FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4361794552> ?p ?o ?g. }

• W4361794552 endingPage "8638" @default.
• W4361794552 startingPage "8617" @default.
• W4361794552 abstract "Fractures and other nonwelded contacts are important mechanical and hydrological features of rock masses. Their effects on seismic wave propagation can be modeled as a boundary condition in the seismic wave equation. Seismic stress is continuous across such a boundary, but seismic particle displacement and seismic particle velocity are not. The complete solutions for seismic wave reflection, conversion, and transmission across a displacement and velocity discontinuity between two half‐spaces with different densities and elastic properties are derived for all angles of the incident wave. The ratio between the seismic stress across this boundary and the seismic particle displacement and velocity are described by a specific stiffness and a specific viscosity, respectively. A displacement discontinuity results in frequency‐dependent reflection and transmission coefficients and a frequency‐dependent group time delay. The velocity discontinuity results in frequency‐independent coefficients and zero delay. Results of laboratory experiments on compressional and shear wave transmission across three different natural fractures in a quartz monzonite are described. Measurements were made at different effective stresses under dry and saturated conditions at room temperature. It is shown that the effect of these fractures on the spectral amplitudes for compressional and shear pulses transmitted across these fractures are described well by a displacement discontinuity for compressional pulses under dry and saturated conditions and by a combined displacement and velocity discontinuity for shear wave pulses under dry and saturated conditions. Values of specific stiffness and specific viscosity vary between fractures and increase with increasing effective stress, as does the static specific stiffness of these fractures. Changes in the spectral amplitudes of transmitted pulses are also analyzed in terms of attenuation using the seismic quality factor Q , which is found to be a function of frequency." @default.
• W4361794552 created "2023-04-05" @default.
• W4361794552 creator A5010159152 @default.
• W4361794552 creator A5058689845 @default.
• W4361794552 creator A5066832511 @default.
• W4361794552 date "1990-06-10" @default.
• W4361794552 modified "2023-10-11" @default.
• W4361794552 title "Transmission of seismic waves across single natural fractures" @default.
• W4361794552 cites W1593291553 @default.
• W4361794552 cites W1967067305 @default.
• W4361794552 cites W1980811494 @default.
• W4361794552 cites W1985082252 @default.
• W4361794552 cites W1985392048 @default.
• W4361794552 cites W1987007071 @default.
• W4361794552 cites W2000229319 @default.
• W4361794552 cites W2000241135 @default.
• W4361794552 cites W2015364220 @default.
• W4361794552 cites W2017450455 @default.
• W4361794552 cites W2019260018 @default.
• W4361794552 cites W2024207616 @default.
• W4361794552 cites W2028011226 @default.
• W4361794552 cites W2041855500 @default.
• W4361794552 cites W2049596313 @default.
• W4361794552 cites W2053315555 @default.
• W4361794552 cites W2057934842 @default.
• W4361794552 cites W2069119098 @default.
• W4361794552 cites W2070524598 @default.
• W4361794552 cites W2089907692 @default.
• W4361794552 cites W2090459202 @default.
• W4361794552 cites W2093238563 @default.
• W4361794552 cites W2117114165 @default.
• W4361794552 cites W2125780847 @default.
• W4361794552 cites W2142435286 @default.
• W4361794552 cites W2143922509 @default.
• W4361794552 cites W2163035644 @default.
• W4361794552 cites W2166238385 @default.
• W4361794552 doi "https://doi.org/10.1029/jb095ib06p08617" @default.
• W4361794552 hasPublicationYear "1990" @default.
• W4361794552 type Work @default.
• W4361794552 citedByCount "443" @default.
• W4361794552 countsByYear W43617945522012 @default.
• W4361794552 countsByYear W43617945522013 @default.
• W4361794552 countsByYear W43617945522014 @default.
• W4361794552 countsByYear W43617945522015 @default.
• W4361794552 countsByYear W43617945522016 @default.
• W4361794552 countsByYear W43617945522017 @default.
• W4361794552 countsByYear W43617945522018 @default.
• W4361794552 countsByYear W43617945522019 @default.
• W4361794552 countsByYear W43617945522020 @default.
• W4361794552 countsByYear W43617945522021 @default.
• W4361794552 countsByYear W43617945522022 @default.
• W4361794552 countsByYear W43617945522023 @default.
• W4361794552 crossrefType "journal-article" @default.
• W4361794552 hasAuthorship W4361794552A5010159152 @default.
• W4361794552 hasAuthorship W4361794552A5058689845 @default.
• W4361794552 hasAuthorship W4361794552A5066832511 @default.
• W4361794552 hasConcept C107551265 @default.
• W4361794552 hasConcept C120665830 @default.
• W4361794552 hasConcept C121332964 @default.
• W4361794552 hasConcept C127313418 @default.
• W4361794552 hasConcept C134306372 @default.
• W4361794552 hasConcept C15744967 @default.
• W4361794552 hasConcept C165205528 @default.
• W4361794552 hasConcept C180205008 @default.
• W4361794552 hasConcept C187320778 @default.
• W4361794552 hasConcept C2777042112 @default.
• W4361794552 hasConcept C2779438780 @default.
• W4361794552 hasConcept C33923547 @default.
• W4361794552 hasConcept C35515768 @default.
• W4361794552 hasConcept C542102704 @default.
• W4361794552 hasConcept C57879066 @default.
• W4361794552 hasConcept C5900021 @default.
• W4361794552 hasConcept C78542244 @default.
• W4361794552 hasConcept C86038547 @default.
• W4361794552 hasConcept C96035792 @default.
• W4361794552 hasConceptScore W4361794552C107551265 @default.
• W4361794552 hasConceptScore W4361794552C120665830 @default.
• W4361794552 hasConceptScore W4361794552C121332964 @default.
• W4361794552 hasConceptScore W4361794552C127313418 @default.
• W4361794552 hasConceptScore W4361794552C134306372 @default.
• W4361794552 hasConceptScore W4361794552C15744967 @default.
• W4361794552 hasConceptScore W4361794552C165205528 @default.
• W4361794552 hasConceptScore W4361794552C180205008 @default.
• W4361794552 hasConceptScore W4361794552C187320778 @default.
• W4361794552 hasConceptScore W4361794552C2777042112 @default.
• W4361794552 hasConceptScore W4361794552C2779438780 @default.
• W4361794552 hasConceptScore W4361794552C33923547 @default.
• W4361794552 hasConceptScore W4361794552C35515768 @default.
• W4361794552 hasConceptScore W4361794552C542102704 @default.
• W4361794552 hasConceptScore W4361794552C57879066 @default.
• W4361794552 hasConceptScore W4361794552C5900021 @default.
• W4361794552 hasConceptScore W4361794552C78542244 @default.
• W4361794552 hasConceptScore W4361794552C86038547 @default.
• W4361794552 hasConceptScore W4361794552C96035792 @default.
• W4361794552 hasIssue "B6" @default.
• W4361794552 hasLocation W43617945521 @default.
• W4361794552 hasOpenAccess W4361794552 @default.
• W4361794552 hasPrimaryLocation W43617945521 @default.

• next