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As can be seen in Figs. 12 and 13, there was a good agreement between calculated and measured F y before fracture start (up to the maximum on the force-displacement curves) and a fair agreement during the steady state phase with the force maximum; there was a large discrepancy between predicted and measured forces in the last phase where only partly sheared material remained.
The fracture start of the main, primary fracture was localized for each crown.
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A fracture starts to heal at the very moment that it occurs.
However, the positions of these two fracture starting point remain unchanged.
Currently, in China, the study on the position of fracture starting point and fracture propagation of radial well is still at the preliminary stage and the fracture initiation pressure and position of fracture starting point remain unclear.
The permeability increases by four orders of magnitudes and the fracture initiation pressure goes up 34.5%, with no influence on the fracture starting point.
The finding shows that the fracture starts in the electrolyte for the big tube radius after 50 000 h because of the mismatch creep properties between SOFC layers.
The result shows that initiation pressure and distance between well and fracture starting point increases as the length, diameter and azimuth of radial well section rise.
In both cases, the fracture started in the corner between the paddle and the coupling body and propagated around the corner.
Our results indicate that sheet fracture starts through partial delamination of the layers, which results in a change in slope of the stress-strain curve.
This chapter presents an overview of the work of ESIS TC 4. Technical Committee 4 of the European Group on Fracture started with the decision to form an activity in polymers and composites at the ECF conference in Portugal.
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