Summary of annual repeat magnetotelluric surveys of the Geysers geothermal field

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Abstract

As part of a multi-year project, funded by the California Energy Commission, annual magnetotelluric (MT) surveys have been collected at The Geysers geothermal field in northern California with the goal of measuring temporal changes within the steam field. The repeat surveys started in 2021 and repeated a 2017 survey (Peacock et al., 2020) with further extension to the southern part of the geothermal field. Temporal variations in the MT transfer functions are observed to be spatially coherent and compartmentalized. Mapping residual phase tensor ellipses demonstrates the direction of maximum change is often aligned with existing fracture orientations. Three dimensional inversion of the MT data, using the inversion results from previous years as the starting model, indicates that the steam reservoir has generally become more resistive over time (~10%), suggesting more steam in the field. A few pockets within the steam field have become more electrically conductive over time and are collocated with injection wells, suggesting either more fluid content in those zones, less steam, or more saline fluids.  

Suggested Citation

Peacock, J.R., Alumbaugh, D., Mitchell, M.A., and Hartline, C., 2024, Summary of annual repeat magnetotelluric surveys of the Geysers geothermal field, 49th Workshop on Geothermal Reservoir Engineering, Stanford, CA, February 12-14, 2024, 6 p.

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Publication type Conference Paper
Publication Subtype Conference Paper
Title Summary of annual repeat magnetotelluric surveys of the Geysers geothermal field
Year Published 2024
Language English
Publisher Stanford University
Contributing office(s) Geology, Minerals, Energy, and Geophysics Science Center
Description 6 p.
Conference Title 49th Workshop on Geothermal Reservoir Engineering
Conference Location Stanford, CA
Conference Date February 12-14, 2024
Country United States
State California
Other Geospatial Geysers geothermal field
Additional publication details