150 ON THE DEPRESSION OF THE FREEZING-POINT 
TABLE I. 
Sp. Mol. Cond. Sp. Mol. Cond. = 
Gonveniration, || ab 1s Peat Ore i a 
(18) (Uo) Hi8 
KCl. (74.59). 
010 | 1226 Sams | 367 
005 | 1244 | 787 | B67 
001 127 809 367 
0005 1284 84 366 
0002 1293 821 365 
0001 1298 824 365 
Na Cl. (58.50). 
010 1028 638 | 379 
005 1049 651 380 
001 1075 664 | 382 
0005 1084 670 382 
0002 | 1094. 676 | 382 
0001 | 1098 679 382 
| 
H Cl. (36.46). 
010 3706 2505 -300 
005 3731 2608 301 
002 3753 2625 301 
O01 3757 | 2626 B01 
The ratio [1 Yo appears to increase as the concentration 
18 
diminishes, except in the case of potassium chloride where it 
decreases. This peculiarity is also shown in the values as caleu- 
lated by means of } Déguisne’s data. The agreement between 
Déguisne’s conductivity values at 0° and the above for the solu- 
tions of concentration .01 is very close, but with the dilute 
solutions it is not so good. It was found impossible to obtain 
1 Kohl. u. Holb., loc. cit., p. 199, tab. 7. 
