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首页> 外文期刊>Journal of molecular modeling >Effect of CO2 and H2O on the behavior of shale gas confined inside calcite [104] slit-like nanopore: a molecular dynamics simulation study
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Effect of CO2 and H2O on the behavior of shale gas confined inside calcite [104] slit-like nanopore: a molecular dynamics simulation study

机译:CO2和H2O对方解石内狭窄的岩石气体行为的影响[104]狭缝纳米孔:分子动力学模拟研究

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The effect of CO2 and H2O on the behavior of shale gas confined in calcite [104] slit-like nanopore is investigated using molecular dynamics simulation technique. The study is relevant as the advancement of enhance gas recovery (EGR) technologies requires in-depth atomistic understanding of the hydrocarbons, water, carbon dioxide, and other fracturing fluid constituents inside the nanopores of shale gas reservoirs. We are considering carbon dioxide (CO2) because it is an attractive displacing agent for enhanced gas recovery and has the potential to be an "exotic" fracturing fluid. Water (H2O) is considered as it is the major component of water-based fracturing fluids. The structural and dynamical properties of the confined species are computed. The results indicate that the presence of CO2 and H2O in the nanopore drastically affects the behavior of shale gas. The shale gas molecules that were tightly packed near the pore wall displaced towards the center by CO2 and H2O molecules. A new layer of carbon dioxide and water is formed near the pore wall. Further investigation reveals that CO2 molecules align themselves flat near the surface, whereas H2O molecules have directional orientation with oxygen atoms of water molecules pointing towards to wall. The predicted lateral (in-plane) self-diffusion coefficient values of methane, ethane, carbon dioxide and water indicate complex dynamics inside the pore. The investigation shows the fastest dynamics for methane gas followed by ethane. Both CO2 and H2O are almost immobile. The increase in temperature in the range from 300 to 450 K does not appear to have any significant impact on the behavior of the molecules inside the pore. The adsorption energies show that both CO2 and H2O have stronger interactions with calcite [104] surface than shale gas molecules.
机译:使用分子动力学模拟技术研究了CO2和H2O对方解石中限制的页岩气体行为的影响。该研究与增强天然气回收(EGR)技术的进步有关,需要深入的原子理解碳氢化合物,水,二氧化碳和其他纳米孔内纳米孔内的压裂流体成分。我们正在考虑二氧化碳(CO2),因为它是增强气体回收的有吸引力的置换剂,并且具有“异国情调”的压裂液。水(H2O)被认为是水基压裂液的主要成分。计算狭窄物种的结构和动态特性。结果表明,纳米孔中CO 2和H 2 O的存在急剧影响页岩气的行为。通过CO 2和H 2 O分子将孔壁上靠近孔壁紧密包装的页岩气分子。在孔壁附近形成了新的二氧化碳和水层。进一步的研究表明,二氧化碳分子在表面附近平坦使它们平坦地对齐,而H2O分子具有与指向壁向壁的水分子的氧原子的定向取向。甲烷,乙烷,二氧化碳和水的预测的横向(面内)自扩散系数值表明孔隙内的复杂动态。该研究表明,甲烷气体随后是乙烷的最快动态。二氧化碳和H2O几乎是不可动的。从300至450k的温度的增加似乎没有对孔隙内分子的行为产生任何显着影响。吸附能量表明,二氧化碳和H 2 O与岩石气体分子的方解石表面具有较强的相互作用。

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