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Mass flow rate prediction of shale gas considering gas diffusion and water film evaporation

机译:考虑气体扩散和水膜蒸发的页岩气体质量流量预测

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The difference between organic and inorganic matters in shale matrix has significantly influence on the transport capacity of shale gas and the total production of shale gas further. Previous studies have demonstrated that the organic pores are hydrophobic and the inorganic pores are hydrophilic. Therefore, the water film can be adsorbed on the walls of the inorganic pores. However, the evaporation of water film in inorganic pore is often overlooked due to the analytical challenge and the effect of the water film evaporation on gas transport capacity is rarely discussed. Thus, it is important to accurately predict mass flow rate of the shale gas through a single nanopore whether it is organic or inorganic. In this article, the mass flow rate prediction model of the organic pore is developed firstly, which considers the interactions of slip flow, gas adsorbed at pore walls, surface diffusion for adsorbed gas and gas diffusing from the kerogen which contains dissolved shale gas in organic pores at nanoscale. This model is then used to investigate the influences of initial pressure, pressure gradient, and thickness of kerogen on the gas mass flow rate. For inorganic pores, the mass flow rate prediction model is developed secondly and the interactions of water film and the evaporation of water film have been considered. The influence of evaporation, initial humidity, water-methane diffusivity is investigated on the gas mass flow rate. Results show that diffusion from kerogen plays an important role in the transport capacity of shale gas. Both higher pressure gradient and thicker kerogen can contribute to higher gas mass flow rate and higher diffusion from kerogen. Higher initial pressure and thicker kerogen can contribute to the lower shale gas desorption. The thicker kerogen can contribute to the higher surface diffusion. The evaporation in inorganic pore should not be ignored, because it impacts gas mass flow rate and can contribute to the higher flow rate. Experimental data was compared with our prediction model, which proves the correctness and validity of our model.
机译:页岩基质有机和无机物质之间的差异显着影响页岩气的运输能力和进一步的页岩气的总产量。以前的研究表明,有机孔是疏水性的,无机孔是亲水的。因此,水膜可以吸附在无机孔的壁上。然而,由于分析攻击,通常忽略了无机孔中水膜的蒸发,并且很少讨论水膜蒸发对气体运输能力的影响。因此,无论是有机或无机的单个纳米孔,都很重要。在本文中,首先开发了有机孔的质量流量预测模型,其考虑了滑动流的相互作用,吸附在孔壁上的气体,吸附气体的表面扩散和从含有有机溶解的页岩气中延伸的吸附气体和气体的气体扩散纳米尺度的毛孔。然后使用该模型来研究初始压力,压力梯度和基因原厚度对气体质量流量的影响。对于无机孔,已经开发了质量流量预测模型,并考虑了水膜的相互作用和水膜的蒸发。对气体质量流速研究了蒸发,初始湿度,水 - 甲烷扩散率的影响。结果表明,从恶作子的扩散在页岩气的运输能力中起着重要作用。较高的压力梯度和较厚的角化剂可以有助于较高的气体质量流量和来自Kerogen的更高的扩散。更高的初始压力和更厚的角化剂可以有助于较低的页岩气体解吸。较厚的基因可能有助于较高的表面扩散。无机孔中的蒸发不应忽略,因为它会影响气体质量流量并且可以促进较高的流速。与我们的预测模型进行比较实验数据,证明了我们模型的正确性和有效性。

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