2019
DOI: 10.3390/en12203932
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The Effect of Hydration on Pores of Shale Oil Reservoirs in the Third Submember of the Triassic Chang 7 Member in Southern Ordos Basin

Abstract: Shale oil is an unconventional kind of oil and gas resource with great potential. China has huge reserves of shale oil, and shale oil resources are abundant in the third submember of the Triassic Chang 7 member in the southern Ordos Basin. At present, this area is in the initial stage of shale oil exploration and development. The reservoir pore is one of the key factors affecting oil accumulation, drilling safety, and oil production. It is also an important reservoir parameter that must be defined in the explo… Show more

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Cited by 6 publications
(2 citation statements)
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“…The hydration reaction will lead to the increase of porosity, the looseness of internal structure, and the decrease of rock strength. Shale has obvious bedding structure, and microcracks are usually developed along the bedding, which provides a good channel for hydration [13]. The expansion stress produced by hydration will concentrate on the crack tip, which will cause fracture expansion and deformation and cause damage to the rock interior, such as borehole instability [14].…”
Section: Introductionmentioning
confidence: 99%
“…The hydration reaction will lead to the increase of porosity, the looseness of internal structure, and the decrease of rock strength. Shale has obvious bedding structure, and microcracks are usually developed along the bedding, which provides a good channel for hydration [13]. The expansion stress produced by hydration will concentrate on the crack tip, which will cause fracture expansion and deformation and cause damage to the rock interior, such as borehole instability [14].…”
Section: Introductionmentioning
confidence: 99%
“…This rule is similar to the result of bedding shale obtained in the literature [32], but the difference is that lamellar shale shows more significant change under the effect of hydration. This may be due to the fact that the inclusion of lamellar structures, which contain a lot of clay minerals, would have more significant swelling deformation after hydration compared with bedding shale [36]. Thus, the increase in rock particle spacing is more obvious, leading to the reduction in elastic brittleness and increase in plasticity and ductility [37].…”
Section: Influence Of Hydration On Mechanical Properties Of Lamellar Shalementioning
confidence: 99%