Volume 40 Issue 4
Jun.  2021
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Guanbao Li, Jingqiang Wang, Xiangmei Meng, Baohua Liu, Guangming Kan, Guozhong Han, Qingfeng Hua, Yanliang Pei, Lei Sun. Relationships between the sound speed ratio and physical properties of surface sediments in the South Yellow Sea[J]. Acta Oceanologica Sinica, 2021, 40(4): 65-73. doi: 10.1007/s13131-021-1764-8
Citation: Guanbao Li, Jingqiang Wang, Xiangmei Meng, Baohua Liu, Guangming Kan, Guozhong Han, Qingfeng Hua, Yanliang Pei, Lei Sun. Relationships between the sound speed ratio and physical properties of surface sediments in the South Yellow Sea[J]. Acta Oceanologica Sinica, 2021, 40(4): 65-73. doi: 10.1007/s13131-021-1764-8

Relationships between the sound speed ratio and physical properties of surface sediments in the South Yellow Sea

doi: 10.1007/s13131-021-1764-8
Funds:  The National Natural Science Foundation of China under contract Nos 42076082, 41706062 and 41676055; the Director Fund of Pilot National Laboratory for Marine Science and Technology (Qingdao) under contract No. QNLM201713; the Public Science and Technology Research Funds Projects of Ocean under contract No. 201405032; the Taishan Scholar Project Funding under contract No. tspd20161007.
More Information
  • Corresponding author: E-mail: bhliu@ndsc.org.cn
  • Received Date: 2020-01-08
  • Accepted Date: 2020-11-21
  • Available Online: 2021-05-07
  • Publish Date: 2021-06-03
  • Building empirical equations is an effective way to link the acoustic and physical properties of sediments. These equations play an important role in the prediction of sediments sound speeds required in underwater acoustics. Although many empirical equations coupling acoustic and physical properties have been developed over the past few decades, further confirmation of their applicability by obtaining large amounts of data, especially for equations based on in situ acoustic measurement techniques, is required. A sediment acoustic survey in the South Yellow Sea from 2009 to 2010 revealed statistical relationships between the in situ sound speed and sediment physical properties. To improve the comparability of these relationships with existing empirical equations, the present study calculated the ratio of the in situ sediment sound speed to the bottom seawater sound speed, and established the relationships between the sound speed ratio and the mean grain size, density and porosity of the sediment. The sound speed of seawater at in situ measurement stations was calculated using a perennially averaged seawater sound speed map by an interpolation method. Moreover, empirical relations between the index of impedance and the sound speed and the physical properties were established. The results confirmed that the existing empirical equations between the in situ sound speed ratio and the density and porosity have general suitability for application. This study also considered that a multiple-parameter equation coupling the sound speed ratio to both the porosity and the mean grain size may be more useful for predicting the sound speed than an equation coupling the sound speed ratio to the mean grain size.
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  • [1]
    Bachman R T. 1989. Estimating velocity ratio in marine sediment. The Journal of the Acoustical Society of America, 86(5): 2029–2032. doi: 10.1121/1.398585
    [2]
    Bae S H, Kim D C, Lee G S, et al. 2014. Physical and acoustic properties of inner shelf sediments in the South Sea, Korea. Quaternary International, 344: 125–142. doi: 10.1016/j.quaint.2014.03.058
    [3]
    Biot M A. 1956a. Theory of propagation of elastic waves in a fluid-saturated porous solid: I. Low-frequency range. The Journal of the Acoustical Society of America, 28(2): 168–178. doi: 10.1121/1.1908239
    [4]
    Biot M A. 1956b. Theory of propagation of elastic waves in a fluid-saturated porous solid: II. Higher frequency range. The Journal of the Acoustical Society of America, 28(2): 179–191. doi: 10.1121/1.1908241
    [5]
    Buckingham M J. 2000. Wave propagation, stress relaxation, and grain-to-grain shearing in saturated, unconsolidated marine sediments. The Journal of the Acoustical Society of America, 108(6): 2796–2815. doi: 10.1121/1.1322018
    [6]
    Buckingham M J. 2007. On pore-fluid viscosity and the wave properties of saturated granular materials including marine sediments. The Journal of the Acoustical Society of America, 122(3): 1486–1501. doi: 10.1121/1.2759167
    [7]
    Chotiros N P, Isakson M J. 2004. A broadband model of sandy ocean sediments: biot-Stoll with contact squirt flow and shear drag. The Journal of the Acoustical Society of America, 116(4): 2011–2022. doi: 10.1121/1.1791715
    [8]
    Chotiros N P, Isakson M J. 2014. Shear wave attenuation and micro-fluidics in water-saturated sand and glass beads. The Journal of the Acoustical Society of America, 135(6): 3264–3279. doi: 10.1121/1.4874955
