Q increases with depth to the top of the dry steam reservoir and decreases with depth within the reservoir. This decrease of Q with depth suggests that the liquid saturation of the reservoir rock matrix increases with depth.

OSTI ID:
6841976
Journal Information:
Geothermics (International Journal of Geothermal Research and its Applications); (United Kingdom), Vol. 23:2; ISSN 0375-6505
Country of Publication:
United States
Language:
English