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Energy decay and selfpreserving correlation functions in isotropic
Elastic stresses due to a semiinfinite band of hydrostatic pressure
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according angle antenna applied approximation assumed axis becomes boundary conditions bounded calculated characteristic coefficients complete components computed consider constant continuous corresponding defined depends derived determined differential direction discussed displacement distribution effect elements equal equation example expression fact field finite flow formula frequency function given gives Hence infinite integral interest introduce known layer leading length limit linear mathematical mean method noise normal obtained origin plane plate positive potential present problem reference region relation represents respectively roots satisfies shown shows similar solution solved space stream stress surface Table theorem theory tion transform unit values vanishes variable vector velocity wave write written yields zero