2011
DOI: 10.1016/j.quaint.2009.07.028
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Physical and geoacoustic properties of surface sediments off eastern Geoje Island, South Sea of Korea

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Cited by 34 publications
(9 citation statements)
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“…Moreover, these parameters are vital for the theory of wave propagation in unconsolidated seafloor sediment [9][10][11][12][13][14][15][16]. In addition, these parameters can be used to evaluate the geological events of marine sedimentary environments and control seismoacoustic propagation in the ocean [17][18][19][20][21][22][23].…”
Section: Introductionmentioning
confidence: 99%
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“…Moreover, these parameters are vital for the theory of wave propagation in unconsolidated seafloor sediment [9][10][11][12][13][14][15][16]. In addition, these parameters can be used to evaluate the geological events of marine sedimentary environments and control seismoacoustic propagation in the ocean [17][18][19][20][21][22][23].…”
Section: Introductionmentioning
confidence: 99%
“…In recent decades, extensive studies have been conducted to reveal the relationships between compression waves and physical properties and textural parameters relative to various regions, such as the North Pacific [17], Yellow Sea of China [2,8,[24][25][26], South China Sea (SCS) [7,14,15,23,27,28], South Sea of Korea [12,19,20,22,30], West coast of India [31], and West coast of Scotland [32]. These relationships show that the density, porosity, and mean grain size play a central role in determining the compression wave speed of seafloor sediment [33,34].…”
Section: Introductionmentioning
confidence: 99%
“…Geoacoustic models based on physical properties have been established to study the sediment-geoacoustic relationships (Hamilton, 1980;Huang et al, 2018;Kim et al, 2011;Wang et al, 2016;Zhou et al, 2009). However, there is variability of sediments properties, especially for sediments in different regions with different properties.…”
Section: Introductionmentioning
confidence: 99%
“…The Coastal Benthic Boundary Layer project measured the top 40 cm of sediment and the results indicated that the sound speed and attenuation exhibited vertical and lateral variability [6]. Kim et al [22] classified the seafloor of the South Sea shelf into four areas based on the distribution of grain size, and established the prediction equation of sound speed. Yang and Seong [38] presented the sound speed and attenuation data as a function of frequency and grain size distribution.…”
Section: Introductionmentioning
confidence: 99%