FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2043262778> ?p ?o ?g. }

• W2043262778 endingPage "113" @default.
• W2043262778 startingPage "101" @default.
• W2043262778 abstract "Obtaining high-quality dispersion curves is a critical step in the development of reliable shear wave velocity profiles from surface wave measurements. Because of its limited equipment and space requirements, the refraction microtremor (ReMi) method has become a popular approach for determining surface wave dispersion curves, and is increasingly being used for estimating low-frequency (long wavelength) surface wave velocities that are beyond the range of most active sources. The recent development of a low-frequency field vibrator as part of the Network for Earthquake Engineering Simulation (NEES) program has made it possible to actively generate surface wave energy down to frequencies of less than 1 Hz. This paper presents a comparative study of the ReMi method and the active-source frequency-wavenumber [Formula: see text] method (using the NEES vibrator) for developing low-frequency dispersion curves. Linear arrays of 1-Hz seismometers were deployed at eight deep soil sites in the Mississippi Embayment. Using both ambient and active energy, surface wave dispersion curves were determined to wavelengths of 600 m. The dispersion data from the two methods were in good agreement (within about ±5%) to wavelengths of 100 to 150 m (3 to 4 Hz) at most sites. However, at longer wavelengths the dispersion estimates from the ReMi approach deviated significantly from the active source measurements. The validity of the [Formula: see text] dispersion curve was supported by dispersion data obtained using the SASW method, as well as ambient vibration measurements performed using a circular array at four of the sites. Analyses of ambient vibrations recorded using circular arrays show that the poor performance of the ReMi method at long wavelengths is not because of a lack of ambient surface wave energy at low frequencies, but can be attributed to invalid assumptions about the nature of the ambient wavefield." @default.
• W2043262778 created "2016-06-24" @default.
• W2043262778 creator A5025199261 @default.
• W2043262778 creator A5046380471 @default.
• W2043262778 date "2009-09-01" @default.
• W2043262778 modified "2023-10-18" @default.
• W2043262778 title "Comparative Study of Refraction Microtremor (ReMi) and Active Source Methods for Developing Low-Frequency Surface Wave Dispersion Curves" @default.
• W2043262778 cites W2053932217 @default.
• W2043262778 cites W2064903949 @default.
• W2043262778 cites W2097629416 @default.
• W2043262778 cites W2102027744 @default.
• W2043262778 cites W2103726382 @default.
• W2043262778 cites W2106632637 @default.
• W2043262778 cites W2109874633 @default.
• W2043262778 cites W2143336779 @default.
• W2043262778 cites W2153814770 @default.
• W2043262778 cites W2334913705 @default.
• W2043262778 cites W3022743960 @default.
• W2043262778 cites W4237696845 @default.
• W2043262778 doi "https://doi.org/10.2113/jeeg14.3.101" @default.
• W2043262778 hasPublicationYear "2009" @default.
• W2043262778 type Work @default.
• W2043262778 sameAs 2043262778 @default.
• W2043262778 citedByCount "17" @default.
• W2043262778 countsByYear W20432627782012 @default.
• W2043262778 countsByYear W20432627782013 @default.
• W2043262778 countsByYear W20432627782014 @default.
• W2043262778 countsByYear W20432627782015 @default.
• W2043262778 countsByYear W20432627782018 @default.
• W2043262778 countsByYear W20432627782020 @default.
• W2043262778 countsByYear W20432627782021 @default.
• W2043262778 countsByYear W20432627782022 @default.
• W2043262778 countsByYear W20432627782023 @default.
• W2043262778 crossrefType "journal-article" @default.
• W2043262778 hasAuthorship W2043262778A5025199261 @default.
• W2043262778 hasAuthorship W2043262778A5046380471 @default.
• W2043262778 hasConcept C120665830 @default.
• W2043262778 hasConcept C121332964 @default.
• W2043262778 hasConcept C122205909 @default.
• W2043262778 hasConcept C127313418 @default.
• W2043262778 hasConcept C165205528 @default.
• W2043262778 hasConcept C177562468 @default.
• W2043262778 hasConcept C205318122 @default.
• W2043262778 hasConcept C30475298 @default.
• W2043262778 hasConcept C6260449 @default.
• W2043262778 hasConcept C84174578 @default.
• W2043262778 hasConceptScore W2043262778C120665830 @default.
• W2043262778 hasConceptScore W2043262778C121332964 @default.
• W2043262778 hasConceptScore W2043262778C122205909 @default.
• W2043262778 hasConceptScore W2043262778C127313418 @default.
• W2043262778 hasConceptScore W2043262778C165205528 @default.
• W2043262778 hasConceptScore W2043262778C177562468 @default.
• W2043262778 hasConceptScore W2043262778C205318122 @default.
• W2043262778 hasConceptScore W2043262778C30475298 @default.
• W2043262778 hasConceptScore W2043262778C6260449 @default.
• W2043262778 hasConceptScore W2043262778C84174578 @default.
• W2043262778 hasIssue "3" @default.
• W2043262778 hasLocation W20432627781 @default.
• W2043262778 hasOpenAccess W2043262778 @default.
• W2043262778 hasPrimaryLocation W20432627781 @default.
• W2043262778 hasRelatedWork W1481439772 @default.
• W2043262778 hasRelatedWork W2021115869 @default.
• W2043262778 hasRelatedWork W2059132183 @default.
• W2043262778 hasRelatedWork W2062228663 @default.
• W2043262778 hasRelatedWork W2086614337 @default.
• W2043262778 hasRelatedWork W2113976481 @default.
• W2043262778 hasRelatedWork W2368098336 @default.
• W2043262778 hasRelatedWork W2736843684 @default.
• W2043262778 hasRelatedWork W4234390543 @default.
• W2043262778 hasRelatedWork W3091628328 @default.
• W2043262778 hasVolume "14" @default.
• W2043262778 isParatext "false" @default.
• W2043262778 isRetracted "false" @default.
• W2043262778 magId "2043262778" @default.
• W2043262778 workType "article" @default.