1962
DOI: 10.1121/1.1918213
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Sound Absorption in Sea Water

Abstract: An expression is presented for sound absorption in sea water as a function of frequency, temperature, salinity, and pressure. It is based on available data reported in the literature and new data taken in the North Atlantic Ocean in the frequency range 2–25 kcps.

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Cited by 111 publications
(30 citation statements)
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“…At each value of water temperature, the bars plotted include the combined range of the effects of pressure and salinity. Shown in this figure are the values of α W calculated by the methods of Schulkin and Marsh (1962) and, for comparison, Ainslie and McColm (1998).…”
Section: Appendix 4 Comparison Of the Effects Of Water Temperature mentioning
confidence: 99%
See 1 more Smart Citation
“…At each value of water temperature, the bars plotted include the combined range of the effects of pressure and salinity. Shown in this figure are the values of α W calculated by the methods of Schulkin and Marsh (1962) and, for comparison, Ainslie and McColm (1998).…”
Section: Appendix 4 Comparison Of the Effects Of Water Temperature mentioning
confidence: 99%
“…Under the relatively shallow-water and low-salinity conditions in rivers, however, α W meaningfully depends only on water temperature (appendix 4). In our study, we use the α W of Schulkin and Marsh (1962), which is calculated on the basis of varying water temperature while pressure and salinity are held constant at appropriate low values. α S depends on the properties of the suspended sediment and is discussed in detail in the "Physical Basis for the Sediment Attenuation Coefficient" section below.…”
Section: Two-way Transmission Lossmentioning
confidence: 99%
“…Finally, an acoustic propagation model proposed by Schulkin [20] is considered. According to that model, the received signal should be multiplied by a corrective coefficient p:…”
Section: Underwater Acoustic Channelmentioning
confidence: 99%
“…Pressure does not have a significant effect on the absorption coefficient for shallow water systems (depth ≤20 m; Alvarez and Jones 2002). The absorption coefficients (α) for water used in the signal strength calculations for the ADV for different temperature and salinity values were estimated by the approach of Shulkin and Marsh (1962):…”
Section: Methodsmentioning
confidence: 99%