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Geysers Valley CO2 Cycling Geological Engine (Kamchatka, Russia)

Journal Article · · Geofluids
DOI:https://doi.org/10.1155/2018/1963618· OSTI ID:1476608
 [1];  [2];  [3]
  1. Inst. of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky (Russia); Kronotsky Federal Nature Biosphere Reserve, Yelizovo (Russia)
  2. Inst. of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky (Russia)
  3. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)

1941–2017 period of the Valley of Geysers monitoring (Kamchatka, Kronotsky Reserve) reveals a very dynamic geyser behavior under natural state conditions: significant changes of IBE (interval between eruptions) and power of eruptions, chloride and other chemical components, and preeruption bottom temperature. Nevertheless, the total deep thermal water discharge remains relatively stable; thus all of the changes are caused by redistribution of the thermal discharge due to giant landslide of June 3, 2007, mudflow of Jan. 3, 2014, and other events of geothermal caprock erosion and water injection into the geothermal reservoir. In some cases, water chemistry and isotope data point to local meteoric water influx into the geothermal reservoir and geysers conduits. TOUGHREACT V.3 modeling of Velikan geyser chemical history confirms 20% dilution of deep recharge water and CO2components after 2014. Temperature logging in geysers Velikan (1994, 2007, 2015, 2016, and 2017) and Bolshoy (2015, 2016, and 2017) conduits shows preeruption temperatures below boiling at corresponding hydrostatic pressure, which means partial pressure of CO2 creates gas-lift upflow conditions in geyser conduits. Velikan geyser IBE history explained in terms of gradual CO2 recharge decline (1941–2013), followed by CO2 recharge significant dilution after the mudflow of Jan. 3, 2014, also reshaped geyser conduit and diminished its power.

Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
Grant/Contract Number:
AC02-05CH11231
OSTI ID:
1476608
Journal Information:
Geofluids, Journal Name: Geofluids Vol. 2018; ISSN 1468-8115
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English

References (9)

Geothermal solute equilibria. Derivation of Na-K-Mg-Ca geoindicators journal December 1988
Formation of the hydrothermal system in Geysers Valley (Kronotsky Nature Reserve, Kamchatka) and triggers of the Giant Landslide journal September 2012
TOUGHREACT Version 2.0: A simulator for subsurface reactive transport under non-isothermal multiphase flow conditions journal June 2011
Modeling and observations of geyser activity in relation to catastrophic landslides–mudflows (Kronotsky nature reserve, Kamchatka, Russia) journal September 2016
Inflation model of Uzon caldera, Kamchatka, constrained by satellite radar interferometry observations journal January 2006
Video observations inside conduits of erupting geysers in Kamchatka, Russia, and their geological framework: Implications for the geyser mechanism journal April 2013
An analysis of hydrogeological behavior in the Geyser Valley, Kronotskii nature reserve, Kamchatka after the disaster of June 3, 2007 journal January 2015
The Fascinating and Complex Dynamics of Geyser Eruptions journal August 2017
Geofluid Systems of Koryaksky-Avachinsky Volcanoes (Kamchatka, Russia) journal January 2017

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