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The fracture density (f) and the rupture value (I) may have a positive correlation, so the rupture value (I) is an effective index for fracture prediction through empirical formulas established between them.
The possibility of rock's failure is very small when the rupture value (I) is far smaller than 1, whereas the possibility is relatively larger when the rupture value (I) exceeds 1.
Rupture value (I) stands for the possibility of rock failure, whereas the strain energy density (U) stands for the developing ability of structural fractures.
In all the tests carried out, the premature debonding of the SS strip was observed at a strain somewhat lower than its rupture value.
Similar to the rupture value, there is obvious positive correlation between the strain energy density and the thickness of sandstone layers.
Besides that, from Fig. 11 it can also be seen that the maximum axial stress in the stainless steel used on the EBR with SS specimens and measured by the strain gauges is quite far away from its rupture value.
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However panels made with 15 mm thickness had higher modulus of rupture values.
The regional stress fields during different periods also influence the rupture values, resulting in the Cenozoic rupture values being smaller than the Late Mesozoic ones.
Porosity, bulk density, water absorption and modulus of rupture values were recorded for each sample.
I and U denote the calculated rupture values and the strain energy densities (104 J/m3), respectively.
Moreover, gels containing sucrose showed the highest stress at rupture values and had lower influence of polymer concentrations.
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