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Analysis of Multiscale Porosity at the Coso Geothermal Field

Published

Author(s)

Lawrence M Anovitz, David R. Cole, David D. Faulder, Julie Sheets, Gernot Rother, Matthew John Wasbrough, Rex P. Hjelm, Monika Hartl, Vitaliy Pipich, Zhensdong Fu

Abstract

The multiscale pore structure of the rocks making up a geothermal reservoir and the mineralogy associated with those pores are critical factors for estimating a number of reservoir properties including fluid mass in place, permeability, and capillary pressures as well as geochemical and thermal interactions between the rock and fluid. This paper describes the results of a combined neutron scattering and imagine analysis of samples from a well on the east flank of the Coso reservoir in California and delineates the close relationship between alteration mineralogy and multiscale porosity.
Proceedings Title
Thirty-Eighth Workshop on Geothermal Reservoir Engineering
Volume
SGP-TR-198
Conference Dates
February 11-13, 2013
Conference Location
Stanford, CA, US
Conference Title
Stanford Geothermal Workshop

Citation

Anovitz, L. , Cole, D. , Faulder, D. , Sheets, J. , Rother, G. , Wasbrough, M. , Hjelm, R. , Hartl, M. , Pipich, V. and Fu, Z. (2013), Analysis of Multiscale Porosity at the Coso Geothermal Field, Thirty-Eighth Workshop on Geothermal Reservoir Engineering, Stanford, CA, US, [online], https://tsapps.nist.gov/publication/get_pdf.cfm?pub_id=913354 (Accessed December 15, 2024)

Issues

If you have any questions about this publication or are having problems accessing it, please contact reflib@nist.gov.

Created February 12, 2013, Updated October 12, 2021