616 WILLIAM LAWTON GOODWIN ON THE 
$(C1C1,+ NaCl). : 
ae p Na,8,0, a 
—1-4 745 6-7 0°7842 
—05 73 0°8160 
+2°4 91 1:0172 
58 114 1:2473 
1 cc. =0:0127 gm. iodine. 
Nickel and Sodium Chlorides.—Chlorine hydrate appeared at_ 2°. = ‘iite 
curve falls between those of the two single salts on both sides of the maximum, 
but lies nearer the curve for sodium chloride. It shows the flat top character- 
istic of the nickel chloride curve. ; 
1(NiCl,+NaCl). Plate XXXVL, Diagram vu. 
E 
p Na,S,0, a 
—155 7646 11°85 315i. 
—03 12-4 13761 
ee 14-1 15648 
3°5 17-9 1:9865 
8-0 17°6 (2) 19532 
11:3 17°8 1:9754 
16-0 14:8 16425 
24:5 11:3 12541 
29-0 8:3 0-9211. 
1 c.c =0:0127 gm. iodine. 
Strontium and Sodium Chlorides.—Chlorine hydrate appeared at —3°, began 
to decompose at 2°°6, and had completely disappeared at 5°°6. The curve lies 
-above those of the single salts before the maximum, afterwards falls between 
them. 
2(SrCl, + NaCl). 
p Na,S,0, ie F 
—3'0 766°7 11°6 1:2838 
—16 119 13170 
0:0 13°6 15052 
+2°6 14:7 16269 
5°6 165 18261 
7:0 15:0 16601 
9°5 12°7 1:4056 
14:3 10°5 11621 
22°8 85 09407 
28:7 72 0:7968 
373 56 06198 
Discussion of Results.—In discussing these results it must be premised that 
the curves are not strictly comparable after the maximum point is passed in 
