NissirosV1, Main, Exploration, bibRecord, 000218

Time-variation of hydrothermal discharge at selected sites in the western United States: implications for monitoring

Identifieur interne : 000218 ( Main/Exploration ); précédent : 000217; suivant : 000219

Time-variation of hydrothermal discharge at selected sites in the western United States: implications for monitoring

Auteurs : S. E. Ingebritsen [États-Unis] ; D. L. Galloway [États-Unis] ; E. M. Colvard [États-Unis] ; M. L. Sorey [États-Unis] ; R. H. Mariner [États-Unis]

Source :

Journal of Volcanology and Geothermal Research [ 0377-0273 ] ; 2001.

RBID : ISTEX:0DFB9AAC0DFAD8EC74EC9C316079B68C8359C822

Descripteurs français

Wicri :
- topic : Parc national, Volcanologie.

English descriptors

Abstract

Abstract: We compiled time series of hydrothermal discharge consisting of 3593 chloride- or heat-flux measurements from 24 sites in the Yellowstone region, the northern Oregon Cascades, Lassen Volcanic National Park and vicinity, and Long Valley, California. At all of these sites the hydrothermal phenomena are believed to be as yet unaffected by human activity, though much of the data collection was driven by mandates to collect environmental-baseline data in anticipation of geothermal development. The time series average 19years in length and some of the Yellowstone sites have been monitored intermittently for over 30 years. Many sites show strong seasonality but few show clear long-term trends, and at most sites statistically significant decadal-scale trends are absent. Thus, the data provide robust estimates of advective heat flow ranging from ∼130MW in the north-central Oregon Cascades to ∼6100MW in the Yellowstone region, and also document Yellowstone hydrothermal chloride and arsenic fluxes of 1740 and 15–20g/s, respectively. The discharge time series show little sensitivity to regional tectonic events such as earthquakes or inflation/deflation cycles. Most long-term monitoring to date has focused on high-chloride springs and low-temperature fumaroles. The relative stability of these features suggests that discharge measurements done as part of volcano-monitoring programs should focus instead on high-temperature fumaroles, which may be more immediately linked to the magmatic heat source.

Url:

https://api.istex.fr/document/0DFB9AAC0DFAD8EC74EC9C316079B68C8359C822/fulltext/pdf

DOI: 10.1016/S0377-0273(01)00207-4

Affiliations:

