
Walter P. Murphy Professor Emeritus
BS, physics, 1948
DSc physics, 1951 Carnegie Institute of Technology (now Carnegie Mellon University)
Our research areas are the mechanical properties
of metals, including fatigue and fracture of metals, the high-temperature
creep of crystalline solids, and dislocation theory applied to these phenomena.
We are developing dislocation-based solutions of the plastic regions around
stressed cracks. These solutions rely on dislocation crack tip shielding
and dislocation crack extension force conditions. In fact, we believe that
complete solutions for crack problems in elastic plastic solids cannot be
obtained, except for the most simple problems, without use of the dislocation
equations. In the area of geophysics, we recently developed a theory for
the migration of subglacial lakes under ice sheets and earthquake dislocations
moving at a transonic velocity on a fault separating rock of sightly different
elastic constants.
In the area of geophysics, our primary research area
is in the theory of the flow of glaciers and ice sheets.
Prof. Weertman has an island
in Antarctica named after him.
Walter P. Murphy Professor Emeritus of Materials Science and Engineering
Member, American Academy of Arts and Sciences, 1997
Seligman Crystal of the International Glaciological Society, 1983
Acta Metallurgica Gold Medal, 1980
Champion H. Mathewson Gold Medal of the Metallurgical Society of AIME for work on creep and fatigue fracture, 1977
Member, National Academy of Engineering, 1976
Guggenheim Fellowship, 1970
Robert E. Horton Award, American Geophysical Union, 1962
Fulbright Fellowship, 1951
Fellow, Geological Society of America, 1970; ASM International, 1972; American Physical Society, 1982; American Geophysical Union, 1982; TMS–AIME, 1990; American Academy of Mechanics
J. Weertman, Asymptotic crack tip stress, rotation pseudo-stress field and dislocation fields for mixed mode I and II cracks in elastic perfectly plastic solids, Mechanics of Materials. 35, pp. 433-452 (2003).
J. Weertman, Relationship between stress-strain potentials and maximum shear and zero shear trajectories for mode III crack, in Electron Microscopy: its Role in Materials Science (The Mike Meshii Symposium), edited by J.R. Weertman, M. Fine, K. Faber, D. Quesnel, W. King and P. Liaw, The Minerals, Metals & Materials Society (TMS), Warrendale, PA, pp. 107-112 (2003).
Subsonic-type earthquake dislocation moving at approximately
21/2 x shear wave velocity on interface between half spaces
of slightly different elastic constants. Geophys. Res. Lett. 29:
art no. 1470 (2002).
Why the stress trajectories in the Dean-Hutchinson plastic sector of the
growing mode III crack are an unfocused fan. J. Mech. Phys. Solids 50:
153-63 (2002).
Anomalous work hardening, non-redundant screw dislocations in a circular bar deformed in torsion, and non-redundant edge dislocations in a bent foil, Acta Materialia 50, pp. 673-689 (2002).
The Comninou-Dundurs Effect and position stability of subglacial lakes, Annals of Glaciology 35, pp. 495-502 (2002).