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Experimental investigation on water adsorption and desorption isotherms of the Longmaxi shale in the Sichuan Basin, China

机译:四川盆地龙马西页岩水吸附和解吸等温水试验研究

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The understanding of water adsorption and desorption behavior in the shale rocks is of great significance in the reserve estimation, wellbore stability and hydrocarbon extraction in the shale gas reservoirs. However, the water sorption behavior in the shales remains unclear. In this study, water vapor adsorption/desorption isotherms of the Longmaxi shale in the Sichuan Basin, China were conducted at various temperatures (30?°C, 60?°C) and a relative pressure up to 0.97 to understand the water sorption behavior. Then the effects of temperature and shale properties were analyzed, and the water adsorption, hysteresis, saturation and capillary pressure were discussed. The results indicate that water adsorption isotherms of the Longmaxi shale exhibit the type II characteristics. The water molecules initially adsorb on the shale particle/pore surfaces at low relative pressure while the capillary condensation dominates at high relative pressure. Temperature favors the water sorption in the shales at high relative pressure, and the GAB isotherm model is found to be suitable for describe the water adsorption/desorption behavior. The high organic carbon and full bedding are beneficial to water adsorption in the shales while the calcite inhibits the behavior. There exists the hysteresis between water adsorption and desorption at the whole relative pressure, which suggests that the depletion of condensed water from smaller capillary pores is more difficult than that from larger pores, and the chemical interaction contributes to the hysteresis loop for water sorption. The capillary pressure in the shales can be up to the order of several hundreds of MPa, and thus the desorption of water from the shales may not be as easy as the water adsorption due to the high capillary pressure, which results in water retention behavior in the shale gas reservoirs. These results can provide insights into a better understanding of water sorption behavior in the shale so as to optimize extraction conditions and predict gas productivity in the shale gas reservoirs.
机译:在页岩气藏的储备估计,井筒稳定性和烃萃取中,对页岩岩石中的水吸附和解吸行为的理解具有重要意义。然而,Shales中的水吸附行为仍然不清楚。在这项研究中,四川盆地龙曼西页岩的水蒸气吸附/解吸等温度在各种温度(30?°C,60℃)和高达0.97的相对压力下进行,以了解水吸附行为。然后分析温度和页岩性能的影响,并讨论了水吸附,滞后,饱和度和毛细管压力。结果表明,龙马西页岩的水吸附等温线表现出II型特征。水分子最初在低相对压力下吸附在页岩粒子/孔表面上,同时毛细血管缩合在高相对压力下占主导地位。在高相对压力下,温度有利于Shales中的水吸附,并且发现GAB等温线模型适合描述水吸附/解吸行为。高有机碳和全套床上用品对Shales中的水吸附有益,而核石路径抑制行为。在整个相对压力下存在水吸附和解吸之间的滞后,这表明来自较小毛细血管孔的冷凝水的耗尽比从较大的孔隙中更困难,化学相互作用有助于滞后回水用于水吸附。 Shales中的毛细管压力可以达到几百MPa的顺序,因此来自Shales的水的解吸可能不如由于高毛细管压力导致的水吸附而容易,这导致水保留行为页岩气水库。这些结果可以在页岩中更好地理解水吸附行为的洞察中,以优化提取条件并预测页岩气藏中的气体生产率。

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