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Geochemical characterization of secondary microbial gas occurrence in the Songliao Basin, NE China

机译:东北地区松辽盆地次生微生物气赋存的地球化学特征

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A suite of natural gases from the northern Songliao Basin in NE China were characterized for their molecular and carbon isotopic composition. Gases from shallow reservoirs display clear geochemical evidence of alteration by biodegradation, with very high dryness (C_1/C_(2+)>100), high C_2/C_3 and i-C_4-C_4 ratios, high nitrogen content and variable carbon dioxide content. Isotopic values show wide range variations (δ~(13)CCH4 from -79.5‰ to -45.0‰, δ~(13)CC2H6 from -53.7‰ to -32.2‰, δ~(13)CC3H8 from -36.5‰ to -20.1‰, δ~(13)CnC4H10 from -32.7‰ to -24.5‰, and δ~(13)CCO2 from -21.6‰ to +10.5‰). A variety of genetic types can be recognized on the basis of chemical and isotopic composition together with their geological occurrence. Secondary microbial gas generation was masked by primary microbial gas and the mixing of newly generated methane with thermogenic methane already in place in the reservoir can cause very complicated isotopic signatures. System openness also was considered for shallow biodegraded gas accumulations. Gases from the Daqing Anticline are relatively wet with ~(13)C enriched methane and ~(13)C depleted CO_2, representing typically thermogenic origin. Gases within the Longhupao-Da'an Terrace have variable dryness, ~(13)C enriched methane and variable δ~(13)C of CO_2, suggesting dominant thermogenic origin and minor secondary microbial methane augment. The Puqian-Ao'nan Uplift contains relatively dry gas with ~(13)C depleted methane and ~(13)C enriched CO_2, typical for secondary microbial gas with a minor part of thermogenic methane. Gas accumulations in the Western Slope are very dry with low carbon dioxide concentrations. Some gases contain ~(13)C depleted methane, ethane and propane, indicating low maturity/primary microbial origin. Recognition of varying genetic gas types in the Songliao Basin helps explain the observed dominance of gas in the shallow reservoir and could serve as an analogue for other similar shallow gas systems.
机译:来自中国东北松辽盆地北部的一系列天然气以其分子和碳同位素组成为特征。浅层储集层中的气体显示出明显的地球化学证据,表明其被生物降解而改变,具有非常高的干燥度(C_1 / C_(2 +)> 100),高的C_2 / C_3和i-C_4 / n-C_4比率,高的氮含量和可变的二氧化碳内容。同位素值显示出宽范围的变化(δ〜(13)CCH4从-79.5‰至-45.0‰,δ〜(13)CC2H6从-53.7‰至-32.2‰,δ〜(13)CC3H8从-36.5‰至-20.1 ‰,δ〜(13)CnC4H10从-32.7‰至-24.5‰,δ〜(13)CCO2从-21.6‰至+ 10.5‰)。可以根据化学和同位素组成以及它们的地质发生来识别各种遗传类型。次级微生物气体的产生被初级微生物气体所掩盖,新生成的甲烷与储层中已经存在的产热甲烷的混合会导致非常复杂的同位素特征。对于浅层生物降解气藏也考虑了系统开放性。来自大庆背斜的气体相对较湿,富含〜(13)C的甲烷和〜(13)C的贫化CO_2,这通常是热成因。龙虎堡-大安阶地内的气体具有不同的干燥度,〜(13)C富集的甲烷和可变的~~(13)C CO_2,表明主要的成热源和次要的微生物甲烷增加。 q前—A南隆起区含有相对干燥的天然气,其中甲烷消耗的甲烷约为(13)C,而二氧化碳富集的二氧化碳约为(13)C,通常是次级微生物气体中的一小部分产热甲烷。西坡的气藏非常干燥,二氧化碳浓度低。一些气体包含〜(13)C贫化的甲烷,乙烷和丙烷,表明其成熟度低/主要微生物来源。对松辽盆地不同成因天然气类型的认识有助于解释在浅层储层中观测到的天然气优势,并且可以作为其他类似浅层天然气系统的类似物。

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