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THE FORMATION OF DOUBLE SALTS. [FOURTH PAPER.]
1911
Journal of the American Chemical Society
If the above coeflicients of diffusion be corrected to 16' (corr. 3 per cent. per degree), we get kcop = 1.378 and h0, = 1.607, and it is evident that they agree fairly well with the values or' Stefan and Hufner (cited above). Hagenbach's figures ( I I .37 uncorr.) for the diffusion of oxygen in water must therefore be considered quite incorrect, due to the source of error mentioned ab0L-e. Further, -the ratio between the coefficients of oxygen and carbon dioside, according to the above
doi:10.1021/ja02220a003
fatcat:agzb6lpe2zc6bjgm7zwtai6rn4