Nanoscale mechanical property variations concerning mineral composition and contact of marine shale

被引:57
作者
Li, Yong [1 ]
Chen, Jianqi [1 ]
Elsworth, Derek [2 ,3 ]
Pan, Zhejun [4 ]
Ma, Xiaotian [1 ]
机构
[1] China Univ Min & Technol, Coll Geosci & Surveying Engn, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China
[2] Penn State Univ, EMS Energy Inst, Dept Energy & Mineral Engn, University Pk, PA 16802 USA
[3] Penn State Univ, G3 Ctr, University Pk, PA 16802 USA
[4] Northeast Petr Univ, Key Lab Continental Shale Hydrocarbon Accumulat &, Minist Educ, Daqing 163318, Heilongjiang, Peoples R China
关键词
Shale oil and gas; Shale lithofacies; Mineral composition; Multiscale mechanical property; Nanoscale mechanics; Finite-element simulation; SILURIAN LONGMAXI FORMATION; EASTERN SICHUAN BASIN; ELASTIC PROPERTIES; ACOUSTIC-EMISSION; ROCK; GAS; PROPAGATION; PARAMETERS; INVERSION; WELL;
D O I
10.1016/j.gsf.2022.101405
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Mechanical properties of shales are key parameters influencing hydrocarbon production ??? impacting borehole stability, hydraulic fracture extension and microscale variations in in situ stress. We use Ordovician shale (Sichuan Basin, China) as a type-example to characterize variations in mineral particle properties at microscale including particle morphology, form of contact and spatial distribution via mineral liberation analysis (MLA) and scanning electron microscopy (SEM). Deformation-based constitutive models are then built using finite element methods to define the impact of various architectures of fracture and mineral distributions at nanometer scale on the deformation characteristics at macroscale. Relative compositions of siliceous, calcareous and clay mineral particles are shown to be the key factors influencing brittleness. Shales with similar mineral composition show a spectrum of equivalent medium mechanical properties due to differing particle morphology and mineral heterogeneity. The predominance of small particles and/or point-point contacts are conducive to brittle failure, in general, and especially so when quartz-rich. Fracture morphology, length and extent of filling all influence shale deformability. High aspect-ratio fractures concentrate stress at fracture tips and are conducive to extension, as when part-filled by carbonate minerals. As fracture spacing increases, stress transfer between adjacent fractures weakens, stress concentrations are amplified and fracture extension is favored. The higher the fractal dimension of the fracture and heterogeneity of the host the more pervasive the fractures. Moreover, when fractures extend, their potential for intersection and interconnection contributes to a reduction in strength and the promotion of brittle failure. Thus, these results provide important theoretical insights into the role of heterogeneity on the deformability and strength of shale reservoirs with practical implications for their stimulation and in the recovery of hydrocarbons from them. ?? 2022 China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/ licenses/by-nc-nd/4.0/).
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页数:16
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