Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4391
AuthorsBaciu, C.* 
Etiope, G.* 
Cuna, S.* 
Spulber, L.* 
TitleMethane seepage in an urban development area (Bacau, Romania): origin, extent, and hazard
Issue DateNov-2008
Series/Report no.4 / 8 (2008)
DOI10.1111/j.1468-8123.2008.00228.x
URIhttp://hdl.handle.net/2122/4391
Keywordsgas hazard
methane seepage
soil degassing
thermogenic gas
Subject Classification03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gases 
AbstractThe paper describes a case of a natural emission of methane from soil in an urban development area, generating a significant risk for the local population and buildings, due to gas explosiveness and asphyxiation potential. The site is located on the south-western margin of the East-European Platform in eastern Romania, in a hydrocarbon-prone area crossed by the Pericarpathian lineament and regional faults. Molecular composition of gas and stable isotopic analyses of methane (CH4>90%, δ to the power of 13 C1: -49.4‰, δD1: -173.4‰) indicate a dominant thermogenic origin, with significant amounts of C2-C5 alkanes (~5%), likely migrating through faults from a deep reservoir. Possible candidates are the Saucesti and Secuieni gas fields, located in the same petroleum system. Two surface geochemical surveys, based on closed-chamber flux measurements, were performed to assess the degassing intensity and the extent of the affected area. Methane fluxes from soil reach orders of 10 to the power of 4 mg m to the power of -2 day to the power of -1. Gas seepage mainly occurs in one zone 30 000 m2 wide, and it is likely controlled by channeling along a fault and gas accumulation in permeable sediments and shallow subsoil. The estimated total CH4 emission is about 40 t year to the power of -1 CH4, of which 8–9 t year to the power of -1 are naturally released from soil and 30–35 t year to the power of -1 are emitted from shallow boreholes. These wells have likely channeled the gas accumulated in shallow alluvial sediment but gas flux from soil is still high and mitigation measures are needed to reduce the risk for humans and buildings.
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