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Gas-water relative permeability measurement of high temperature and high pressure tight gas reservoirs

机译:高温高压致密气藏气水相对渗透率测量

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Generally, gas-water relative permeability curves of tight gas reservoirs are obtained from unsteady experiment under room temperature and normal pressure, which greatly differs from the curves under high temperature and high pressure. In this research, the relative permeability curves of three cores were firstly measured using conventional standard method by displacing formation water with nitrogen under room temperature and normal pressure. Then the relative permeability curves of the same cores were measured by displacing formation water with natural gas on one self-developed full-diameter seepage flow equipment (200 °C, 200 MPa) under reservoir conditions (160 °C, 116 MPa) after several processing of the cores. Difference between the relative permeability curves obtained by the two methods shows that, under high temperature and high pressure, there exists a larger two-phase seepage zone and lower irreducible water saturation. At the same gas saturation, gas relative permeability under high temperature and high pressure is higher than that under room temperature and normal pressure, which means, under reservoir situation, the two-phase flow ability of gas and water is stronger and the irreducible water saturation is lower in tight gas reservoirs. The gas-water viscosity ratio, gas-water density ratio and interfacial tension are lower under this situation, which leads to higher sweep efficiency.
机译:通常,致密气藏的气水相对渗透率曲线是在常温常压下的非稳态实验得到的,与高温高压下的曲线有很大的不同。在这项研究中,首先使用常规标准方法通过在室温和常压下用氮气置换地层水来测量三个岩心的相对渗透率曲线。然后,在储层条件(160°C,116 MPa)中,经过数次注水后,在一台自行开发的全直径渗流设备(200°C,200 MPa)上用天然气置换地层水,测量了相同岩心的相对渗透率曲线。核心处理。两种方法得到的相对渗透率曲线的差异表明,在高温高压下,存在较大的两相渗流区,较低的不可还原水饱和度。在相同的饱和度下,高温高压下的相对渗透率要高于室温和常压下的相对渗透率,这意味着在储层条件下,水和气的两相流动能力更强,水饱和度无法降低。在致密气藏中较低。在这种情况下,气水粘度比,气水密度比和界面张力较低,这导致较高的吹扫效率。

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