166 A. W. Wright—Gases contained in Meteorites, 
e 
suilicient to mention that, as the meteorite gives 
I e 
Kold Bokkeveld. 
: co Sn N. 
300°-350° 87°34 5°08 = 55°93 trace? «1°65 = 7°45 
500° 95°53 P82 914 004? 047 1 
Total. 93°11 2-42 325 0-38? 0°84 25°23 
e volume of the gases obtained is much greater in this 
than in the previous determinations; but it will be seen that 
The percentage of carbon di-oxide is somewhat larger at the 
higher temperature than in the other cases, but the real differ- 
that 1s, with more carbon atoms than are contained in I- 
Bas, might be found. But both the analyses, and special “ 
Die chemische Natur der Meteoriten. Abhandl. der Konig!. 
