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Tytuł artykułu

Molecular and isotopic compositions of gases adsorbed to near surface sediments at Starunia palaeontological site and vicinity (Carpathian region, Ukraine)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The near-surface geochemical survey of gases desorbed from sediment samples was carried out in the area of an abandoned ozokerite mine in Starunia, where remnants of mammoth and three woolly rhinoceroses and one almost completely preserved rhinoceros carcass were discovered in 1907 and 1929. Numerous hydrocarbon seeps (gas and oil "eyes") occur on the surface of the study area. Analyses of molecular and stable carbon isotope compositions of adsorbed gases were carried out in two variants. The first included sampling of cuttings from 30 auger boreholes at depths of 4.8, 5.6 and 6.4 m. In total, 88 samples were collected. In the second variant core samples were collected from 17 selected boreholes. In total, 78 samples were taken from various depths to 12 m. The results of molecular composition analyses of desorbed gases indicated high saturation of near-surface sediments with the oil. The highest concentrations of alkanes were detected in Miocene strata. Hydrocarbon migration from deep accumulations to the surface was relatively fast and proceeded along the faults, fractures and cracks. In the near-surface zone hydrocarbons were subjected to oxidation and dehydrogenation, which resulted in generation of unsaturated hydrocarbons and hydrogen. These processes were most intensive in the Pleistocene sediments and in the mine dumps. Increased concentrations of hydrogen may also originate from water radiolysis in the presence of hydrocarbons. Concentrations of carbon dioxide in the adsorbed gases show the higher values in comparison with the analysed gaseous compounds. However, a slight increase in CO2 concentration was detected in the mine dump, which may indicate conditions more favourable for hydrocarbon oxidation. Carbon dioxide from the analysed adsorbed gases is of thermogenic origin. Occasionally, insignificant influence of secondary hydrocarbon oxidation and/or Quaternary organic matter can be observed. Concentrations of alkanes, alkenes and carbon dioxide in the gas derived from desorption of rock samples are lower and the concentration of hydrogen is higher than those measured in free gases. This indicates that additional effects from recent (e.g. microbial) processes are absent.
Rocznik
Strony
421--437
Opis fizyczny
bibliogr. 28 poz., rys., tab., wykr.
Twórcy
autor
  • Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Kraków, Poland, dzieniew@agh.edu.pl
Bibliografia
  • Alexandrowicz, S. W., 2004. Starunia and the Quaternary research in the tradition and initiatives of the Polish Academy of Arts and Sciences. (In Polish, English summary). Studia i materiały do dziejów Polskiej Akademii Umiejętności. Polska Akademia Umiejętności, Kraków, 3, 261 pp.
  • Alexandrowicz, S. W., 2005. The history of Starunia - a palaeontologic site and old ozokerite mine. In: Kotarba, M. J. (ed.), Polish and Ukrainian studies (2004-2005) at Starunia - the area of discoveries of woolly rhinoceroses. Polish Geological Institute and Society of Research on Environmental Changes "Geosphere", Warszawa-Kraków: 21-38.
  • Hawkes, H. E., 1972. Free hydrogen in genesis of petroleum. American Association of Petroleum Geologists Bulletin, 56: 2268-2277.
  • Karèev, A. A., Tabasaranskiy, Z. M., Subbota, M. I. & Mogilevskiy, G. A., 1954. Geokhimi-cheskiye metody poiskov i razvedki nieftianykh i gazovykh miestorozhdieniy. (In Russian). Gostoptekhizdat, Moskva, 430 pp.
  • Koltun, Y. V., Adamenko, O. M., Kotarba, M. J., Dudok, I. V., Pavluk, M. I., Burzewski, W. & Stelmakh, O. R., 2005. Geological setting and petroleum occurrence of the Starunia area, fore-Carpathian region, Ukraine. In: Kotarba, M. J. (ed.), Polish and Ukrainian studies (2004-2005) at Starunia - the area of discoveries of woolly rhinoceroses. Polish Geological Institute and Society of Research on Environmental Changes "Geosphere", Warszawa-Kraków: 61-78.
  • Kotarba, M. J., Sechman, H. & Dzieniewicz, M., 2009. Distribution and origin of gaseous hydrocarbons and carbon dioxide in the Quaternary sediments at Starunia palaeontological site and vicinity (Carpathian region, Ukraine). Annales Societatis Geologorum Poloniae, 79: 403-419.
  • Kubiak, H. & Drygant, D. M., 2005. The Starunia collections in Lviv and Kraków natural history museums and history of palaeontological studies. In: Kotarba, M. J. (ed.), Polish and Ukrainian studies (2004-2005) at Starunia - the area of discoveries of woolly rhinoceroses. Polish Geological Institute and Society of Research on Environmental Changes "Geosphere", Warszawa-Kraków: 37-44.
  • Lundegard, P. D., Swee ney, R. E. & Ririe, G. T., 2000. Soil gas methane at petroleum contaminated sites: forensic determination of origin and source. Environmental Forensics, 1: 3-10.
  • Morrison, R. T. & Boyd, R. N., 1983. Study guide to organic chemistry. Allyn and Bacon, Boston, 745 pp.
