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Published **1965**
by s.n.] in [New York .

Written in English

- Dislocations in crystals.

**Edition Notes**

Statement | Werner F. Hartl. |

Classifications | |
---|---|

LC Classifications | QD921 .H34 |

The Physical Object | |

Pagination | 97 leaves : |

Number of Pages | 97 |

ID Numbers | |

Open Library | OL4297574M |

LC Control Number | 78325910 |

The dynamics of an edge dislocation in a two-dimensional crystal model are investigated using a localized unstable normal mode of vibration of the model. The model used is a simple-cubic lattice with linear central and noncentral nearest-neighbor interactions and a piecewise linear restoring force between atoms on the slip plane. The atoms below the slip plane are by: 6. The modeling of the discrete dislocation behaviour at the mesoscopic level in two dimensions dates back to the late s,. In the early s, the interest in simulating curved dislocations in three dimensions [4], [5] increased, as these simulations have the potential of making quantitative rather than just qualitative by: We develop a long-time moving window framework using Molecular Dynamics (MD) to model shock wave propagation through a one-dimensional chain of atoms.. Modeling beam bending using two-dimensional dislocation dynamics: (1) dislocation population and (2) grid distortion (Cleveringa et al., ). Further illustration of the results of dislocation dynamics simulations carried out by van der Giessen et al. are provided in Figs. and

The Read–Shockley model also explains why the dislocation velocities in the x direction relative to the crystal nearly canceled the local extrusion velocity of the crystal. In this way, the x spacing between neighboring dislocations was maintained at the value s required by the model. Three‐dimensional dislocation model for great earthquakes of the Cascadia Subduction Zone. elastic dislocation modeling of interseismic deformation geodetic data. In this study, a general 3‐D dislocation model for thrust faults has been developed that accommodates curved fault geometry and nonuniform interseismic locking or coseismic. As in previous dislocation dynamics models 4,5,6,7, we consider a two-dimensional cross-section of the crystal (that is, the xy plane), and randomly place N straight-edge dislocations gliding. Dislocation motion and interactions are at the core of all deformation and failure mechanisms in ductile metallic systems. As has been discussed throughout the chapters of this book, much of the study of nanograined metals has emphasized the effects of limited grain volume on the hindrance or absence of classical dislocation mechanisms and processes.

l are dislocation Burgers vector and line direction, respectively. The unit vector n is the glide plane normal, i.e. n||l×b, and unit vector t is parallel to l ×n. Both dislocation velocity v and driving force f are 2-dimensional vectors in the tangent (shaded) plane spanned by n and t (see text). node i with two neighbors, 0 and 1. We can. GPS velocity observations from the Kenai Peninsula and Kodiak Island, Alaska, display a pattern of spatial variability suggesting the presence of multiple active processes on the underlying Pacific—N. It pointed out the unsuitability of two dimensional discrete dislocation plasticity to treat high strain rate processes and introduced a new formulation termed dynamic discrete dislocation. [1] CAS3D‐2, a new three‐dimensional (3‐D) dislocation model, is developed to model interseismic deformation rates at the Cascadia subduction zone. The model is considered a snapshot description of the deformation field that changes with time. The effect of northward secular motion of the central and southern Cascadia forearc sliver is subtracted to obtain the effective convergence.

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