David A Lockner
David Lockner is a geophysicist in the Earthquake Science Center.
Science and Products
Filter Total Items: 115
A test of the double-shearing model of flow for granular materials A test of the double-shearing model of flow for granular materials
The double-shearing model of flow attributes plastic deformation in granular materials to cooperative slip on conjugate Coulomb shears (surfaces upon which the Coulomb yield condition is satisfied). The strict formulation of the double-shearing model then requires that the slip lines in the material coincide with the Coulomb shears. Three different experiments that approximate simple...
Authors
J.C. Savage, D.A. Lockner
Strengths of serpentinite gouges at elevated temperatures Strengths of serpentinite gouges at elevated temperatures
Serpentinite has been proposed as a cause of both low strength and aseismic creep of fault zones. To test these hypotheses, we have measured the strength of chrysotile-, lizardite-, and antigorite-rich serpentinite gouges under hydrothermal conditions, with emphasis on chrysotile, which has thus far received little attention. At 25°C, the coefficient of friction, μ, of chrysotile gouge...
Authors
Diane E. Moore, D.A. Lockner, S. Ma, R. Summers, J.D. Byerlee
Physical modeling of the formation and evolution of seismically active fault zones Physical modeling of the formation and evolution of seismically active fault zones
Acoustic emission (AE) in rocks is studied as a model of natural seismicity. A special technique for rock loading has been used to help study the processes that control the development of AE during brittle deformation. This technique allows us to extend to hours fault growth which would normally occur very rapidly. In this way, the period of most intense interaction of acoustic events...
Authors
A.V. Ponomarev, A.D. Zavyalov, V.B. Smirnov, D.A. Lockner
Permeability and porosity of the Illinois UPH 3 drillhole granite and a comparison with other deep drillhole rocks Permeability and porosity of the Illinois UPH 3 drillhole granite and a comparison with other deep drillhole rocks
Permeability, porosity, and volumetric strain measurements were conducted on granite cores obtained at depths of 0.7 to 1.6 km from the Illinois UPH 3 drillhole at effective confining pressures from 5 to 100 MPa. Initial permeabilities were in the range of 10-17 to 10-19 m2 and dropped rapidly with applied pressure to values between 10-20 and 10-24 m2 at 100 MPa, typical of other deep...
Authors
C.A. Morrow, D.A. Lockner
Sample characterizations and strength measurements of serpentinite gouges Sample characterizations and strength measurements of serpentinite gouges
No abstract available.
Authors
Diane E. Moore, D.A. Lockner, R. Summers, J.D. Byerlee
Is internal friction friction? Is internal friction friction?
Mogi [1974] proposed a simple model of the incipient rupture surface to explain the Coulomb failure criterion. We show here that this model can plausibly be extended to explain the Mohr failure criterion. In Mogi's model the incipient rupture surface immediately before fracture consists of areas across which material integrity is maintained (intact areas) and areas across which it is not...
Authors
J.C. Savage, J.D. Byerlee, D.A. Lockner
Filter Total Items: 14
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Science and Products
Filter Total Items: 115
A test of the double-shearing model of flow for granular materials A test of the double-shearing model of flow for granular materials
The double-shearing model of flow attributes plastic deformation in granular materials to cooperative slip on conjugate Coulomb shears (surfaces upon which the Coulomb yield condition is satisfied). The strict formulation of the double-shearing model then requires that the slip lines in the material coincide with the Coulomb shears. Three different experiments that approximate simple...
Authors
J.C. Savage, D.A. Lockner
Strengths of serpentinite gouges at elevated temperatures Strengths of serpentinite gouges at elevated temperatures
Serpentinite has been proposed as a cause of both low strength and aseismic creep of fault zones. To test these hypotheses, we have measured the strength of chrysotile-, lizardite-, and antigorite-rich serpentinite gouges under hydrothermal conditions, with emphasis on chrysotile, which has thus far received little attention. At 25°C, the coefficient of friction, μ, of chrysotile gouge...
Authors
Diane E. Moore, D.A. Lockner, S. Ma, R. Summers, J.D. Byerlee
Physical modeling of the formation and evolution of seismically active fault zones Physical modeling of the formation and evolution of seismically active fault zones
Acoustic emission (AE) in rocks is studied as a model of natural seismicity. A special technique for rock loading has been used to help study the processes that control the development of AE during brittle deformation. This technique allows us to extend to hours fault growth which would normally occur very rapidly. In this way, the period of most intense interaction of acoustic events...
Authors
A.V. Ponomarev, A.D. Zavyalov, V.B. Smirnov, D.A. Lockner
Permeability and porosity of the Illinois UPH 3 drillhole granite and a comparison with other deep drillhole rocks Permeability and porosity of the Illinois UPH 3 drillhole granite and a comparison with other deep drillhole rocks
Permeability, porosity, and volumetric strain measurements were conducted on granite cores obtained at depths of 0.7 to 1.6 km from the Illinois UPH 3 drillhole at effective confining pressures from 5 to 100 MPa. Initial permeabilities were in the range of 10-17 to 10-19 m2 and dropped rapidly with applied pressure to values between 10-20 and 10-24 m2 at 100 MPa, typical of other deep...
Authors
C.A. Morrow, D.A. Lockner
Sample characterizations and strength measurements of serpentinite gouges Sample characterizations and strength measurements of serpentinite gouges
No abstract available.
Authors
Diane E. Moore, D.A. Lockner, R. Summers, J.D. Byerlee
Is internal friction friction? Is internal friction friction?
Mogi [1974] proposed a simple model of the incipient rupture surface to explain the Coulomb failure criterion. We show here that this model can plausibly be extended to explain the Mohr failure criterion. In Mogi's model the incipient rupture surface immediately before fracture consists of areas across which material integrity is maintained (intact areas) and areas across which it is not...
Authors
J.C. Savage, J.D. Byerlee, D.A. Lockner
Filter Total Items: 14
No Result Found