( 548 ) 



T\ pA Bi ] 



^ . I'i ( ^^ ^ ) 



it" y>, ;ni(l- /^, avo cxprossrd i]i atmosplioro 'O ('.45' iKnilin'ii l.iiitiidoV 

 A Sf'CDiid ,i)i|ti()\iiii;ili(ni w liorc' tlic (•(icrficiciit ('\ would occiii' is 

 )i(»l iiocossarv ^^illl a \i('\N' to the acciiracv i-(M|iiii-ed. 



TABLE Xa. 



TAHLE \h. 



A 



B 



^ I 



I 



) 8.878 



I 



1.8913 ' i.SüKi 



( t . 1 ( I 



1 .'.«!»( ; 1 O'iOO + 0.022 



I -— 5 j 1.2422 1.252(1' - n.();2 



I ^4 ! 



Table X sli()\N> tlic i-('sidl> of tlic caliitralion. There \\'<' lia\e 

 called; r„ llie \(tliiiiie al>t>\(' FJi^^. 1', iIm' <>iie al)()\"e 7;//., 1"., llie 

 Olie al»o\(' A'A„ ele. C'oliiinii .1 of talile \(i uiNcs tlie relalioii> ot 

 flie vuliinies aeeoi'diiiü lo ilic iiiereiii-\ ealihratioii, l» aeeordiiiu If» 

 the \-ohiiiieiioiiicli-ical dclcriiiiiiatioii. (' Ihe |»ei-ceiila,ue diirereiiees. 

 Coluiiiii l] of laUle XA Lii\c> llic i'elalioii of tin- noIiiihc of 1 mm. 

 of the iiidiealed l»oi-c U» llie ciiliic xoliimc ahoxe il. Jt mav he seen 

 that the aüreemeiit helweeii the Iwo calihi-atioiis is sidïieient. In 

 followiiiu- calcnlalifdis the mcreuiv calihi-atioii lia> hecii ado})ted as 

 being the more aeeurate. 



For the eaU'idatioii of Ihe composition we derive from the meas- 

 urements in the \ olnmeiioinefeithila. as those for the mi.vtnre (^.2 

 (oxygen in carbon dioxide ai'e combined in fable XI. .1 contains tlie 

 data of the oxvgen in the \ohnneJionieter. l'> i-efei> to the o.\yi>eii 

 whieh has remained in E after the transferejice of the greater part 

 into F^ C refers to the carbon dioxide. 



T ABLE XL 



A 



B 



Vnlmii.' i 0.99979 F^ 



PressuPH i().H9() 



TiinipiTiitiui' ID.xi 



0.9890.") /'„ I 0.99994 F^ 



().:'.S(i (■>(■>. '.lO! 



)'.).. ")3 19.83 



