Isotopic and molecular composition of coal-bed gas in the Amasra region (Zonguldak basin - western Black Sea)

Abstract

Previous studies on the coal-bed methane potential of the Zonguldak basin have indicated that the gases are thermogenic and sourced by the coal-bearing Carboniferous units. In this earlier work, the origin of coal-bed gas was only defined according to the molecular composition of gases and to organic geochemical properties of the respective source rocks, since data on isotopic composition of gases were not available. Furthermore, in the western Black Sea region there also exist other source rocks, which may have contributed to the coal-bed gas accumulations. The aim of this study is to determine the origin of coal-bed gas and to try a gas-source rock correlation. For this purpose, the molecular and isotopic compositions of 13 headspace gases from coals and adjacent sediments of two wells in the Amasra region have been analyzed. Total organic carbon (TOC) measurements and Rock-Eval pyrolysis were performed in order to characterize the respective source rocks. Coals and sediments are bearing humic type organic matter, which have hydrogen indices (HI) of up to 300 mgHC/gTOC, indicating a certain content of liptinitic material. The stable carbon isotope ratios (delta(13)C) of the kerogen vary from -23.1 to -27.7parts per thousand. Air-free calculated gases contain hydrocarbons up to C(5), carbon dioxide ( 98%). The stable carbon isotope ratios of methane, ethane and propane are defined as delta(13)C(1): -51.1 to -48.3parts per thousand, delta(13)C(2): -37.9 to -25.3parts per thousand, delta(13)C(3): -26.0 to -19.2parts per thousand, respectively. The deltaD(1) values of methane range from -190 to -178parts per thousand. According to its isotopic composition, methane is a mixture, partly generated bacterially, partly thermogenic. Molecular and isotopic composition of the gases and organic geochemical properties of possible source rocks indicate that the thermogenic gas generation took place in coals and organic rich shales of the Westphalian-A Kozlu formation. The bacterial input can be related to a primary bacterial methane generation during Carboniferous and/or to a recent secondary bacterial methane generation. However, some peculiarities of respective isotope values of headspace gases can also be related to the desorption process, which took place by sampling. (C) 2002 Elsevier Science Ltd. All rights reserved.