致密油储层微观孔隙网络特征对可动流体性质的影响

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-11-14 DOI:10.1155/2023/7464640
Jie Gao, Hu Wang, Xiaojun Ding, Qingxiao Yuchi, Qiang Ren, Bo Ning, Junxiang Nan
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To promote this process, in this study, core samples obtained from the Chang 7 reservoir of the Triassic Yanchang Formation in the Longdong region of Ordos Basin, China, were tested. The results show that the average movable fluid percentage and average movable fluid porosity of the total 16 core samples are 36.01% and 2.77%, respectively. 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引用次数: 0

摘要

流体的流动行为,一般称为渗流,可以决定油气和盐水的运移行为。可动流体属性作为渗流特性评价的重要参数之一,通常用于致密油储层流体流动能力评价。利用核磁共振技术对可动流体百分比和可动流体孔隙度进行实验,可以对可在多孔介质中流动的流体量进行真实评估。其他技术也用于分析调节可动流体参数差异的主要因素。然而,对流体流动特性的研究一般是基于传统的方法,而从孔隙尺度的角度来研究渗流特征仍然是一个迷。为了促进这一进程,本研究对鄂尔多斯盆地陇东地区三叠系延长组长7储层的岩心样品进行了测试。结果表明,16个岩心样品的平均可动流体百分比和平均可动流体孔隙度分别为36.01%和2.77%。可动流体主要存在于中大型孔隙中,相应的t2弛豫时间大于10 ms。t2分布主要呈现四种典型模式:(1)两峰振幅相近的双峰分布(占6.25%),(2)右峰高左峰低的双峰分布(占18.75%),(3)左峰高右峰低的双峰分布(占56.25%),(4)单峰分布(占18.75%)。孔隙结构非均质性与可动流体参数密切相关;可动流体参数与岩心喉道半径和渗透率具有较好的相关性。由于物性、粘土矿物含量、微裂缝、孔隙结构特征等方面的差异,致密油储层可动流体参数与微观特征因素存在明显差异。该研究为可动流体物性评价提供了一个新的视角,相关研究结果对油田开发具有一定的指导意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Impact of Microscopic Pore Network Characteristics on Movable Fluid Properties in Tight Oil Reservoir
The fluid flow behavior, generally referred to as seepage, could determine the hydrocarbon and brine movement behavior. Movable fluid property, as one of the vital parameters for seepage characteristic evaluation, was generally used for tight oil reservoirs’ fluid flow ability assessment. The nuclear magnetic resonance technique was used to experiment with movable fluid percentage and movable fluid porosity, which can provide a realistic assessment of the amount of fluid that can flow in the porous media. Other techniques were also used to analyze the main factors in regulating the differences in movable fluid parameters. However, the research about fluid flow behavior was generally based on traditional methods, while the seepage characteristics from the pore-scale view are still a myth. To promote this process, in this study, core samples obtained from the Chang 7 reservoir of the Triassic Yanchang Formation in the Longdong region of Ordos Basin, China, were tested. The results show that the average movable fluid percentage and average movable fluid porosity of the total 16 core samples are 36.01% and 2.77%, respectively. The movable fluid exists mainly in the midlarge pores with the corresponding T 2 relaxation time over 10 ms. T 2 distributions mainly present four typical patterns: (1) bimodal distribution with similar amplitudes of the two peaks (occupying 6.25%), (2) bimodal distribution with higher right peak and lower left peak (occupying 18.75%), (3) bimodal distribution with higher left peak and lower right peak (occupying 56.25%), and (4) unimodal distribution (occupying 18.75%). Pore structure heterogeneity is closely related to the movable fluid parameters; the movable fluid parameters exhibit a relatively good correlation with core throat radius as well as permeability. There is an obvious difference between the movable fluid parameters and the microscopic characteristic factors in tight oil reservoirs due to the difference in physical properties, clay mineral content, microcracks, and pore structure characteristics. This research has provided a new perspective for the movable fluid property evaluation, and the relevant results can give some advice for the oil field development.
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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