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• W2277492079 abstract "Research Article| March 01, 2016 Dissolved gases in hydrothermal (phreatic) and geyser eruptions at Yellowstone National Park, USA Shaul Hurwitz; Shaul Hurwitz 1U.S. Geological Survey, Menlo Park, California 94025, USA Search for other works by this author on: GSW Google Scholar Laura E. Clor; Laura E. Clor 1U.S. Geological Survey, Menlo Park, California 94025, USA Search for other works by this author on: GSW Google Scholar R. Blaine McCleskey; R. Blaine McCleskey 2U.S. Geological Survey, Boulder, Colorado 80303, USA Search for other works by this author on: GSW Google Scholar D. Kirk Nordstrom; D. Kirk Nordstrom 2U.S. Geological Survey, Boulder, Colorado 80303, USA Search for other works by this author on: GSW Google Scholar Andrew G. Hunt; Andrew G. Hunt 3U.S. Geological Survey, Denver, Colorado 80225, USA Search for other works by this author on: GSW Google Scholar William C. Evans William C. Evans 1U.S. Geological Survey, Menlo Park, California 94025, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Shaul Hurwitz 1U.S. Geological Survey, Menlo Park, California 94025, USA Laura E. Clor 1U.S. Geological Survey, Menlo Park, California 94025, USA R. Blaine McCleskey 2U.S. Geological Survey, Boulder, Colorado 80303, USA D. Kirk Nordstrom 2U.S. Geological Survey, Boulder, Colorado 80303, USA Andrew G. Hunt 3U.S. Geological Survey, Denver, Colorado 80225, USA William C. Evans 1U.S. Geological Survey, Menlo Park, California 94025, USA Publisher: Geological Society of America Received: 30 Oct 2015 Revision Received: 25 Jan 2016 Accepted: 29 Jan 2016 First Online: 09 Mar 2017 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2016 Geological Society of America Geology (2016) 44 (3): 235–238. https://doi.org/10.1130/G37478.1 Article history Received: 30 Oct 2015 Revision Received: 25 Jan 2016 Accepted: 29 Jan 2016 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Shaul Hurwitz, Laura E. Clor, R. Blaine McCleskey, D. Kirk Nordstrom, Andrew G. Hunt, William C. Evans; Dissolved gases in hydrothermal (phreatic) and geyser eruptions at Yellowstone National Park, USA. Geology 2016;; 44 (3): 235–238. doi: https://doi.org/10.1130/G37478.1 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 SocietyGeology Search Advanced Search Abstract Multiphase and multicomponent fluid flow in the shallow continental crust plays a significant role in a variety of processes over a broad range of temperatures and pressures. The presence of dissolved gases in aqueous fluids reduces the liquid stability field toward lower temperatures and enhances the explosivity potential with respect to pure water. Therefore, in areas where magma is actively degassing into a hydrothermal system, gas-rich aqueous fluids can exert a major control on geothermal energy production, can be propellants in hazardous hydrothermal (phreatic) eruptions, and can modulate the dynamics of geyser eruptions. We collected pressurized samples of thermal water that preserved dissolved gases in conjunction with precise temperature measurements with depth in research well Y-7 (maximum depth of 70.1 m; casing to 31 m) and five thermal pools (maximum depth of 11.3 m) in the Upper Geyser Basin of Yellowstone National Park, USA. Based on the dissolved gas concentrations, we demonstrate that CO2 mainly derived from magma and N2 from air-saturated meteoric water reduce the near-surface saturation temperature, consistent with some previous observations in geyser conduits. Thermodynamic calculations suggest that the dissolved CO2 and N2 modulate the dynamics of geyser eruptions and are likely triggers of hydrothermal eruptions when recharged into shallow reservoirs at high concentrations. Therefore, monitoring changes in gas emission rate and composition in areas with neutral and alkaline chlorine thermal features could provide important information on the natural resources (geysers) and hazards (eruptions) in these areas. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2277492079 date "2016-02-05" @default.
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• W2277492079 title "Dissolved gases in hydrothermal (phreatic) and geyser eruptions at Yellowstone National Park, USA" @default.
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