Geodynamic processes in the NW Bohemian swarm earthquake region, Czech Republic, identified by continuous gas monitoring
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F13%3A00435243" target="_blank" >RIV/67985891:_____/13:00435243 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1111/gfl.12027" target="_blank" >http://dx.doi.org/10.1111/gfl.12027</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/gfl.12027" target="_blank" >10.1111/gfl.12027</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Geodynamic processes in the NW Bohemian swarm earthquake region, Czech Republic, identified by continuous gas monitoring
Popis výsledku v původním jazyce
The time series of two continuously operating gas monitoring stations at Oldrisska and Novy Kostel located along seismoactive faults in the epicentral area of the NW Bohemian swarm earthquakes (Czech Republic) are compared with water level fluctuations in two boreholes positioned along these faults and with gas flux variations of a mofette at the Soos mofette field at 9 km distance. The seasonal trend of the monitored CO2 concentration with a maximum in November and a minimum in March/April is governedby groundwater temperatures, superimposed in spring by soil temperatures. CO2 concentration variations identified at Oldrisska are also reflected in gas flux variations in the Soos mofette and/or water level fluctuations of two boreholes. Variations in the gas monitoring recordings of station at Novy Kostel are also linked with variations at Oldrisska. In all data sets, diurnal variations generated by earth tides occur, reflecting a daily stress - fault permeability cycle. Additional str
Název v anglickém jazyce
Geodynamic processes in the NW Bohemian swarm earthquake region, Czech Republic, identified by continuous gas monitoring
Popis výsledku anglicky
The time series of two continuously operating gas monitoring stations at Oldrisska and Novy Kostel located along seismoactive faults in the epicentral area of the NW Bohemian swarm earthquakes (Czech Republic) are compared with water level fluctuations in two boreholes positioned along these faults and with gas flux variations of a mofette at the Soos mofette field at 9 km distance. The seasonal trend of the monitored CO2 concentration with a maximum in November and a minimum in March/April is governedby groundwater temperatures, superimposed in spring by soil temperatures. CO2 concentration variations identified at Oldrisska are also reflected in gas flux variations in the Soos mofette and/or water level fluctuations of two boreholes. Variations in the gas monitoring recordings of station at Novy Kostel are also linked with variations at Oldrisska. In all data sets, diurnal variations generated by earth tides occur, reflecting a daily stress - fault permeability cycle. Additional str
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DD - Geochemie
OECD FORD obor
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Návaznosti výsledku
Projekt
—
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geofluids
ISSN
1468-8115
e-ISSN
—
Svazek periodika
13
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
26
Strana od-do
305-330
Kód UT WoS článku
000322160100004
EID výsledku v databázi Scopus
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