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Towards Relative Permeability Measurements in Tight Gas Formations

机译:致密气层中的相对渗透率测量

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Relative permeability is a concept used to convey the reduction in flow capability due to the presence of multiple fluids. Relative permeability governs the multiphase flow, therefore it has a significant importance in understanding the reservoir behavior. These parameters are routinely measured on conventional rocks, however their measurement becomes quite challenging for low permeability rocks such as tight gas formations.This study demonstrates a methodology for relative permeability measurements on tight gas samples. The gas permeability has been measured by the Step Decay method and two different techniques have been used to vary the saturations: steady state flooding and vapor desorption.Series of steady-state gas/water simultaneous injection have been performed on a tight gas sample. After stabilization at each injection ratio, NMR T2, NMR Saturation profile and low pressure Step Decay gas permeability have been measured. In parallel, progressive desaturation by vapor desorption technique has been performed on twin plugs. After stabilization at each relative humidity level the NMR T2 and Step Decay gas permeability have been measured in order to compare and validate the two approaches.The techniques were used to gain insight into the tight gas two phase relative permeability of extremely low petrophysical properties (K<100 nD, phi < 5 pu) of tight gas samples of Pyrophyllite outcrop.The two methods show quite good agreement. Both methods demonstrate significant permeability degradation at water saturation higher than irreducible. NMR T2 measurements for both methods indicates bimodal T2-distributions, and desaturation first occurs on low T2 signal (small pores).Comparison of humidity drying and steady-state desaturation technique has shown a 12-18 su difference between critical water saturation (Swc) measured in gas/water steady-state injection and irreducible saturation (Swirr) measured by vapor desorption.
机译:相对渗透率是用于传达由于存在多种流体而导致流量降低的概念。相对渗透率控制着多相流,因此对于理解储层行为具有重要意义。这些参数通常在常规岩石上进行测量,但是对于低渗透率岩石(如致密气地层)而言,它们的测量变得颇具挑战性。这项研究证明了对致密气样品进行相对渗透率测量的方法。气体渗透率已通过逐步衰减法进行了测量,并已使用两种不同的技术来改变饱和度:稳态驱替和蒸汽脱附。已在致密的气体样品上进行了一系列的稳态气/水同时注入。在每种注入比例下稳定后,已测量了NMR T2,NMR饱和曲线和低压阶跃衰减气体渗透率。平行地,已经通过蒸气解吸技术对双塞进行了渐进式去饱和。在每个相对湿度水平稳定之后,已测量了NMR T2和阶梯衰减气体渗透率,以便比较和验证这两种方法。该技术用于深入了解岩石物理性质极低的致密气两相相对渗透率(K叶蜡石露头致密气样品的<100 nD,phi <5 pu)这两种方法显示出很好的一致性。两种方法都表明,在水饱和度下,渗透率会显着降低,而渗透率却无法降低。两种方法的NMR T2测量结果均显示了双峰T2分布,并且首先在低T2信号(小孔)上发生了去饱和。湿法干燥和稳态去饱和技术的比较表明,临界水饱和度(Swc)之间存在12-18 su的差异在气/水稳态注入条件下测得的饱和度,以及通过蒸气解吸测量得到的不可还原饱和度(Swirr)。

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