Physical Foundations of Technical Acoustics 1969
DOI: 10.1016/b978-0-08-011097-4.50017-6
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Two-Dimensional Systems

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Cited by 3 publications
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“…This kind of lattice instability is equivalent to the softening of the effective elastic constant in (1 11) directions: Ceff(111) =!dC11+2C12 +4C44)* Ceffcl 1 > can be obtained by analysing the longitudinal elastic wave propagation in the ( 1 1 1 ) directions (e.g. see Malecki 1969). Therefore the effect of stress on the lattice instability responsible for the R and martensitic transformations can be studied by investigating the effect of stress on Cefr(lll) and C' which also can be obtained by analysing the ( 1 TO) transverse elastic wave propagation in the cubic crystal:…”
Section: Downloaded By [New York University] At 02:01 31 July 2015mentioning
confidence: 99%
“…This kind of lattice instability is equivalent to the softening of the effective elastic constant in (1 11) directions: Ceff(111) =!dC11+2C12 +4C44)* Ceffcl 1 > can be obtained by analysing the longitudinal elastic wave propagation in the ( 1 1 1 ) directions (e.g. see Malecki 1969). Therefore the effect of stress on the lattice instability responsible for the R and martensitic transformations can be studied by investigating the effect of stress on Cefr(lll) and C' which also can be obtained by analysing the ( 1 TO) transverse elastic wave propagation in the cubic crystal:…”
Section: Downloaded By [New York University] At 02:01 31 July 2015mentioning
confidence: 99%
“…As the temperature increased from −2 to 84°F, the normalized amplitude decreased considerably, at the greatest distance, the normalized amplitude dropped from approximately 0.2 at −2°F to approximately 0.01 at 84°F. The amplitude attenuation of the SH waves can be expressed using an exponential function ( 22 ):…”
Section: Effect Of Temperature On Asphalt Propertiesmentioning
confidence: 99%
“…For stress-free surfaces, an infinite matrix system arises [1,2]. Physically [3], at the surfaces a coupling of transverse and longitudinal waves occurs, so individual component waves cannot in general be treated independently. In this note we restrict attention to the plane-strain case and seek analytic solutions for the natural oscillations of a cuboid with two pairs of opposite sides free.…”
mentioning
confidence: 99%