Combined Scaling of Fluid Flow and Seismic Stiffness in Single Fractures

The connection between fluid flow and seismic stiffness in single fractures is governed by the geometry of the fracture through the size and spatial distributions of the void and contact areas. Flow and stiffness each exhibit scaling behavior as the scale of observation shifts from local to global s...

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Published in:Rock mechanics and rock engineering Vol. 47; no. 5; pp. 1613 - 1623
Main Authors: Petrovitch, C. L., Pyrak-Nolte, L. J., Nolte, D. D.
Format: Journal Article Conference Proceeding
Language:English
Published: Vienna Springer Vienna 01-09-2014
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Springer Nature B.V
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Abstract The connection between fluid flow and seismic stiffness in single fractures is governed by the geometry of the fracture through the size and spatial distributions of the void and contact areas. Flow and stiffness each exhibit scaling behavior as the scale of observation shifts from local to global sample sizes. The purpose of this study was to explore the joint scaling of both properties using numerical models. Finite-size scaling methods are used to extract critical thresholds and power laws for fluid flow through weakly correlated fractures under increasing load. An important element in the numerical fracture deformation is the use of extended boundary conditions that simulate differences between laboratory cores relative to in situ field studies. The simulated field conditions enable joint scaling of flow and stiffness to emerge with the potential to extrapolate from small laboratory samples to behavior on the field scale.
AbstractList The connection between fluid flow and seismic stiffness in single fractures is governed by the geometry of the fracture through the size and spatial distributions of the void and contact areas. Flow and stiffness each exhibit scaling behavior as the scale of observation shifts from local to global sample sizes. The purpose of this study was to explore the joint scaling of both properties using numerical models. Finite-size scaling methods are used to extract critical thresholds and power laws for fluid flow through weakly correlated fractures under increasing load. An important element in the numerical fracture deformation is the use of extended boundary conditions that simulate differences between laboratory cores relative to in situ field studies. The simulated field conditions enable joint scaling of flow and stiffness to emerge with the potential to extrapolate from small laboratory samples to behavior on the field scale.
Issue Title: Special Issue: Including Selected Papers from the 47th US Rock Mechanics/Geomechanics Symposium, San Francisco, June 23-26, 2013 The connection between fluid flow and seismic stiffness in single fractures is governed by the geometry of the fracture through the size and spatial distributions of the void and contact areas. Flow and stiffness each exhibit scaling behavior as the scale of observation shifts from local to global sample sizes. The purpose of this study was to explore the joint scaling of both properties using numerical models. Finite-size scaling methods are used to extract critical thresholds and power laws for fluid flow through weakly correlated fractures under increasing load. An important element in the numerical fracture deformation is the use of extended boundary conditions that simulate differences between laboratory cores relative to in situ field studies. The simulated field conditions enable joint scaling of flow and stiffness to emerge with the potential to extrapolate from small laboratory samples to behavior on the field scale.[PUBLICATION ABSTRACT]
Author Pyrak-Nolte, L. J.
Petrovitch, C. L.
Nolte, D. D.
Author_xml – sequence: 1
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  surname: Petrovitch
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  givenname: L. J.
  surname: Pyrak-Nolte
  fullname: Pyrak-Nolte, L. J.
  organization: Department of Physics, Purdue University, School of Civil Engineering, Purdue University, Department of Earth, Atmospheric and Planetary Sciences, Purdue University
– sequence: 3
  givenname: D. D.
  surname: Nolte
  fullname: Nolte, D. D.
  organization: Department of Physics, Purdue University
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Issue 5
Keywords Scaling
Fracture deformation
Fracture
Rock fractures
Hydromechanical scaling
Finite size effect
Deformation
Rock mechanics
Fracture mechanics
Mechanical properties
Modeling
Flow(fluid)
Hydromechanics
Jointed rock
Stiffness
Coupling
Hydraulic properties
Language English
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Snippet The connection between fluid flow and seismic stiffness in single fractures is governed by the geometry of the fracture through the size and spatial...
Issue Title: Special Issue: Including Selected Papers from the 47th US Rock Mechanics/Geomechanics Symposium, San Francisco, June 23-26, 2013 The connection...
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SubjectTerms Applied sciences
Boundary conditions
Buildings. Public works
Civil Engineering
Computation methods. Tables. Charts
Computational fluid dynamics
Computer simulation
Earth and Environmental Science
Earth Sciences
Exact sciences and technology
Fluid dynamics
Fluid flow
Fluids
Fracture mechanics
Fracture zones
Geophysics/Geodesy
Geotechnics
Mathematical models
Original Paper
Rock
Rock mechanics
Rocks
Seismology
Soil mechanics. Rocks mechanics
Spatial distribution
Stiffness
Structural analysis. Stresses
Water effect, drainage, ground water lowering, filtration
Title Combined Scaling of Fluid Flow and Seismic Stiffness in Single Fractures
URI https://link.springer.com/article/10.1007/s00603-014-0591-z
https://www.proquest.com/docview/1556936749
https://search.proquest.com/docview/1620109983
Volume 47
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