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Varying law of water saturation in the depletion-drive development of sandstone gas reservoirs

机译:砂岩气藏耗竭开发中含水饱和度的变化规律

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The varying law of on-way water saturation in the depletion-drive development (the formation pressure: 20 MPa depleting to abandonment pressure) of water-bearing gas reservoirs was studied through four groups of cores whose physical properties represent the rocks in Sichuan Xujiahe gas reservoirs, and cores permeability are 1.630×10?3μm2, 0.580×10?3μm2, 0.175×10?3μm2, 0.063×10?3μm2, respectively. Combined with the rock characteristics of microscopic pore structure and capillary pressure, the interaction mechanism between different permeability sandstone and water was analyzed and verified on two wells. The conclusions are as follows: (1) The water trapping effect in the sandstone reservoir is dependent on the sandstone reservoir permeability (the critical value is 0.175×10?3? 0.580×10?3μm2). (2) The formation with permeability greater than 0.580×10?3μm2is characterized with big size pore and throat, low capillary pressure and weak trapping effect. So a portion of pore water would be displaced by gas and became movable water. (3) The tight formation with permeability less than 0.175×10?3μm2is characterized with small size pore and throat, high capillary pressure and strong trapping effect. When the rock core is saturated by moisture gas, the pore water would not be displaced by gas and would be trapped in the sandstone, which results in the water saturation increases rather than decreases. Drawdown pressure should be kept within a proper range to extend the life cycle of wells.
机译:通过四组岩心代表四川徐家河气田的岩石,研究了含水驱气藏驱油开发中地层水饱和度的变化规律(地层压力:20 MPa,耗水至废弃压力)。储层和岩心渗透率分别为1.630×10?3μm2、0.580×10?3μm2、0.175×10?3μm2、0.063×10?3μm2。结合岩石微观孔隙结构特征和毛细压力,分析了两口井不同渗透率砂岩与水的相互作用机理。结论如下:(1)砂岩储层的集水效果取决于砂岩储层的渗透率(临界值为0.175×10?3?0.580×10?3μm2)。 (2)渗透率大于0.580×10?3μm2的地层,具有较大的孔喉分布,毛管压力低,捕集作用弱。因此,一部分孔隙水将被气体置换而成为可移动水。 (3)渗透率小于0.175×10?3μm2的致密地层,孔隙和喉孔小,毛细压力高,捕集作用强。当岩心被湿气饱和时,孔隙水将不会被气体置换而被困在砂岩中,这导致水饱和度增加而不是减少。压降压力应保持在适当范围内,以延长油井的使用寿命。

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