  • Mościcki, W. J., 2009. Characterization of near-surface sediments based on combined geoelectric studies at Starunia palaeontological site and vicinity (Carpathian region, Ukraine). Annales Societatis Geologorum Poloniae, 79: 333-342.
  • Porzucek, S. & Madej, J., 2009a. Recognition of geological structures at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on gravity surveys. Annales Societatis Geologorum Poloniae, 79: 357-363.
  • Porzucek, S. & Madej, J., 2009b Kotarba, M. J., 2002. Composition and origin of hydrocarbons saturating the remnants of woolly rhinoceros from Starunia, the Ukrainian Carpathians. (In Polish, English summary). Przegląd Geologiczny, 50: 531-534.
  • Kotarba, M. J. (ed.), 2005. Polish and Ukrainian geological studies (2004-2005) at Starunia - the area of discoveries of woolly rhinoceroses. Polish Geological Institute and Society of Research on Environmental Changes "Geosphere", Warszawa- Kraków, 218 pp.
  • Kotarba, M. J., 2009. Interdisciplinary studies at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) in the years 2006-2009: Previous discoveries and research, purposes, results and perspectives. Annales Societatis Geologorum Poloniae, 79: 219-241.
  • Kotarba, M. J., Alexandrowicz, S. W. & Stachowicz-Rybka, R., 2008a. Historia i pro gram dalszych badań geologicznych na obszarze byłej kopalni ozokerytu i stanowiska paleontologicznego w Staruni. (In Polish). Przegląd Geologiczny, 56: 34-441.
  • Kotarba, M. J., Dzieniewicz, M., Mościcki, W. J. & Sechman, H., 2008b. Unique Quaternary environment for discoveries of woolly rhinoceroses in Starunia, fore-Carpathian region, Ukraine: Geochemical and geoelectric studies. Geology, 36: 567-570.
  • Kotarba, M. J., Dzieniewicz, M. & Sechman, H., 2005. Geochemical survey, molecular and isotopic compositions, and genetic identification of near-surface gases from the Starunia area, fore-Carpathian region, Ukraine. In: Kotarba, M. J. (ed.), Polish and Ukrainian studies (2004-2005) at Starunia - the area of discoveries of woolly rhinoceroses. Polish Geological Institute and Society of Research on Environmental Changes "Geosphere", Warszawa-Kraków: 157-174.
  • Kotarba, M. J. & Stachowicz-Rybka, R., 2008. Wyjątkowe stanowisko paleontologiczne i środowisko osadów plejstoceńskich, w których znaleziono nosorożce włochate w Staruni (Karpaty Wschodnie). (In Polish). Przegląd. Detection of near-surface geological heterogeneity at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on microgravity survey. Annales Societatis Geologorum Poloniae, 79: 365- 374.
  • Saunders, D. F., Burson, K. R. & Thomp son, C. K., 1999. Model for hydrocarbon microseepage and related near-surface alterations. American Association of Petroleum Geologists Bulletin, 83, 1: 170-184.
  • Sechman, H. & Dzieniewicz, M., 2007. Influence of soil moisture on the results of surface geochemical survey applied to petroleum exploration. Journal of Petroleum Science and Engineering, 56, 4: 267-282.
  • Sechman, H., Kotarba, M. J. & Dzieniewicz, M., 2009. Surface geochemical survey at Starunia palaeontological site and vicinity (Carpathian region, Ukraine). Annales Societatis Geologorum Poloniae, 79: 375-390.
  • Sechman, H. & Dzieniewicz, M., 2007. Influence of soil moisture on the re sults of surface geochemical survey applied to petroleum exploration. Journal of Petroleum Science and Engineering, 56, 4: 267-282.
  • Sokołowski, T. & Stachowicz-Rybka, R., 2009. Chronostratigraphy and changes of environment of Late Pleistocene and Holocene at Starunia palaeontological site and vicinity (Carpathian region, Ukraine). Annales Societatis Geologorum Poloniae, 79: 315-331.
  • Sokołowski, T., Stachowicz-Rybka, R. & Woronko, B., 2009. Upper Pleistocene and Holocene deposits at Starunia palaeontological site and vicinity (Carpathian region, Ukraine). Annales Societatis Geologorum Poloniae, 79: 255-278.
  • Stachowicz-Rybka, R., Granoszewski, W. & Hrynowiecka- Czmielewska, A., 2009. Quaternary environmental changes at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on palaeobotanical studies. Annales Societatis Geologorum Poloniae, 79: 279-288.
  • Starobiniec, I. S., 1986. Gazokhimicheskije pokazatieli neftegazonosti i prognoz sostava uglevodorodnykh skoplenij. (In Russian). Izdatelstvo Niedra, Moskva, 200 pp.
  • Whiticar, M. J. & Faber, E., 1986. Methane oxidation in sediment and water column environments - isotope evidence. Organic Geochemistry, 11: 759-768.
  • Whiticar, M. J., Faber, E. & Schoell, M., 1986. Biogenic methane formation in marine and Fresh water environments: CO2 reduction vs. acetate fermentation - isotope evidence. Geochimicaet Cosmochimica Acta, 50: 693-709
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS7-0001-0015
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