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Erschienen in: Rock Mechanics and Rock Engineering 8/2023

10.05.2023 | Original Paper

Geomechanical Properties of Thinly Interbedded Rocks Based on Micro- and Macro-Scale Measurements

verfasst von: Richao Cong, Ruiyue Yang, Gensheng Li, Zhongwei Huang, Yanjin Gong, Meiyang Jing, Meiquan Lu

Erschienen in: Rock Mechanics and Rock Engineering | Ausgabe 8/2023

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Abstract

Clarifying the geomechanical properties and inherent heterogeneity of layered rocks is essential for predicting fracture morphology and designing hydraulic fracturing pumping schemes. Grid nanoindentation combined with high-resolution scanning electron microscopy and energy-dispersive spectroscopy (SEM–EDS) techniques were used to investigate mechanical differences between the sandstone layer and the mudstone layer for the downhole thinly interbedded core rocks (layered core rocks). Subsequently, the indent impressions and mechanical responses of individual minerals and multiple minerals were quantified. On this basis, the bulk mechanical properties and failure modes of the layered core rocks are investigated under confining pressures. Results indicate that quartz exhibits the highest hardness and Young’s modulus with the smallest indent impression, whereas kaolinite exhibits the opposite in each layer. When the indenter covers multiple minerals simultaneously, the mechanical responses of which are determined by the softer phases. Moreover, minerals exhibit diverse deformations and cracking patterns in different layers. Quartz shows elastic-dominated deformation in the sandstone layer, whereas medium-plastic deformation in the mudstone layer. Since the unstable sheet structures, kaolinite exhibits plastic-dominated deformation in each layer. Shear cracks and radical cracks are prone to occur in elastic-dominated minerals, while chipping damage is induced in plastic-dominated minerals. In addition, the failures of the layered core rocks tend to create along the mudstone layer since the lower mechanical properties. With the increasing of confining pressure, the compressive strength of layered core rocks gradually grows and the failure changes from tensile splitting to tensile–shear mixed failure mode and shear failure mode. The key findings of this paper can provide reliable input data for multiscale geomechanical modeling in understanding proppant embedment mechanisms and designing hydraulic fracturing treatments in coal measure strata.

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Literatur
Zurück zum Zitat Wang Y, Xu S, Hao F, Zhang B, Shu Z, Gou Q, Lu Y, Cong F (2020) Multiscale petrographic heterogeneity and their implications for the nanoporous system of the Wufeng–Longmaxi shales in Jiaoshiba area, Southeast China: response to depositional-diagenetic process. GSA Bull 132:1704–1721. https://doi.org/10.1130/B35324.1CrossRef Wang Y, Xu S, Hao F, Zhang B, Shu Z, Gou Q, Lu Y, Cong F (2020) Multiscale petrographic heterogeneity and their implications for the nanoporous system of the Wufeng–Longmaxi shales in Jiaoshiba area, Southeast China: response to depositional-diagenetic process. GSA Bull 132:1704–1721. https://​doi.​org/​10.​1130/​B35324.​1CrossRef
Zurück zum Zitat Zhong J, Hu CN, Fan HH, Cai YQ, Chen Q, Chen JY, Meng YN (2019) A new type U-Th-REE-Nb mineralization related to albitite: a case study from the Chachaxiangka deposit in the northeastern Qaidam Basin of China, China. Geology 2:422–438. https://doi.org/10.31035/cg2018133CrossRef Zhong J, Hu CN, Fan HH, Cai YQ, Chen Q, Chen JY, Meng YN (2019) A new type U-Th-REE-Nb mineralization related to albitite: a case study from the Chachaxiangka deposit in the northeastern Qaidam Basin of China, China. Geology 2:422–438. https://​doi.​org/​10.​31035/​cg2018133CrossRef
Metadaten
Titel
Geomechanical Properties of Thinly Interbedded Rocks Based on Micro- and Macro-Scale Measurements
verfasst von
Richao Cong
Ruiyue Yang
Gensheng Li
Zhongwei Huang
Yanjin Gong
Meiyang Jing
Meiquan Lu
Publikationsdatum
10.05.2023
Verlag
Springer Vienna
Erschienen in
Rock Mechanics and Rock Engineering / Ausgabe 8/2023
Print ISSN: 0723-2632
Elektronische ISSN: 1434-453X
DOI
https://doi.org/10.1007/s00603-023-03360-w

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