Molecular Insight into the Methane Occurrence inside a Shale Nanochannel with Formation Water

Abstract

The occurrence status of shale gas inside a nanochannel of a shale reservoir is crucial for shale gas reserve assessment and exploitation. In this work, adopting molecular dynamics simulations, the methane occurrence inside a shale nanochannel was investigated under different formation water saturations. Moreover, employing three common inorganic minerals including of quartz, calcite, and kaolinite, the influence of mineral hydrophilicity on methane occurrence was also examined. The simulations indicate that there are three occurrence statuses of methane inside nanochannels including a free status located in the internal nanochannel, an adsorption status on mineral and water film surfaces, and a dissolution status inside the water phase. Among them, free-status methane is the dominant contribution to the recoverable reserve assessment and could be feasibly exploited. Without formation water, methane gives two occurrence statuses including an adsorption status on mineral surfaces and a free status. Once the formation water emerges, it will preferentially adsorb onto the mineral surface to form a water film. With the increase of formation water saturation, the proportions of free-status and dissolution-status methanes increase, while the proportion of adsorption-status methane decreases. In three mineral nanochannels with hydrophilicity orders of quartz > calcite > kaolinite, the proportion of adsorption-status methane follows the order of kaolinite > calcite > quartz, and free-status methane gives the order of kaolinite ≈ quartz > calcite. The underlying mechanisms of these occurrence features were discussed at length from the view of microscopic interactions among mineral surfaces, water, and methane. Our work presents the methane occurrence structure inside a shale nanochannel, and the discussion of the three methane occurrence statuses could provide fundamental data and theoretical guidance for shale gas reserve assessment and exploitation.

The role of water bridge on gas adsorption and transportation mechanisms in organic shale

“…Based on the molecular distribution description in Fig. 2 a,b, the water bridge distribution is in line with the observation in previous studies 30 , 31 . The increasing moisture content contributes to a water bridge formation between the shale slit.…”

Molecular Insight into the Occurrence Characteristics of Deep Oil with Associated Gas Methane and the Displacement Resistance in Water Flooding in Nano-Pore Throat

“…The adsorption peaks of methane molecules appear in the region of 1.5-2.4 nm and 6.6-7.5 nm, and the free-state zone of methane molecules is in the region of 2.4-6.6 nm. The adsorption zone of oil and methane is consistent with previous research [20,[45][46][47]. It can be seen from Figure 2f that with the increase in methane content, the density of oil molecules shows a downward trend.…”

Molecular Simulation of Adsorption and Diffusion of Methane and Ethane in Kaolinite Clay under Supercritical Conditions: Effects of Water and Temperature

“…The analysis shows that the presence of water molecules is not conducive to the adsorption of CH 4 and C 2 H 6 . Due to the strong hydrophilicity of the mineral surface, water molecules are preferentially adsorbed on the pore surface of kaolinite to form water molecular layers [40]. With the increase in water content, two or three layers of water molecular layers can be formed, and these water molecular layers occupy the low-energy adsorption sites on the surface of kaolinite.…”