Soil gas composition above gas deposits and perspective structures of the Carpathian Foredeep, SE Poland

Abstract

Abstract In 2001 a surface geochemical survey was carried out in the Carpathian Foredeep, in the area between Jaroslaw and Radymno (SE Poland) where multihorizon gas deposits were discovered. These deposits accumulate microbial CH 4 with small amounts of N 2 and higher molecular weight gaseous hydrocarbons. Soil–gas composition in the hydrocarbon fields in the study area is relatively different from the original composition of natural gas occurring in the subsurface reservoir. In 449 analyzed soil gas samples collected from 1.2 m depth relatively low concentrations were found for CH 4 (median value 2.2 ppm) and its homologues (median value of total alkanes C 2 –C 4 – 0.02 ppm). Alkenes were encountered in 36.3% of the analyzed samples (mean value of total alkenes C 2 –C 4 – 0.015 ppm) together with distinctly higher concentrations of H 2 (maximum value – 544 ppm, mean value – 42 ppm) and CO 2 (maximum value – 10.26 vol.%, mean value – 2.27 vol.%). Individual, very high concentrations of CH 4 (up to about 35 vol.%) resulted from sub-surface biochemical reactions whereas higher alkanes detected in soil gases (up to about 68 ppm) originated from deep gas accumulations. Both the H 2 and alkenes may be indirect indicators of deep hydrocarbon accumulations. Carbon dioxide may also be useful for hydrocarbon exploration, revealing increased concentrations in those sampling sites where CH 4 concentrations are strongly depleted, presumably due to bacterial oxidation. These relationships are valid only for the study area and should not be extended as an universal principle. The interpreted zones of cumulative anomalies of CH 4 , higher molecular weight gaseous hydrocarbons, H 2 and CO 2 related to the results of geological and geophysical studies directly or indirectly point to the presence of undiscovered, deep gas accumulations and suggest larger sizes for known deposits. The character of the anomalies along with the relationships between the components of soil gases support the opinion that gas accumulations occur at various depths. Moreover, the results indicate that the surface geochemical pattern is significantly influenced by tectonic discontinuities.