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首页> 外文期刊>Journal of natural gas science and engineering >Preliminary study on shale gas microreservoir characteristics of the Lower Silurian Longmaxi Formation in the southern Sichuan Basin, China
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Preliminary study on shale gas microreservoir characteristics of the Lower Silurian Longmaxi Formation in the southern Sichuan Basin, China

机译:四川盆地南部下志留统龙马溪组页岩气微储层特征初步研究

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The Lower Silurian Longmaxi Formation marine shales are the main shale gas reservoirs in the Sichuan Basin, SW China. The present study analyzes the characteristics of the Longmaxi shales using samples selected from wells N1 and N2 in the Changning block, southern Sichuan Basin. Several methods, including X-ray diffraction (XRD), scanning electron microscopy (SEM), helium gas expansion and low pressure nitrogen (N2) adsorption/desorption, were used to investigate the mineralogical composition, geochemical characteristics, pore structure and other characteristics of the shales. The total organic carbon (TOC) contents of the samples range from 0.8 to 6.429%, and the thermal maturity is at the overmature stage. Two wells are rich in quartz and clay, with the average contents of 39.4% and 29.6%, respectively. The Longmaxi shales have the specific surface area and total pore volume around 16.6 m(2)/g and 0.0165 mL/g, respectively. It is suggested that the TOC content contributes significantly to the average pore size, specific surface area and total pore volume, and the thermal maturity strongly influences the development of porosity, as does the mineralogical composition. Based on imagine analysis, we classify shale gas microreservoirs into three types: organic matter with microfractures, organic matter alone and organic matter with mineral pores (interparticle pores (InterP pores) and intraparticle pores (IntraP pores)). The first type is the best for shale gas exploitation. The second type and the type of organic matter with InterP pores are better, while the type of organic matter with IntraP pores is almost useless. The analysis results show that the microreservoirs of well N1 mainly contain the type of organic matter with InterP pores, while the microreservoirs of well N2 are dominated by the type of organic matter with InterP pores and the type of organic matter with microfractures. Combing all the analysis results and their influencing factors, we consider that well N2 is more favorable for gas production than well N1. (C) 2016 Elsevier B.V. All rights reserved.
机译:下志留纪龙马溪组海相页岩是中国西南四川盆地的主要页岩气藏。本研究使用选自四川盆地南部长宁区块N1和N2井的样本分析了Longmaxi页岩的特征。 X射线衍射(XRD),扫描电子显微镜(SEM),氦气膨胀和低压氮(N2)吸附/脱附等几种方法被用来研究矿物组成,地球化学特征,孔隙结构和其他特征。页岩。样品中的总有机碳(TOC)含量在0.8至6.429%的范围内,热成熟度处于过成熟阶段。两口井均富含石英和粘土,平均含量分别为39.4%和29.6%。 Longmaxi页岩的比表面积和总孔体积分别约为16.6 m(2)/ g和0.0165 mL / g。建议TOC含量显着影响平均孔径,比表面积和总孔体积,并且热成熟度和矿物组成也强烈影响孔隙度的发展。基于想象分析,我们将页岩气微储层分为三种类型:带微裂缝的有机质,仅有机质和具有矿物孔隙(颗粒间孔隙(InterP孔隙)和颗粒内孔隙(IntraP孔隙)的有机物质)。第一种类型最适合页岩气开采。第二种类型和带InterP孔的有机物的类型更好,而带IntraP孔的有机物的类型几乎没有用。分析结果表明,N1井的微储层主要为具有InterP孔隙的有机质类型,而N2井的微储层主要为具有InterP孔隙的有机质类型和微裂缝有机质的类型。综合所有分析结果及其影响因素,我们认为N2井比N1井更有利于天然气生产。 (C)2016 Elsevier B.V.保留所有权利。

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