Chemical sound absorption in sea water cannot be considered the sum of independent relaxation processes because many equilibria have common ions. Effects of coupling on the MgCO30 and MgB(OH)+4 relaxations can be explained as simple buffer reactions that equilibrate rapidly and follow the slower reactions. The B(OH)3 relaxation, however, is explained by a different mechanism involving exchange with the HCO3−/CO32− system.
Topics
Acoustic phenomena
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© 1981 Acoustical Society of America.
1981
Acoustical Society of America
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