Equivalent Biot and Skempton Poroelastic Coefficients for a Fractured Rock Mass from a DFN Approach.
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| Title: | Equivalent Biot and Skempton Poroelastic Coefficients for a Fractured Rock Mass from a DFN Approach. |
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| Authors: | De Simone, Silvia1,2 (AUTHOR) silvia.desimone@idaea.csic.es, Darcel, Caroline3 (AUTHOR), Kasani, Hossein A.4 (AUTHOR), Mas Ivars, Diego5,6 (AUTHOR), Davy, Philippe1 (AUTHOR) |
| Source: | Rock Mechanics & Rock Engineering. Dec2023, Vol. 56 Issue 12, p8907-8925. 19p. |
| Subjects: | Mass transfer coefficients, Poroelasticity, Strains & stresses (Mechanics), Rock deformation, Rock properties, Stress fractures (Orthopedics) |
| Abstract: | A quantitative and analytical approach is adopted to estimate two important parameters for coupled hydro-mechanical analysis at the scale of a fractured rock mass, namely the equivalent Biot effective stress coefficient α ¯ and Skempton pore pressure coefficient B ¯ . We derive formal expressions that estimate the two equivalent poroelastic coefficients from the properties of both the porous intact rock and the discrete fracture network, which includes fractures with different orientation, size, and mechanical properties. The coefficients are equivalent in the sense that they allow effectively predicting the volumetric deformation of the fluid-saturated fractured rock under an applied load in drained and undrained conditions. The formal expressions are validated against results from fully coupled hydro-mechanical simulations on systems with explicit representation of deformable fractures and rock blocks. We find that the coefficients are highly anisotropic as they largely vary with fracture orientations with respect to the applied stress tensor. For a given set of fracture and rock properties, B ¯ increases with the ratio of normal to average stress undergone by the fractures, while the opposite occurs for α ¯ . Additionally, both α ¯ and B ¯ increase with fracture density, which directly impacts the deformation caused by a load in undrained conditions. Because the effective stress variation is proportional to the applied load by 1 - α ¯ B ¯ , a factor that partly compensates for the decrease in equivalent rock stiffness caused by the fractures, a fully saturated fractured rock may deform less than an intact rock in undrained conditions, while the opposite occurs in dry conditions. Highlights: Equivalent Biot and Skempton coefficients for a fractured rock mass are estimated as the ones that define the bulk volumetric deformation. The coefficients depend on the orientations of the fractures and the applied load. Densely fractured rocks are characterized by larger equivalent coefficients than intact rocks Disregarding the presence of fractures may incur an incorrect evaluation of the hydro-mechanical response [ABSTRACT FROM AUTHOR] |
| Copyright of Rock Mechanics & Rock Engineering is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
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| Items | – Name: Title Label: Title Group: Ti Data: Equivalent Biot and Skempton Poroelastic Coefficients for a Fractured Rock Mass from a DFN Approach. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22De+Simone%2C+Silvia%22">De Simone, Silvia</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<i> silvia.desimone@idaea.csic.es</i><br /><searchLink fieldCode="AR" term="%22Darcel%2C+Caroline%22">Darcel, Caroline</searchLink><relatesTo>3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Kasani%2C+Hossein+A%2E%22">Kasani, Hossein A.</searchLink><relatesTo>4</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Mas+Ivars%2C+Diego%22">Mas Ivars, Diego</searchLink><relatesTo>5,6</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Davy%2C+Philippe%22">Davy, Philippe</searchLink><relatesTo>1</relatesTo> (AUTHOR) – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Rock+Mechanics+%26+Rock+Engineering%22">Rock Mechanics & Rock Engineering</searchLink>. Dec2023, Vol. 56 Issue 12, p8907-8925. 19p. – Name: Subject Label: Subjects Group: Su Data: <searchLink fieldCode="DE" term="%22Mass+transfer+coefficients%22">Mass transfer coefficients</searchLink><br /><searchLink fieldCode="DE" term="%22Poroelasticity%22">Poroelasticity</searchLink><br /><searchLink fieldCode="DE" term="%22Strains+%26+stresses+%28Mechanics%29%22">Strains & stresses (Mechanics)</searchLink><br /><searchLink fieldCode="DE" term="%22Rock+deformation%22">Rock deformation</searchLink><br /><searchLink fieldCode="DE" term="%22Rock+properties%22">Rock properties</searchLink><br /><searchLink fieldCode="DE" term="%22Stress+fractures+%28Orthopedics%29%22">Stress fractures (Orthopedics)</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: A quantitative and analytical approach is adopted to estimate two important parameters for coupled hydro-mechanical analysis at the scale of a fractured rock mass, namely the equivalent Biot effective stress coefficient α ¯ and Skempton pore pressure coefficient B ¯ . We derive formal expressions that estimate the two equivalent poroelastic coefficients from the properties of both the porous intact rock and the discrete fracture network, which includes fractures with different orientation, size, and mechanical properties. The coefficients are equivalent in the sense that they allow effectively predicting the volumetric deformation of the fluid-saturated fractured rock under an applied load in drained and undrained conditions. The formal expressions are validated against results from fully coupled hydro-mechanical simulations on systems with explicit representation of deformable fractures and rock blocks. We find that the coefficients are highly anisotropic as they largely vary with fracture orientations with respect to the applied stress tensor. For a given set of fracture and rock properties, B ¯ increases with the ratio of normal to average stress undergone by the fractures, while the opposite occurs for α ¯ . Additionally, both α ¯ and B ¯ increase with fracture density, which directly impacts the deformation caused by a load in undrained conditions. Because the effective stress variation is proportional to the applied load by 1 - α ¯ B ¯ , a factor that partly compensates for the decrease in equivalent rock stiffness caused by the fractures, a fully saturated fractured rock may deform less than an intact rock in undrained conditions, while the opposite occurs in dry conditions. Highlights: Equivalent Biot and Skempton coefficients for a fractured rock mass are estimated as the ones that define the bulk volumetric deformation. The coefficients depend on the orientations of the fractures and the applied load. Densely fractured rocks are characterized by larger equivalent coefficients than intact rocks Disregarding the presence of fractures may incur an incorrect evaluation of the hydro-mechanical response [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Rock Mechanics & Rock Engineering is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1007/s00603-023-03515-9 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 19 StartPage: 8907 Subjects: – SubjectFull: Mass transfer coefficients Type: general – SubjectFull: Poroelasticity Type: general – SubjectFull: Strains & stresses (Mechanics) Type: general – SubjectFull: Rock deformation Type: general – SubjectFull: Rock properties Type: general – SubjectFull: Stress fractures (Orthopedics) Type: general Titles: – TitleFull: Equivalent Biot and Skempton Poroelastic Coefficients for a Fractured Rock Mass from a DFN Approach. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: De Simone, Silvia – PersonEntity: Name: NameFull: Darcel, Caroline – PersonEntity: Name: NameFull: Kasani, Hossein A. – PersonEntity: Name: NameFull: Mas Ivars, Diego – PersonEntity: Name: NameFull: Davy, Philippe IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 12 Text: Dec2023 Type: published Y: 2023 Identifiers: – Type: issn-print Value: 07232632 Numbering: – Type: volume Value: 56 – Type: issue Value: 12 Titles: – TitleFull: Rock Mechanics & Rock Engineering Type: main |
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