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Diagenesis and its influence on reservoir quality and oil-water relative permeability: A case study in the Yanchang Formation Chang 8 tight sandstone oil reservoir, Ordos Basin, China

机译:成岩作用及其对油藏质量和油水相对渗透率的影响-以鄂尔多斯盆地长8致密砂岩油藏为例

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Different from conventional reservoirs, unconventional tight sand oil reservoirs are characterized by low or ultra-low porosity and permeability, small pore-throat size, complex pore structure and strong heterogeneity. For the continuous exploration and enhancement of oil recovery from tight oil, further analysis of the origins of the different reservoir qualities is required. The Upper Triassic Chang 8 sandstone of the Yanchang Formation from the Maling Oilfield is one of the major tight oil bearing reservoirs in the Ordos Basin. Practical exploration demonstrates that this formation is a typical tight sandstone reservoir. Samples taken from the oil layer were divided into 6 diagenetic facies based on porosity, permeability and the diagenesis characteristics identified through thin section and scanning electron microscopy. To compare pore structure and their seepage property, a high pressure mercury intrusion experiments (HPMI), nuclear magnetic resonance (NMR), andwater-oil relative permeability test were performed on the three main facies developed in reservoir. The reservoir quality and seepage property are largely controlled by diagenesis. Intense compaction leads to a dominant loss of porosity in all sandstones, while different degrees of intensity of carbonate cementation and dissolution promote the differentiation of reservoir quality. The complex pore structure formed after diagenesis determines the seepage characteristics, while cementation of chlorite and illite reduce the effective pore radius, limit fluid mobility, and lead to a serious reduction of reservoir permeability.
机译:与常规油藏不同,非常规致密砂岩油藏的孔隙度和渗透率低或超低,孔喉尺寸小,孔隙结构复杂,非均质性强。为了不断探索和提高致密油的采收率,需要进一步分析不同储层质量的成因。马岭油田延长组长三叠统长8砂岩是鄂尔多斯盆地主要的致密油储层之一。实际勘探表明,该地层是典型的致密砂岩储层。根据孔隙率,渗透率和通过薄切片和扫描电子显微镜鉴定的成岩特征,将从油层中采集的样品分为6个成岩相。为了比较孔隙结构及其渗透性,对储层中开发的三个主要相进行了高压压汞实验(HPMI),核磁共振(NMR)和水油相对渗透率测试。储层质量和渗流特性很大程度上受成岩作用控制。强烈的压实作用导致所有砂岩孔隙度的主要损失,而不同程度的碳酸盐胶结作用和溶解强度促进了储层质量的分化。成岩作用后形成的复杂孔隙结构决定了渗流特征,而绿泥石和伊利石的胶结作用降低了有效孔隙半径,限制了流体的流动性,并导致储层渗透率的严重降低。

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