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- W2482140504 abstract "When X-ray residual stresses are determined taking into account the stress gradients within the penetration depth of X-rays, three assumptions have usually been made; 1) the stress gradient is linear in respect to the depth from the specimen surface, 2) the penetration depth of X-rays is a function of Sin 2 ψ and 3) the strain measured by X-rays corresponds to the average strain weighted on the intensity of the diffracted X-rays. However, the assumption of the penetration depth of X-rays is the reason we sometimes observed noticeable errors which depend on the combination of stress components in the stress tensor." @default.
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- W2482140504 date "1984-01-01" @default.
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- W2482140504 title "X-ray Multiaxial Stress Analysis on Materials with Stress Gradient by Use of Cos Ψ Function" @default.
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- W2482140504 doi "https://doi.org/10.1154/s0376030800014063" @default.
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