Attenuation and dispersion phenomena of torsional waves in self-weighted, inhomogeneous, pre-stressed poro-elastic and poro-viscoelastic stratified structure
DOI10.1080/17455030.2020.1859641zbMath1506.74161OpenAlexW3112035828MaRDI QIDQ5046773
Kuvar Satya Singh, T. M. Yunus Khan, Parvez Alam, Sarfaraz Kamangar, Irfan Anjum Badruddin
Publication date: 9 November 2022
Published in: Waves in Random and Complex Media (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/17455030.2020.1859641
initial stressdispersion equationdissipation factorcomplex frequency equationBiot gravity parameterdamping equation
Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Inhomogeneity in solid mechanics (74E05) Wave scattering in solid mechanics (74J20) Materials of strain-rate type and history type, other materials with memory (including elastic materials with viscous damping, various viscoelastic materials) (74D99)
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Cites Work
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- Dispersion and attenuation of torsional wave in a viscoelastic layer bonded between a layer and a half-space of dry sandy media
- Rayleigh wave dispersion in an irregular sandy Earth's crust over orthotropic mantle
- Stresses in soils under a foundation
- Propagation of Torsional Surface Waves in Dry Sandy Medium under Gravity
- The torsional surface wave in a prestressed anisotropic intermediate poroelastic layer of varying heterogeneities
- Modeling of magnetoelastic shear waves due to point source in a viscoelastic crustal layer over an inhomogeneous viscoelastic half space
- Torsional Waves in a Fiber Composite Medium at a Loosely Bonded Interface Constrained Between Dry Sandy Layer and Gravitating Poroelastic Substrate
- Study of torsional wave in a poroelastic medium sandwiched between a layer and a half-space of heterogeneous dry sandy media
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