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Hydrothermal discharge from the El Tatio basin, Atacama, Chile

Journal Article · · Journal of Volcanology and Geothermal Research
 [1];  [2];  [3]
  1. University of Chile, Santiago (Chile)
  2. University of California, Berkeley, CA (United States)
  3. U.S. Geological Survey, Menlo Park, CA (United States)
El Tatio in northern Chile is one of the best-studied geothermal fields in South America. However, there remain open questions about the mass and energy budgets, water recharge rates and residence time in the subsurface, origin of dissolved solutes, and processes affecting the phase and chemical composition of groundwater and surface water. Here we measured and sampled surface manifestations of the geothermal system (geysers, perpetual spouters, mud pools/volcanoes, and non-eruptive hot springs) and meteoric water. From the isotopic composition we infer that the thermal water has a meteoric origin that is different from the composition of local meteoric water. The absence of detectable tritium in thermal waters indicates that most of the recharge occurred pre-1950. Boiling and steam separation from the deep reservoir appear to be the main subsurface processes affecting the thermal fluids. A large amount of heat is lost to the atmosphere by evaporation from surface water and by steam emitted from erupting geysers. Finally, using the chloride inventory method, we estimate thermal water discharge to be 218 to 234 L/s, and the advective heat flow to be 120 to 170 MW.
Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
National Commission for Scientific and Technological Research (CONICYT); National Science Foundation (NSF); USDOE
Grant/Contract Number:
AC02-05CH11231
OSTI ID:
1479426
Journal Information:
Journal of Volcanology and Geothermal Research, Journal Name: Journal of Volcanology and Geothermal Research Vol. 361; ISSN 0377-0273
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

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