Liu Xuefen, Kang Yili, Li Jianfeng, Chen Zhanjun, Ji Anzhao, Xu Hongwu
School of Energy Engineering, LongDong University, Qingyang 745000, China.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China.
ACS Omega. 2020 Jun 10;5(24):14316-14323. doi: 10.1021/acsomega.0c00569. eCollection 2020 Jun 23.
The development of tight oil has started relatively late, and the flow mechanisms and fluid movability are still research spotlights. The goal of this paper is to investigate the percolation characteristics and fluid movability of the Chang 6 tight sandstone oil layer in the Upper Triassic Yanchang Formation, Ordos Basin, China. Results show that (1) at low flow velocity, the percolation curve of flow velocity vs pressure gradient is a concave-up nonlinear curve and does not pass through the origin. It is more difficult for oil flow than water flow in cores with similar permeability due to rock wettability and fluid apparent mobility. The application of back pressure makes the nonlinear stage eliminated and the percolation character improved. (2) Two-phase flow tests reveal that oil-phase permeability decreases faster in samples with lower permeability, and the coexistent flow region of oil and water is relatively narrow. The contribution of oil recovery mainly happens at the early stage. The permeability at the isotonic point reduces with the decrease of sample permeability. (3) Flow during water flooding can be roughly divided into four stages according to the injection pressure and flow change. The injection pressure experiences stages of increasing to a peak, then decreasing, and finally becoming stable, accompanied by an increase of oil production until water breaks through. (4) The pore throats of the target reservoir mainly range from 0.001 to 10 μm, and the bound water mainly distributes in pores less than 0.2 μm. The irreducible water saturation is 30-35%, and the movable fluid saturation is 65-70%, mainly distributed in pores at 0.2-10.0 μm with a maximum of 2.0 μm. The results will supplement the existing knowledge of percolation characters and fluid movability in tight sandstone oil reservoirs.
致密油的开发起步相对较晚,其渗流机制和流体可动性仍是研究热点。本文旨在研究中国鄂尔多斯盆地三叠系延长组长6致密砂岩油层的渗流特征和流体可动性。结果表明:(1)在低流速下,流速与压力梯度的渗流曲线为上凹的非线性曲线,且不经过原点。由于岩石润湿性和流体表观迁移率,在渗透率相近的岩心中,油流比水流更困难。施加回压可消除非线性阶段,改善渗流特性。(2)两相流试验表明,渗透率较低的样品中油相渗透率下降更快,油水共存流动区域相对较窄。原油采收主要发生在早期。等渗点处的渗透率随样品渗透率降低而减小。(3)根据注入压力和流量变化,水驱过程中的流动大致可分为四个阶段。注入压力经历先升高到峰值、再降低、最后稳定的阶段,同时产油量增加直至水突破。(4)目标储层的孔喉主要在0.001~10μm之间,束缚水主要分布在小于0.2μm的孔隙中。束缚水饱和度为30%~35%,可动流体饱和度为65%~70%,主要分布在0.2~10.0μm的孔隙中,最大为2.0μm。研究结果将补充致密砂岩油藏渗流特征和流体可动性的现有知识。