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Numerical simulation of chemical potential dominated fracturing fluid flowback in hydraulically fractured shale gas reservoirs

机译:水力压裂页岩气藏中以化学势为主的压裂液回流的数值模拟

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To find out the impact of chemical potential difference between the low salinity fracturing fluid and the high salinity formation water on fracturing fluid flowback, a chemical potential difference expression of fracturing fluid and formation water was deduced, on this basis, a mathematical model which considers viscous force, capillary force and osmosis pressure driven gas-water flow in matrix-fracture system was built, the flow back performance of fracturing fluid driven by chemical potential difference was simulated, and the formation water saturation and salt concentration profile with flow back time were analyzed. The results show that in the process of flow back, the water molecules in the matrix driven by the chemical potential difference continually migrated to the deeper reservoirs, while salt ions in the matrix constantly spread to the fractures. After 168 h of fracturing-fluid flow back, the migration distance of water was up to 40 cm, and the salt concentration near the fracture surface increased by 0.841%, and the cumulative flowback ratio of the gas well was only 22.1%. The cumulative flowback ratio would be 23.5%, 32.4% and 41.1% respectively, without taking into account the effect of gas absorption, chemical osmosis or capillary imbibition. The capillary imbibition and chemical osmosis seriously hindered the fracturing-fluid flow back, therefore, the two factors should be fully considered in the post-fracturing evaluation of shale gas wells.
机译:为了找出低盐度压裂液与高盐度地层水之间的化学势差对压裂液返排的影响,在此基础上推导了压裂液与地层水的化学势差表达式,在此基础上建立了考虑粘性的数学模型。建立了基质-压裂系统中气动力,毛细力和渗透压驱动的气水流,模拟了由化学势差驱动的压裂液的返流性能,分析了随返流时间的地层水饱和度和盐分分布。结果表明,在返排过程中,由化学势差驱动的基质中的水分子不断迁移至较深的储层,而基质中的盐离子则不断扩散至裂缝。压裂液回流168 h后,水的运移距离达到40 cm,裂缝表面附近的盐分浓度增加了0.841%,气井的累计返排率仅为22.1%。如果不考虑气体吸收,化学渗透或毛细管吸收的影响,累积回流比率分别为23.5%,32.4%和41.1%。页岩气井压裂后评价中,毛细吸收和化学渗透作用严重阻碍了压裂液的回流,因此必须充分考虑这两个因素。

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