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It comes after Welsh 15-year-olds were found to be slipping down the international Programme for International Student Assessment (Pisa) league table.
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Also, using poro-elastic formulations, in-situ stress regime was found to be strike-slip (i.e. SH>Sv>Sh).
During rolling the deformation mechanisms were found to be dislocation slip, mechanical twinning, deformation-induced ε-martensite transformation and shear banding.
Crack growth was predominantly found to be either growth on slip planes in a shearing mode, or linking after formation of microcracks ahead of the main crack, which do not require detectable crack opening.
Interestingly this procedure was found to be also successful in predicting slip evolution at higher loads, because of slip localization in the superalloy tested.
Except for one example of basal slip, all slips were found to be on pyramidal planes.
In general, the particle-interaction effects are found to be more significant when the slip coefficients at the particle surfaces become smaller.
The JIS A 1454 test method was found to be a better test of slip resistance than EN 13893 and ASTM D 2047.
Because the density of 〈111〉 superdislocations is found to be very low after the slip transition, glide decomposition of 〈111〉 superdislocations is believed to the primary source mechanism for 〈100〉 dislocations.
The amount of afterslip is found to be proportional to the seismic slip of the asperity, in agreement with observations.
Coulomb stress changes for normal-fault aftershocks near the Japan Trench are found to be strongly dependent on the slip on the shallow portion of the fault.
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