The general form of the three-dimensiona
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R. D. Gregory
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Article
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1992
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Springer Netherlands
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English
β 909 KB
A homogeneous, isotropic plate has free faces and is "stretched" by tractions around its edge which are symmetrical about the mid-plane, but are otherwise generally distributed. We give a rigorous proof that the most general state of stress z~j which can be generated in the plate can be decomposed i