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Effect of dislocation slip on in-situ tensile fracture of vanadium alloys after helium/self-ion irradiation. [PDF]

open access: yesSci Technol Adv Mater
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In-situ stress diagnostics

Surface and Coatings Technology, 2001
Stress is a common property of thin films. After a brief summary of origins and effects of stresses in thin films the particular situation in amorphous and nanocrystalline films is discussed. The problems related to the extremely high compressive stresses in cubic boron nitride (cBN) have been tackled either by the deposition of buffer layers or by ...
Fukarek, W., Fitz, C.
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In-situ calibration of stress chips

40th Conference Proceedings on Electronic Components and Technology, 1990
A novel procedure employing moire interferometry has been successfully implemented for the accurate in-situ calibration of stress chips. Strains were measured by this accurate and extremely sensitive technique at the locations of the gauges and related to corresponding gauge-resistance changes.
A.F. Bastawros, A.S. Voloshin
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Estimating in situ Stresses

1997
Before measuring virgin stresses with some of the methods discussed in the following chapters, an attempt should be made to obtain an estimate of the in situ stress field. This can be done, for instance, from stress versus depth relationships or observations obtained from stress measurements made in the past in the region of interest or by ...
Bernard Amadei, Ove Stephansson
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In-situ Stresses

1990
The state of stress existing in the rock mass prior to any construction work is referred to as the in-situ or primary state of stress. A knowledge of this state is important to the planning and construction of engineering structures in rock. Chapters 11, 12 and 13 in particular demonstrated the considerable influence exercised by the in-situ state of ...
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Stress-states in situ

1989
The undisturbed in situ rock before an excavation is already under a certain stress. This stress-state is due to a variety of causes: gravity, stresses due to tectonic motions, the strata orientation, the creep and relaxation produced during geological periods, possible local unloading due to a relatively fast erosion, thermal contractions, etc.
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