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Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Advected</term>
<term>Advective</term>
<term>Advective heat</term>
<term>Advective heat transport</term>
<term>Arsenic</term>
<term>Borah</term>
<term>Borah peak event</term>
<term>Brantley</term>
<term>Breitenbush</term>
<term>Breitenbush river</term>
<term>Caldera</term>
<term>Cascade</term>
<term>Cascade range</term>
<term>Chloride</term>
<term>Chloride concentration</term>
<term>Clackamas river</term>
<term>Colvard</term>
<term>Continuous monitoring</term>
<term>Corwin springs</term>
<term>Costa rica</term>
<term>Crater</term>
<term>Crater lakes</term>
<term>Creek gorge</term>
<term>Dawson</term>
<term>Devils kitchen</term>
<term>Direct discharge</term>
<term>Discharge</term>
<term>Discharge measurements</term>
<term>Entire data</term>
<term>Farrar</term>
<term>Firehole</term>
<term>Firehole river</term>
<term>Fournier</term>
<term>Friedman</term>
<term>Fumarole</term>
<term>Fumaroles</term>
<term>Fumarolic</term>
<term>Fumarolic areas</term>
<term>Gardner river</term>
<term>Geochemical</term>
<term>Geochemical monitoring</term>
<term>Geological survey</term>
<term>Geological survey bulletin</term>
<term>Geological survey investigations report</term>
<term>Geological survey report</term>
<term>Geophysical</term>
<term>Geophysical research</term>
<term>Geothermal</term>
<term>Geothermal development</term>
<term>Geothermal fumaroles</term>
<term>Geothermal research</term>
<term>Geothermal resources</term>
<term>Geothermal resources area</term>
<term>Glover</term>
<term>Heat advected</term>
<term>Heat discharge</term>
<term>Heat loss</term>
<term>Horse creek</term>
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<term>Hydrothermal discharge</term>
<term>Hydrothermal systems</term>
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<term>Long valley</term>
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<term>Mono county</term>
<term>National park</term>
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<term>Thermal waters</term>
<term>Time series</term>
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<term>Total heat</term>
<term>Total heat loss</term>
<term>Transient storage</term>
<term>Usgs</term>
<term>Uxes</term>
<term>Volcan colima</term>
<term>Volcanic</term>
<term>Volcanic activity</term>
<term>Volcanic fumaroles</term>
<term>Volcanic unrest</term>
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<term>Volcanology</term>
<term>Wairakei</term>
<term>Waring</term>
<term>Yellowstone</term>
<term>Yellowstone region</term>
<term>Zealand</term>
<term>Zealand journal</term>
<term>fumaroles</term>
<term>hot springs</term>
<term>monitoring</term>
<term>time series</term>
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<keywords scheme="Teeft" xml:lang="en"><term>Advected</term>
<term>Advective</term>
<term>Advective heat</term>
<term>Advective heat transport</term>
<term>Arsenic</term>
<term>Borah</term>
<term>Borah peak event</term>
<term>Brantley</term>
<term>Breitenbush</term>
<term>Breitenbush river</term>
<term>Caldera</term>
<term>Cascade</term>
<term>Cascade range</term>
<term>Chloride</term>
<term>Chloride concentration</term>
<term>Clackamas river</term>
<term>Colvard</term>
<term>Continuous monitoring</term>
<term>Corwin springs</term>
<term>Costa rica</term>
<term>Crater</term>
<term>Crater lakes</term>
<term>Creek gorge</term>
<term>Dawson</term>
<term>Devils kitchen</term>
<term>Direct discharge</term>
<term>Discharge</term>
<term>Discharge measurements</term>
<term>Entire data</term>
<term>Farrar</term>
<term>Firehole</term>
<term>Firehole river</term>
<term>Fournier</term>
<term>Friedman</term>
<term>Fumarole</term>
<term>Fumaroles</term>
<term>Fumarolic</term>
<term>Fumarolic areas</term>
<term>Gardner river</term>
<term>Geochemical</term>
<term>Geochemical monitoring</term>
<term>Geological survey</term>
<term>Geological survey bulletin</term>
<term>Geological survey investigations report</term>
<term>Geological survey report</term>
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<term>Geophysical research</term>
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<term>Geothermal development</term>
<term>Geothermal fumaroles</term>
<term>Geothermal research</term>
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<term>Geothermal resources area</term>
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<term>Heat advected</term>
<term>Heat discharge</term>
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<term>Lassen</term>
<term>Long valley</term>
<term>Long valley caldera</term>
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<term>Major earthquakes</term>
<term>Major streams</term>
<term>Mammoth mountain</term>
<term>Mono county</term>
<term>National park</term>
<term>Poa</term>
<term>Poas volcano</term>
<term>Regional tectonic events</term>
<term>Rojstaczer</term>
<term>Seasonality</term>
<term>Solute</term>
<term>Sorey</term>
<term>Spring systems</term>
<term>Springs creek</term>
<term>Standard deviation</term>
<term>Stream discharge</term>
<term>Thermal areas</term>
<term>Thermal features</term>
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<front><div type="abstract" xml:lang="en">Abstract: We compiled time series of hydrothermal discharge consisting of 3593 chloride- or heat-flux measurements from 24 sites in the Yellowstone region, the northern Oregon Cascades, Lassen Volcanic National Park and vicinity, and Long Valley, California. At all of these sites the hydrothermal phenomena are believed to be as yet unaffected by human activity, though much of the data collection was driven by mandates to collect environmental-baseline data in anticipation of geothermal development. The time series average 19years in length and some of the Yellowstone sites have been monitored intermittently for over 30 years. Many sites show strong seasonality but few show clear long-term trends, and at most sites statistically significant decadal-scale trends are absent. Thus, the data provide robust estimates of advective heat flow ranging from ∼130MW in the north-central Oregon Cascades to ∼6100MW in the Yellowstone region, and also document Yellowstone hydrothermal chloride and arsenic fluxes of 1740 and 15–20g/s, respectively. The discharge time series show little sensitivity to regional tectonic events such as earthquakes or inflation/deflation cycles. Most long-term monitoring to date has focused on high-chloride springs and low-temperature fumaroles. The relative stability of these features suggests that discharge measurements done as part of volcano-monitoring programs should focus instead on high-temperature fumaroles, which may be more immediately linked to the magmatic heat source.</div>
</front>
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<name sortKey="Colvard, E M" sort="Colvard, E M" uniqKey="Colvard E" first="E. M." last="Colvard">E. M. Colvard</name>
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<name sortKey="Mariner, R H" sort="Mariner, R H" uniqKey="Mariner R" first="R. H." last="Mariner">R. H. Mariner</name>
<name sortKey="Sorey, M L" sort="Sorey, M L" uniqKey="Sorey M" first="M. L." last="Sorey">M. L. Sorey</name>
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Time-variation of hydrothermal discharge at selected sites in the western United States: implications for monitoring

Time-variation of hydrothermal discharge at selected sites in the western United States: implications for monitoring

Source :

Descripteurs français

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri