296 University Geological Survey of Kaasas. 
39 Andrews. Composition of an inflammable gas issuing from a 
1874 silt bed in Belfast, Ireland. 2?! 
4 Bishop’s Chem. Geol. Composition of gas issuing from marsh 
1885 ground. 222 
56 Charitschkof. Analysis of combustible gas evolved in the Cas- 
1902 pian Sea, near the Gulf of Baku.224- Two samples. 
TABLE No. 39. 
GASES FROM RIVERS, LAKES, MARSHES, ETC. 
24a 246 279, 2792 29a 29b 29¢ 29d 29e 
es) w Q RQ RQ < a} 
we | os Qi} | fee Be | Pallas 
ae) oso act oc 0 a! ro) 
@" | 2. | Marsh-gas at wate a g 2O 5 
5 s ws S Marburg oS = < o ge 2 
: = ae ~ Botanical 5 RE n 5 mn 
ms 00 a Gardens. ae 2:8 = a Q| 
f | 3s ei Se] S ge | & 
O 5 ® & oS _ : 
® : 
Methane Yiacoccecne 48.4 42.5 47.37 76.61 83.6 95.5 90.4 POOR 5.0 
| Od at «anes eee | Mion nitnnn naneeal laa coColllbad gacoclsocoona Noame tana (crmeeerei el neeoee nic 
Bthylene:...3c2ende: 6.3 Roll GAB ETA SRG Dcclilno0a 65 dollooo 668 4.4 tees ene eee nee aen ee oe 
Carbon dioxid. ...... 18.0 8.5 3.10 5.86 4.2 Boll 2 67.0 90.7 
Carbon monoxid...... 14.2 7A Wate el eG Mero Gol lladoo Goo olla Odo aco | GOR Str] Peete teten REN 
Oxygen. fo) soy. ees 0.3 0.4 One ee SS lll eee tae LY 10 0.5 1.0 
Ey drowen epee 10 0 VS S80 Madera csroxsisiell voveyeeeseereeel| | PREM LITE ere er eerel | erro acl eres [evens «ti overs ll oosetavaovere 
INITEROERE0 5 06000000000 2.8 1.9 49.39 18.08 A VASO ATS iene GAG een orors 3.3 
Py drowen sulfide siice-c| iscke.sce octal Gystoractave cl alate taney | epee || CAE OB 2Blleesrreretes |usectagetciesal eteseeocelswer 
‘Rotalsiateseceae 100.0 | 100.0 | 100.08 | 100.00 100.0 | 100.0 100.0 100.0 100.0 
TABLE No. 39—CONCLUDED. 
297 29g 29h 297 4 39 o6a d6b 
> Ht Es = Q wn a a 
9 | 22 | ee | aS | ee | we | ee | ae 
ae 3.0 Rs Bs S th Oy Gc %. 
3 Eo oS eae a8 © Oo © Ws 
Big < &, Sols, pe 3 g 3 2 I) 2.5 
Sh | 3c) | 2s | be | & roy |) aie) ie 
Aes | Sh | ae ee | se | ee ee 
cn gs | S cr B 2 | 8s @ Q 
2 iia ee 
Methanes stad sath cbse Oaiean ne 0.7 73.7 41.0 47.387 83.75 | 96.28 95.17 
IOLA ha: ere er non Incmmena lesa oonulles coooddlliboobccoolllaogcoddu OROOM serra ts eta eae 
1 Diy chid(-10(: eee oar ennl ane arcs Ging oanadlamooooodloboddscclllaccddoas QROOR RAs coil \cenaniees 
Carbonidioxid eeeeeeeree Een 93.2 94.7 0.7 0.3 3.10 DAA ee Darrah intra 
Bi hel ovoy abs ato 010) ¢ (6 (ered! eee (Pee Hall ae ab ol ldadoodoclllovoSbo.ce lodesaood loaeere | Ieee eens 
ORV SEONG isos ore eeioe eee 0 iL dl 5 7 12.3 0.17 OG HI Beecstracea | eevcrserers 
1 ico boyenc1 a eee er an Ib Antennal eo cl lomoen cocloeoo 06 oalllocina coo dlloooonbod toeonnou boomncoe 
INitrovencic sete Ree 5.8 BH 20.4 46.4 49.39 12.75 3.72 4.83 
DER Zopoysa:) ale=10 | bats RRP Meee een [RRM eel Lenn AL. Fe aa ona allooscoedollmosodunnllagage Gaol cone te Sa aaeee s 
Totalsiecsentawtwvecmentee ee 100.0 100.0 100.0 100.0 |} 100.08 | 100.00 | 100.00 100.00 
46 Fouquéand Gorceix. Analysesofa series of gases partly from the 
1869 Tuscan Lagoons (Lagonian Toscanio), partly from the Apennines. 223 
Many of the gases also contain traces of higher hydrocarbons, as 
is shown by the odor. 
221. Chem. News 30, 138, 1874. 
222. Bishop’s Chem. Geol. I, 730. 
223. Compt. Rendus 69, 946; Jahresbericht 1869, p. 1276. 
224. J. Russ. Phys. Chem. Soc. 1902, 34, 712-713. 
