205301 Research on evaluation of dynamic fracture characteristic by ESPI (original) (raw)

2011, The Proceedings of Conference of Kanto Branch

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Estimation of External Forces Using Local Displacement of Elastic Body

If intraoperative measurement and physical estimation of the deformed organs are possible during surgery, the conditions of organs will be recognized physically and quantitatively, which will make the recent surgery more safe and reliable. This study proposes a new method for estimating external forces based on local displacement observation of elastic bodies. By our method, we can estimate the magnitude and position of forces not only on the forceps but also in invisible field. Some simulation studies are planned to confirm the effectiveness of the method. The experiments showed that the external forces are successfully estimated by partial observation of the deformed shape.

Stress Strain Curve Prediction of Single Crystal Using Sachs Deformation Texture Model Combined with Dislocation Theory

Journal of the Japan Society for Technology of Plasticity, 2014

Combining the Sachs deformation model with the dislocation theory, we can predict the stress-strain curve for both face centered cubic (FCC) and body centered cubic (BCC) single crystals generally. Residual dislocation densities are estimated from total amount of microscopic slip, considering cross-slipped dislocations and sessile dislocations. Stresses are calculated from estimated dislocation densities using the Bailey-Hirsch relationship. Finally, we showed a calculation example of the Sachs deformation model to explain low-angle boundary formation.

Fracture Network Analysis based on the Geologic Model of Channels. Part 2: Analysis of the Tracer Migration Test carried out in the Kamaishi Mine, Japan

Journal of the Japan Society of Engineering Geology

A tracer migration test carried out around the KD-90 drift in the Kamaishi Mine, Japan was analyzed using the computer code "Don-Chan". Geological structure developing in the rock mass near this drift was carefully studied for making a 3-D channel network model. It was found that two major fracture sets are developing in the rock mass and that the lineations observed on the fracture planes mainly develope in the perpendicular direction to the intersection line between these fracture sets. Those nature of the fracture system implies that these fractures sets were initially formed as the conjugate sets and the stress conditions acting on the rock mass have not so much changed. A channel network was constructed on the basis of those features of the fracture system. The tracer migration was fairly well analyzed by the "Don-Chan" code. The applicability of this code was also examined.

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