FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2859646976> ?p ?o ?g. }

• W2859646976 endingPage "544" @default.
• W2859646976 startingPage "534" @default.
• W2859646976 abstract "The impact of unconsolidated sedimentary basins on ground motion amplification is of particular interest for earthquake engineers and seismologists. The Mississippi embayment (ME) of the New Madrid seismic zone, located in the central United States, is covered with a thick layer of unconsolidated soil deposits. Thus, the estimation of site response in this region is vital to simulate site-specific ground motions and to conduct site-specific probabilistic seismic hazard analysis. We evaluated site amplification at 11 stations within the ME, employing the horizontal-to-vertical spectral ratio (HVSR) technique. Regarding the results obtained from this study, weak ground motions recorded by stations on the unconsolidated ME sediments are amplified 3–7 times for frequencies less than 5 Hz compared to stations located on bedrock. The fundamental resonant frequencies vary from 0.2 to 0.4 Hz within the ME. We investigated differences between the HVSRs obtained from P-waves, S-waves, coda, and pre-event noise. All fundamental frequencies obtained from different seismic phases are in good agreement with a less than 10% difference. The fundamental frequencies of the P-wave and S-wave are relatively higher due to higher velocity of the P-wave and S-wave compared to other phases since the velocity of seismic waves and fundamental frequencies are proportional. There is a good correlation between the HVSR of the S-wave, coda, and pre-event noise portions for frequencies more than 4 Hz. For the frequencies less than 4 Hz, the HVSR of the S-wave is higher than the HVSR of coda by a factor of 3. Reflections of S-waves from the edges of the unconsolidated sedimentary basin of the ME produce surface waves. The presence of basin-induced surface waves in the coda portion for frequencies less than 3 Hz results in increased amplitude of coda, and as a result, slower decay rate with time implying higher Q values. These basin-induced surface waves have a period of 0.5–4.0 s." @default.
• W2859646976 created "2018-07-19" @default.
• W2859646976 creator A5011141575 @default.
• W2859646976 creator A5059284938 @default.
• W2859646976 creator A5080839075 @default.
• W2859646976 date "2018-10-01" @default.
• W2859646976 modified "2023-09-29" @default.
• W2859646976 title "Site amplification within the Mississippi embayment of the central United States: Investigation of possible differences among various phases of seismic waves and presence of basin waves" @default.
• W2859646976 cites W1819897745 @default.
• W2859646976 cites W1909297638 @default.
• W2859646976 cites W1921024748 @default.
• W2859646976 cites W1965347733 @default.
• W2859646976 cites W1969052312 @default.
• W2859646976 cites W1971207705 @default.
• W2859646976 cites W1973966093 @default.
• W2859646976 cites W1976204513 @default.
• W2859646976 cites W1988977821 @default.
• W2859646976 cites W2004883604 @default.
• W2859646976 cites W2011006169 @default.
• W2859646976 cites W2014273112 @default.
• W2859646976 cites W2015519679 @default.
• W2859646976 cites W2022716782 @default.
• W2859646976 cites W2045846483 @default.
• W2859646976 cites W2053059783 @default.
• W2859646976 cites W2072167209 @default.
• W2859646976 cites W2086188578 @default.
• W2859646976 cites W2086648797 @default.
• W2859646976 cites W2090756253 @default.
• W2859646976 cites W2100896142 @default.
• W2859646976 cites W2103817435 @default.
• W2859646976 cites W2106643862 @default.
• W2859646976 cites W2106822551 @default.
• W2859646976 cites W2112754941 @default.
• W2859646976 cites W2114441808 @default.
• W2859646976 cites W2114637895 @default.
• W2859646976 cites W2119428020 @default.
• W2859646976 cites W2120489623 @default.
• W2859646976 cites W2125290000 @default.
• W2859646976 cites W2128923563 @default.
• W2859646976 cites W2135623048 @default.
• W2859646976 cites W2135782284 @default.
• W2859646976 cites W2139947173 @default.
• W2859646976 cites W2145588834 @default.
• W2859646976 cites W2147762555 @default.
• W2859646976 cites W2153814770 @default.
• W2859646976 cites W2154922118 @default.
• W2859646976 cites W2159613255 @default.
• W2859646976 cites W2167291508 @default.
• W2859646976 cites W2181633651 @default.
• W2859646976 cites W2212995750 @default.
• W2859646976 cites W2268264955 @default.
• W2859646976 cites W2409333246 @default.
• W2859646976 cites W2414373746 @default.
• W2859646976 cites W2515488669 @default.
• W2859646976 cites W2520303659 @default.
• W2859646976 cites W2557852169 @default.
• W2859646976 cites W2563673385 @default.
• W2859646976 cites W2570759567 @default.
• W2859646976 cites W2587299754 @default.
• W2859646976 cites W2675127795 @default.
• W2859646976 cites W2773059956 @default.
• W2859646976 cites W2800842027 @default.
• W2859646976 doi "https://doi.org/10.1016/j.soildyn.2018.04.017" @default.
• W2859646976 hasPublicationYear "2018" @default.
• W2859646976 type Work @default.
• W2859646976 sameAs 2859646976 @default.
• W2859646976 citedByCount "12" @default.
• W2859646976 countsByYear W28596469762019 @default.
• W2859646976 countsByYear W28596469762020 @default.
• W2859646976 countsByYear W28596469762021 @default.
• W2859646976 countsByYear W28596469762022 @default.
• W2859646976 countsByYear W28596469762023 @default.
• W2859646976 crossrefType "journal-article" @default.
• W2859646976 hasAuthorship W2859646976A5011141575 @default.
• W2859646976 hasAuthorship W2859646976A5059284938 @default.
• W2859646976 hasAuthorship W2859646976A5080839075 @default.
• W2859646976 hasConcept C109007969 @default.
• W2859646976 hasConcept C114793014 @default.
• W2859646976 hasConcept C115961682 @default.
• W2859646976 hasConcept C121332964 @default.
• W2859646976 hasConcept C122205909 @default.
• W2859646976 hasConcept C127313418 @default.
• W2859646976 hasConcept C1276947 @default.
• W2859646976 hasConcept C137527640 @default.
• W2859646976 hasConcept C154945302 @default.
• W2859646976 hasConcept C165205528 @default.
• W2859646976 hasConcept C194257627 @default.
• W2859646976 hasConcept C195761226 @default.
• W2859646976 hasConcept C200646496 @default.
• W2859646976 hasConcept C203718221 @default.
• W2859646976 hasConcept C205312793 @default.
• W2859646976 hasConcept C23509580 @default.
• W2859646976 hasConcept C2988284105 @default.
• W2859646976 hasConcept C30947920 @default.
• W2859646976 hasConcept C3962253 @default.
• W2859646976 hasConcept C41008148 @default.
• W2859646976 hasConcept C46362747 @default.
• W2859646976 hasConcept C49040817 @default.

• next