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Chemical Changes in Geothermal Well M-20, Cerro Prieto, Mexico

1969; Geological Society of America; Volume: 80; Issue: 12 Linguagem: Inglês

10.1130/0016-7606(1969)80[2623

1943-2674

S. Mercado,

Geological and Geochemical Analysis

Research Article| December 01, 1969 Chemical Changes in Geothermal Well M-20, Cerro Prieto, Mexico S MERCADO S MERCADO Comisión Federal de Electricidad, Comisión de Energía Geotérmica, Proyecto Cerro Prieto, Justo Sierra 2098, Mexicali, B.Cfa., Mexico Search for other works by this author on: GSW Google Scholar Author and Article Information S MERCADO Comisión Federal de Electricidad, Comisión de Energía Geotérmica, Proyecto Cerro Prieto, Justo Sierra 2098, Mexicali, B.Cfa., Mexico Publisher: Geological Society of America Received: 10 Mar 1969 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1969, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1969) 80 (12): 2623–2630. https://doi.org/10.1130/0016-7606(1969)80[2623:CCIGWM]2.0.CO;2 Article history Received: 10 Mar 1969 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation S MERCADO; Chemical Changes in Geothermal Well M-20, Cerro Prieto, Mexico. GSA Bulletin 1969;; 80 (12): 2623–2630. doi: https://doi.org/10.1130/0016-7606(1969)80[2623:CCIGWM]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Following the initial discharge of well M-20, large variations took place in the pressure and enthalpy of the steam mixture. Results of chemical calculations showed possible causes of this variation, and indicated important limits on the capacity of the hydrothermal reservoir. The principal basis for the calculations were the ratio Na/K and the silica content of the flow. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.