首页> 外文会议>SPE Kingdom of Saudi Arabia Annual Technical Symposium and Exhibition >The Impact of the Geochemical Coupling on the Fate of Fracturing Fluid, Reservoir Characteristics and Early Well Performance in Shale Reservoirs.
【24h】

The Impact of the Geochemical Coupling on the Fate of Fracturing Fluid, Reservoir Characteristics and Early Well Performance in Shale Reservoirs.

机译:地球化学耦合对岩土储层压裂液,储层特性及早期性能的影响。

获取原文

摘要

The fate of the fracturing fluid in shale reservoirs is still a controversial issue. Despite the low recovery observed in field reports, neither the fate nor the impact of these trapped fluids is well-understood. The combination of the large surface area, mild reactive nature of shale and the massive trapped volume of fracturing fluids raises a question on the impact that geochemical interactions have on load recovery, well performance and reservoir characteristics, which is the focus of this study. A fit-for-purpose model is built where a hydraulic fracture stage is modelled using LG-LR-DK model. The initial conditions are simulated by injecting the fracturing fluid, then shutting-in the well to allow the fluids to be soaked into the formation. Different relative permeability sets are used for high and low salinity water since the fluid's mobility is affected by its salinity. Actual connate water composition from Haynesville shale is used to study the impact of connate composition on geochemical coupling. The formation mineralogy and fracturing fluid composition impact on gas and load recovery is investigated. The introduction of the oxygenated, low salinity, fracturing fluid to a reducing environment would definitely catalyze both precipitation and dissolution reactions depending on the formation mineralogy. The dissolution and precipitation rates show a positive correlation with the carbonate content of the rock. Interestingly, the incorporation of the dependence of relative permeability on ion exchange and fluid salinity might reveal the fate of the fracturing fluid. Overestimation of both gas and load recovery is observed when geochemical coupling is neglected. In addition, sea water shows an enhanced performance suggesting a good alternative fracturing fluid. Surprisingly, better performance is observed for less saline connate water cases. The carbonates reactions outweigh the clays reactions in most cases. Also, treating carbonates as only calcite results in more reactions compared to the dolomite case. Sensitivity analysis suggests that the concentration of SO4, K and Na ions in the fracturing fluid, and illite and calcite mineral content of the rock, along with the reservoir temperature are the main key factors affecting well performance. It is worth noting that the salinity contrast between the injected fluid and the formation brine shows a negative correlation with well performance.
机译:页岩水库中压裂液的命运仍然是一个有争议的问题。尽管在现场报告中观察到的恢复较低,但既不是命运也不是这些被困流体的影响。大表面积,页岩的轻度反应性和压裂液的大规模捕获体积的组合引发了地球化学相互作用对负荷回收,井性能和储层特征的影响,这是本研究的重点。建立了一种适合的模型,其中使用LG-LR-DK模型建模液压骨折阶段。通过注入压裂液,然后置于井中来模拟初始条件,以允许流体浸泡到地层中。由于流体的迁移率受其盐度的影响,不同的相对渗透率用于高盐度水。 Haynesville Shale的实际合成水组合物用于研究恶性组合物对地球化学偶联的影响。研究了地层矿物学和压裂液组合物对气体和负荷回收的影响。引入含氧,低盐度,压裂液对还原环境肯定会根据地层矿物学催化沉淀和溶解反应。溶出和沉淀率显示与岩石的碳酸含量呈正相关。有趣的是,纳入相对渗透性对离子交换和液体盐度的依赖性可能揭示压裂液的命运。忽略地球化学耦合时,观察到气体和负载恢复的高估。此外,海水显示出增强的性能,表明良好的替代压裂液。令人惊讶的是,对于少盐酸盐的水箱,观察到更好的性能。在大多数情况下,碳酸盐反应超过粘土反应。此外,与二粒子案例相比,只处理碳酸盐的结果导致更多的反应。敏感性分析表明,压裂液中SO4,K和Na离子的浓度,岩石和岩石的岩石和方解石矿物质含量以及水库温度是影响良好性能的主要关键因素。值得注意的是,注入的流体和地层盐水之间的盐度对比显示出与井的性能的负相关。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号