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Inter turn fault is the second most commonly observed faults in the motors and is considered the most severe.
The predicted frequencies for observed faults in the annulus and sun gears of the gearbox are vividly presented in the experimentally measured frequency spectrum.
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Interpreting this variation between bulk and matrix density in terms of fracture porosity along the seismically observed fault zones, we may suggest fracture porosity in the order of 10%.
While it is true that operators sometimes fail to observe faults or other important signals, a quantitative analysis of monitoring behaviour shows that not even optimal sampling can detect all abnormal events.
We seem to be incredibly myopic when it comes to our own failings and shortcomings, and to be particularly acute in observing faults in others.
After observing fault localization with reduced area overhead, we utilize the self-checking full adder in constructing a self-repairing adder.
From Fig. 5b, the relay R7 8 is observing fault point in Zone-2 instead of Zone-1.
We also discuss the relationship between the fault rupture and observed near-fault ground motions.
The observed stacking faults in the γ matrix form by the dissociation of a/2〈1 1 0〉 matrix dislocations with Burgers vectors perpendicular to the loading direction in the early stages of creep.
If we clearly find that strong motions observed near faults show a misfit to the attenuation relation for any other reason than site amplification, these data should not be used for estimation of the station corrections.
Usually, the aperiodicity observed on faults is larger than this value.
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