Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5770
AuthorsHeinicke, J.* 
Italiano, F.* 
Koch, U.* 
Martinelli, G.* 
Telesca, L.* 
TitleAnomalous fluid emission of a deep borehole in a seismically active area of Northern Apennines (Italy)
Issue Date2009
URIhttp://hdl.handle.net/2122/5770
KeywordsFluids
Earthquakes
Continous monitoring
Subject Classification04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistry 
AbstractThe Miano borehole of 1047 m depth is located close to the river Parma in the Northern Apennines, Italy. A measuring station is installed to observe the discharge of fluids continuously since November 2004. The upwelling fluid of this artesian well is a mixture of thermal water and methane as main components. In non-seismogenic areas, we would expect a relative constant fluid emission perhaps overlaid with long term variations from that kind of deep reservoirs during the time. However, the continuously record of the fluid emission, in particular the water discharge, the gas flow rate and the water temperature, show periods of stable values interrupted by anomalous periods of fluctuations in the recorded parameters. The anomalous variations of these parameters are of low amplitude in comparison to the total values but significant in their long-term trend. Meteorological influences of rain and barometric pressure were not detected in recorded data probably due to reservoir depth and relatively high reservoir overpressure. Influences due to the ambient temperature after the discharge were evaluated by statistical analysis. We consider that recorded changes in fluid emission parameters can be interpreted as a mixing process of different fluid components in depth by variations in pore pressure as result of seismogenic stress variation. Local seismicity was analyzed in comparison to fluid’s physico-chemical data. The analysis supports the idea of an influence to fluid transport conditions due to geodynamic processes exist. Water temperature data show frequent anomalies probably connected with possible precursory phenomena of local seismic events.
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