65 



18. P. W. Bridgeman, Pro. Am. Acad. Arts Sci ., 76, 55, 71 (1 



19. Co E. Weir, J. Research Nat. Bur. Standards , 45, 468(1950). 



20. C. E. Weir, J. Research Nat. Bur. Standards > 50, 95 (1953). 



21. C. E. Weir, J. Research Nat. Bur. Standards, 53, 245 (1954). 



22. See A. Defant, Physical Oceanography, Pergamon Press, New York (1961), 



vol. I, pp. 123-129, for a discussion of the oceanographic significance 

 of and formulas for the adiabatic temperature change with depth in the 

 sea . 



23. S. D. HamannandW. Strauss, Trans . Faraday Soc . , ^, 168(1955). 



24. L. H. Adams andR. E. Hall, J. Phys . Chem ., 35, 2145 (1931). 



25. W. A. Zisman, Phys. Rev ., 39, 151 (1932). 



26. H. U. Sverdrup, M. W. Johnson, and R. H. Fleming, The Oceans , Prentice- 



Hall, Inc., Englewood Cliffs, N. J. (1942), p. 51. 



27. For a discussion of the possible errors in the literature values of the com- 



pressibility of sea water, see V. A. Del Grosso, Conf. Phys. & Chem. 

 Properties of Sea Water (Easton, Md., 1958), Nat. Research Council - 

 Nat. Acad. Sci., Publ. 600 (1959), pp. 185-195. 



28. Although expressed in terms of weight, salinity is a concentration unit; de- 



creasing the volume is therefore equivalent to increasing the salinityj 

 all at constant weight . 



29. ICT, vol. m, p. 440. 



30. S. D. Hamann, op._cito!, pp. 129-131. 



31. H. U. Sverdrup, op. cit., p. 166. 



32. H. W. Jones and C. B. Monk, Trans . Faraday Soc . , 48, 929 (1952). 



33. S. D. Hamann, op. cit., pp. 122-124. 



34. R. Cohen, Ann. Physik, 45, 666(1892). 



35. F.Korber, Z physik. Chem., 67, 212(1909); 77, 420(1911); 80, 478(1912). 



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