2023
DOI: 10.1016/j.jgsce.2023.205051
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Permeability damage and hydrate dissociation barrier caused by invaded fracturing fluid during hydrate reservoir stimulation

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Cited by 7 publications
(3 citation statements)
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“…Changes in cyclic stress can cause deformation of granular shale structures; especially, the opening and closing of pores and fractures under cyclic stress can lead to changes in shale seepage characteristics. The permeability damage rate and irreversible permeability damage rate are commonly used in the oil and gas industry to characterize the permeability change of natural gas reservoirs, and the formulas are as follows 40,41 :…”
Section: Results and Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…Changes in cyclic stress can cause deformation of granular shale structures; especially, the opening and closing of pores and fractures under cyclic stress can lead to changes in shale seepage characteristics. The permeability damage rate and irreversible permeability damage rate are commonly used in the oil and gas industry to characterize the permeability change of natural gas reservoirs, and the formulas are as follows 40,41 :…”
Section: Results and Analysismentioning
confidence: 99%
“…Changes in cyclic stress can cause deformation of granular shale structures; especially, the opening and closing of pores and fractures under cyclic stress can lead to changes in shale seepage characteristics. The permeability damage rate and irreversible permeability damage rate are commonly used in the oil and gas industry to characterize the permeability change of natural gas reservoirs, and the formulas are as follows , : D normalK 1 = k 1 k min k 1 where D K1 is the maximum value of the permeability damage during the process of increasing the stress to the highest point; k 1 indicates the permeability of the shale samples corresponding to the first stress point, mD; and k ′ min is the minimum value of the permeability of the shale samples after reaching the maximum effective stress value, mD. D normalK 2 = k 1 k 1 normalr k 1 × 100 % where D K2 represents the permeability damage rate after the stress is restored to the first stress point and k 1r is the permeability of the shale samples after the stress is restored to the first stress point, mD.…”
Section: Results and Analysismentioning
confidence: 99%
“…Clathrate hydrates, commonly referred to as gas hydrates, are nonstoichiometric crystalline inclusion compounds characterized by a structure that resembles powdered ice. , These hydrates consist of polyhedral cages formed by hydrogen-bonded water molecules, which can accommodate gas molecules or small chemical compounds as “guest” molecules . The nature and composition of the guest molecules encased in the hydrate lattice result in the presence of three distinct structures: structure I (sI), structure II (sII), and structure H (sH), each with different types of cages, each with different cages .…”
Section: Introductionmentioning
confidence: 99%