V031
The Superhot Hydrothermal to Magma Transition: A Scientific Frontier and a Prime Target for Geothermal Energy
The Superhot Hydrothermal to Magma Transition: A Scientific Frontier and a Prime Target for Geothermal Energy
Session ID#: 251772
Session Description:
The fields of volcanology and geothermal engineering now overlap. This session will highlight what we are learning. Drilling has intersected silicic magma at Puna, Hawaii; Krafla, Iceland; and Menengai, Kenya. Boreholes have reached >500oC at multiple sites, first at Kakkonda, Japan. Pinatubo, Philippines was drilled to >300oC at 2-3 km depth, likely into a hydrothermal plume rising from dacitic magma petrologically estimated to be at 5 km depth, of which 5 km3 was subsequently erupted. Drilling at Augustine Volcano, AK may cross the 400oC isotherm at only 1-2 km and reach magma at 2 to 4 km, estimated geophysically and petrologically, respectively. The superhot regime may be dominantly conductive. If so, it will be thin and close to magma, holding the key to making geothermal competitive with non-green energy sources. We welcome papers based on field and drilling observations, experiments, and modeling of the transition from hydrothermal to magmatic reservoirs.
Co-Sponsor(s):
- G - Geodesy
- MR - Mineral and Rock Physics
- NH - Natural Hazards
- P - Planetary Sciences
Index Terms:
8411 Thermodynamics [VOLCANOLOGY]
8412 Reactions and phase equilibria [VOLCANOLOGY]
8424 Hydrothermal systems [VOLCANOLOGY]
8439 Physics and chemistry of magma bodies [VOLCANOLOGY]
Primary Convener: John C Eichelberger, Alaska Department of Natural Resources, Division of Geological and Geophysical Surveys, Fairbanks, United States and Paul Choate
Conveners: Paolo Papale, Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy, Paul Choate, Choate Technology Services, Cambridge, United Kingdom, Charles Carrigan, Stratify/MH Chew LLC, Washington, United States and Paul Choate
See more of: Volcanology, Geochemistry and Petrology