116 



MK J. Y. BUCHANAN ON THE 



Table IX. 



Values of^^^-^ for the Ennead MRO.,. 

 ^ log ^J 











T = 



19-5° C. 











m. 



KCIO3. 



KBiOs. 



KIO3. 



RbOlOg. 



RbBiOj. 



RblOj. 



CSCIO3. 



CsBrOg. 



CSIO3. 



1/4 



2-010 



2-019 



2-031 



1-997 







1-999 







1/8 



2-019 



2-017 



1-980 



1-993 







1-968 







1/16 



2-081 



2-013 



1-996 



2-007 



1-983 



2-018 



2-029 



1-985 



2028 



1/32 



2-021 



1-990 



1-875 



1-982 



2-008 



1-931 



1-859 



2 044 



1-918 



1/64 



2-037 



1-983 



2-165 



1-882 



1-884 



1-924 



2-039 



2-047 



1-788 



1/128 



2-039 



1-965 



1-112 



1-887 



2-122 



1-814 



1-624 



1-792 



1-795 



1/256 



2-746 



1-977 



1-211 



1-653 



1-974 



2-635 



1-376 



1-746 



2-080 



1/512 





















Table X. 



Values of , ^ ^"^ for some Nitrates. 

 ^ log ^J 



m. 



Li. 



Na. 



K. 



Rb. 



Cs. 



Ba". 



Pb". 



Rb. 



Cs. 



T = 



19-6° 0. 



23-0° C. 



8 



4 



2 



1 

 1/2 

 1/4 

 1/8 

 1/16 

 1/32 

 1/64 

 1/128 

 1/256 

 1/512 



1-939 

 1-982 

 2-003 

 1-984 

 2-023 

 1-995 

 2-030 

 2034 

 2-040 

 2-083 



2-019 

 1-993 

 2-049 

 2027 

 2-026 

 2-016 

 2-020 

 2-013 

 1-995 



2-014 

 2-025 

 2-015 

 2-046 

 1-983 

 2-050 



2-000 

 2 006 

 2-008 

 2-015 

 2-068 

 2-082 

 2-258 

 2-379 

 1-961 



2-006 

 2-917 

 2-075 

 1-880 

 2-117 

 2-388 



2-048 

 2-046 

 2-159 

 2-010 

 2-129 

 1-528 



2-056 

 2-086 

 1-981 

 2-031 

 2-359 

 3-010 



2069 

 2-019 

 2-091 

 2-182 

 2-901 

 1-146 



2-019 

 2-013 

 2-048 

 2-245 

 1-851 



Section VIII. — ^Comments on the Changes in the Values of dA — v for Different 

 Values of m in the Case of Solutions op Individual Salts of the Type 



MR AND MRO3. 



§ 46. The earlier introductory notes and discussion of the values of the specific 

 gravity and displacement explain the precise meaning of these terms. A comparison of 

 the values of the increment of displacement (v) caused by the dissolution of m gram- 

 molecules of a salt in 1000 grams of water with the difference (dA) of these consecutive 

 increments of displacement possesses considerable interest. 



The increment of displacement (v) due to the dissolution of m gram-molecules of a 



