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Studies of the storage and transport of water and oil in organic-rich shale using vacuum imbibition method

机译:利用真空吸收法研究富含有机物的页岩中水和油的储运

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The inorganic pores, organic pores, and kerogen matrix are important media to store water and oil in shale rocks. We present a vacuum imbibition method to identify the volume of water and oil in these media. Before the experiments, comprehensive rock characterizations were carried out on shale samples from Shahejie Formation combining various methods including N-2 adsorption, scanning electron microscope (SEM), X-ray diffraction, and RockEval pyrolysis. Total organic carbon (TOC) accounts for 1.59-5.97% of total rock weight. Kerogen thermal maturity (R-o) of the studied samples is 0.62-1.05%. Then, vacuum imbibition experiments were conducted on shale samples using water and n-dodecane. The accurate volumes of water in organic pores, oil in inorganic pores and organic pores, and the volume of dissolved oil were determined from vacuum imbibition experiments. The effects of Ro on shale storage were analyzed. Furthermore, novel mathematical models of oil and water vacuum imbibition in shale were proposed. The water imbibition in inorganic pores is a capillary flow. The oil imbibition in shale includes capillary flow in pore structures and diffusion in kerogen. The pore-kerogen double diffuse layer (PKDDL) physical model was proposed for the mechanisms of the hydrocarbon mass transfer between pore structures and kerogen. The capillary pressure and the dissolution rate constants were obtained by matching mathematical models with experimental results. This study provides new methods to evaluate the water and oil storage and transfer in organic-rich shale and advances the crucial mechanisms for the evaluation and development of shale reservoirs.
机译:无机孔隙,有机孔隙和干酪根基质是在页岩中储存水和油的重要介质。我们提出一种真空吸收方法,以识别这些介质中的水和油的量。在实验之前,结合N-2吸附,扫描电子显微镜(SEM),X射线衍射和RockEval热解等方法,对来自沙河街组的页岩样品进行了全面的岩石表征。总有机碳(TOC)占总岩石重量的1.59-5.97%。研究样品的干酪根热成熟度(R-o)为0.62-1.05%。然后,使用水和正十二烷对页岩样品进行真空吸收实验。通过真空吸收实验确定有机孔中水的准确体积,无机孔和有机孔中油的准确体积以及溶解油的体积。分析了Ro对页岩储量的影响。此外,提出了页岩油和水真空吸收的新数学模型。无机孔中的水吸收是毛细流。页岩中的油吸收包括孔隙结构中的毛细流动和干酪根中的扩散。提出了孔隙-干酪根双重扩散层(PKDDL)物理模型,用于孔隙结构和干酪根之间烃类物质转移的机理。通过将数学模型与实验结果进行匹配,获得了毛细管压力和溶出速率常数。该研究为评价富含有机质的页岩中的水和油的储藏和转移提供了新的方法,并为评价和开发页岩储层的关键机制提供了重要的机制。

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