FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2145563886> ?p ?o ?g. }

• W2145563886 endingPage "283" @default.
• W2145563886 startingPage "266" @default.
• W2145563886 abstract "Geoacoustic properties of the seabed have a controlling role in the propagation and reverberation of sound in shallow-water environments. Several techniques are available to quantify the important properties but are usually unable to adequately sample the region of interest. In this paper, we explore the potential for obtaining geotechnical properties from a process-based stratigraphic model. Grain-size predictions from the stratigraphic model are combined with two acoustic models to estimate sound speed with distance across the New Jersey continental shelf and with depth below the seabed. Model predictions are compared to two independent sets of data: 1) Surficial sound speeds obtained through direct measurement using in situ compressional wave probes, and 2) sound speed as a function of depth obtained through inversion of seabed reflection measurements. In water depths less than 100 m, the model predictions produce a trend of decreasing grain-size and sound speed with increasing water depth as similarly observed in the measured surficial data. In water depths between 100 and 130 m, the model predictions exhibit an increase in sound speed that was not observed in the measured surficial data. A closer comparison indicates that the grain-sizes predicted for the surficial sediments are generally too small producing sound speeds that are too slow. The predicted sound speeds also tend to be too slow for sediments 0.5-20 m below the seabed in water depths greater than 100 m. However, in water depths less than 100 m, the sound speeds between 0.5-20-m subbottom depth are generally too fast. There are several reasons for the discrepancies including the stratigraphic model was limited to two dimensions, the model was unable to simulate biologic processes responsible for the high sound-speed shell material common in the model area, and incomplete geological records necessary to accurately predict grain-size" @default.
• W2145563886 created "2016-06-24" @default.
• W2145563886 creator A5016014077 @default.
• W2145563886 creator A5021009892 @default.
• W2145563886 creator A5025845776 @default.
• W2145563886 creator A5031810651 @default.
• W2145563886 creator A5043878489 @default.
• W2145563886 creator A5076119636 @default.
• W2145563886 date "2006-04-01" @default.
• W2145563886 modified "2023-10-18" @default.
• W2145563886 title "Stratigraphic Model Predictions of Geoacoustic Properties" @default.
• W2145563886 cites W152384092 @default.
• W2145563886 cites W1968796659 @default.
• W2145563886 cites W1971754296 @default.
• W2145563886 cites W1972450900 @default.
• W2145563886 cites W1976157543 @default.
• W2145563886 cites W1977439062 @default.
• W2145563886 cites W1984617729 @default.
• W2145563886 cites W1986669645 @default.
• W2145563886 cites W1995129528 @default.
• W2145563886 cites W1996606146 @default.
• W2145563886 cites W1996720026 @default.
• W2145563886 cites W2000474073 @default.
• W2145563886 cites W2000647453 @default.
• W2145563886 cites W2003584756 @default.
• W2145563886 cites W2004203253 @default.
• W2145563886 cites W2012144497 @default.
• W2145563886 cites W2017741943 @default.
• W2145563886 cites W2028177713 @default.
• W2145563886 cites W2033153518 @default.
• W2145563886 cites W2035157786 @default.
• W2145563886 cites W2039056822 @default.
• W2145563886 cites W2039419519 @default.
• W2145563886 cites W2040990829 @default.
• W2145563886 cites W2041371647 @default.
• W2145563886 cites W2042883028 @default.
• W2145563886 cites W2044009994 @default.
• W2145563886 cites W2046543856 @default.
• W2145563886 cites W2048690053 @default.
• W2145563886 cites W2049860289 @default.
• W2145563886 cites W2053606088 @default.
• W2145563886 cites W2066514319 @default.
• W2145563886 cites W2069434808 @default.
• W2145563886 cites W2076330525 @default.
• W2145563886 cites W2092155773 @default.
• W2145563886 cites W2094394939 @default.
• W2145563886 cites W2094464437 @default.
• W2145563886 cites W2103146228 @default.
• W2145563886 cites W2109459276 @default.
• W2145563886 cites W2111400803 @default.
• W2145563886 cites W2127918736 @default.
• W2145563886 cites W2128415525 @default.
• W2145563886 cites W2133290278 @default.
• W2145563886 cites W2136227156 @default.
• W2145563886 cites W2143727093 @default.
• W2145563886 cites W2164830765 @default.
• W2145563886 cites W2168052759 @default.
• W2145563886 cites W2176241949 @default.
• W2145563886 cites W2345394035 @default.
• W2145563886 cites W3033809548 @default.
• W2145563886 cites W42395612 @default.
• W2145563886 doi "https://doi.org/10.1109/joe.2006.875235" @default.
• W2145563886 hasPublicationYear "2006" @default.
• W2145563886 type Work @default.
• W2145563886 sameAs 2145563886 @default.
• W2145563886 citedByCount "7" @default.
• W2145563886 crossrefType "journal-article" @default.
• W2145563886 hasAuthorship W2145563886A5016014077 @default.
• W2145563886 hasAuthorship W2145563886A5021009892 @default.
• W2145563886 hasAuthorship W2145563886A5025845776 @default.
• W2145563886 hasAuthorship W2145563886A5031810651 @default.
• W2145563886 hasAuthorship W2145563886A5043878489 @default.
• W2145563886 hasAuthorship W2145563886A5076119636 @default.
• W2145563886 hasConcept C111368507 @default.
• W2145563886 hasConcept C114793014 @default.
• W2145563886 hasConcept C121332964 @default.
• W2145563886 hasConcept C127313418 @default.
• W2145563886 hasConcept C165205528 @default.
• W2145563886 hasConcept C186348155 @default.
• W2145563886 hasConcept C192191005 @default.
• W2145563886 hasConcept C200351514 @default.
• W2145563886 hasConcept C203718221 @default.
• W2145563886 hasConcept C24890656 @default.
• W2145563886 hasConcept C33613203 @default.
• W2145563886 hasConcept C95851461 @default.
• W2145563886 hasConceptScore W2145563886C111368507 @default.
• W2145563886 hasConceptScore W2145563886C114793014 @default.
• W2145563886 hasConceptScore W2145563886C121332964 @default.
• W2145563886 hasConceptScore W2145563886C127313418 @default.
• W2145563886 hasConceptScore W2145563886C165205528 @default.
• W2145563886 hasConceptScore W2145563886C186348155 @default.
• W2145563886 hasConceptScore W2145563886C192191005 @default.
• W2145563886 hasConceptScore W2145563886C200351514 @default.
• W2145563886 hasConceptScore W2145563886C203718221 @default.
• W2145563886 hasConceptScore W2145563886C24890656 @default.
• W2145563886 hasConceptScore W2145563886C33613203 @default.
• W2145563886 hasConceptScore W2145563886C95851461 @default.
• W2145563886 hasIssue "2" @default.

• next