    [9]
    Editorial Board for Marine Atlas. 1993. Marine Atlas of Bohai Sea, Huanghai Sea and East China Sea (Hydrology) (in Chinese). Beijing: China Ocean Press
    [10]
    Fu S S, Wilkens R H, Frazer L N. 1996. Acoustic lance: new in situ seafloor velocity profiles. The Journal of the Acoustical Society of America, 99(1): 234–242. doi: 10.1121/1.414506
    [11]
    Hamilton E L. 1963. Sediment sound velocity measurements made in situ from Bathyscaph Trieste. Journal of Geophysical Research, 68(21): 5991–5998. doi: 10.1029/JZ068i021p05991
    [12]
    Hamilton E L. 1971. Prediction of in-situ acoustic and elastic properties of marine sediments. Geophysics, 36(2): 266–284. doi: 10.1190/1.1440168
    [13]
    Hamilton E L, Bachman R T. 1982. Sound velocity and related properties of marine sediments. The Journal of the Acoustical Society of America, 72(6): 1891–1904. doi: 10.1121/1.388539
    [14]
    Hamilton E L, Shumway G, Menard H W, et al. 1956. Acoustic and other physical properties of shallow-water sediments off San Diego. The Journal of the Acoustical Society of America, 28(1): 1–15. doi: 10.1121/1.1908210
    [15]
    Jackson D R, Richardson M D. 2007. High-Frequency Seafloor Acoustics. New York: Springer
    [16]
    Kamann P J, Ritzi R W, Dominic D F, et al. 2007. Porosity and permeability in sediment mixtures. Groundwater, 45(4): 429–438. doi: 10.1111/j.1745-6584.2007.00313.x
    [17]
    Kan Guangming, Liu Baohua, Zhao Yuexia, et al. 2011. Self-contained in situ sediment acoustic measurement system based on hydraulic driving penetration. High Technology Letters, 17(3): 311–316
    [18]
    Kim G Y, Kim D C, Yoo D G, et al. 2011. Physical and geoacoustic properties of surface sediments off eastern Geoje Island, South Sea of Korea. Quaternary International, 230(1–2): 21–33. doi: 10.1016/j.quaint.2009.07.028
    [19]
    Kimura M. 2011. Velocity dispersion and attenuation in granular marine sediments: comparison of measurements with predictions using acoustic models. The Journal of the Acoustical Society of America, 129(6): 3544–3561. doi: 10.1121/1.3585841
    [20]
    Liu Baohua, Han Tongcheng, Kan Guangming, et al. 2013. Correlations between the in situ acoustic properties and geotechnical parameters of sediments in the Yellow Sea, China. Journal of Asian Earth Sciences, 77: 83–90. doi: 10.1016/j.jseaes.2013.07.040
    [21]
    Meng Xiangmei, Liu Baohua, Kan Guangming, et al. 2012. An experimental study on acoustic properties and their influencing factors of marine sediment in the southern Huanghai Sea. Acta Oceanologia Sinica (in Chinese), 34(6): 74–83
    [22]
    Richardson M D. 1997. In-situ, shallow-water sediments geoacoustic properties. In: Zhang R, Zhou J, eds. Shallow-Water Acoustics. Beijing: China Ocean Press, 163–170
    [23]
    Richardson M D, Briggs K B. 1993. On the use of acoustic impedance values to determine sediment properties. In: Pace N G, Langhorne D N, eds. Acoustic Classification and Mapping of the Seabed. Bath: Institute of Acoustics, 15–25
    [24]
    Richardson M D, Briggs K B. 1996. In situ and laboratory geoacoustic measurements in soft mud and hard-packed sand sediments: implications for high-frequency acoustic propagation and scattering. Geo-Marine Letters, 16(3): 196–203. doi: 10.1007/BF01204509
    [25]
    Richardson M D, Briggs K B. 2004. Empirical predictions of seafloor properties based on remotely measured sediment impedance. In: Porter M B, Siderius M, eds. High Frequency Ocean Acoustic Conference. Melville: AIP Press, 12–21
    [26]
    Shi Xuefa. 2012. China Coastal Seas-Marine Sediment (in Chinese). Beijing: China Ocean Press, 27–46
    [27]
    Stoll R D. 1977. Acoustic waves in ocean sediments. Geophysics, 42(4): 715–725. doi: 10.1190/1.1440741
    [28]
    Wang Jingqiang, Li Guanbao, Liu Baohua, et al. 2018. Experimental study of the ballast in situ sediment acoustic measurement system in South China Sea. Marine Georesources & Geotechnology, 36(5): 515–521
    [29]
    Williams K L. 2001. An effective density fluid model for acoustic propagation in sediments derived from Biot theory. The Journal of the Acoustical Society of America, 110(5): 2276–2281. doi: 10.1121/1.1412449
    [30]
    Yang Jie, Tang Dajun. 2017. Direct measurements of sediment sound speed and attenuation in the frequency band of 2–8 kHz at the target and reverberation experiment site. IEEE Journal of Oceanic Engineering, 42(4): 1102–1109. doi: 10.1109/JOE.2017.2714722
    [31]
    Zhou Jixun, Zhang Xuezhen, Knobles D P. 2009. Low-frequency geoacoustic model for the effective properties of sandy seabottoms. The Journal of the Acoustical Society of America, 125(5): 2847–2866. doi: 10.1121/1.3089218
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