19 December 2012 4 4K Report

Most of the earliest determinations of CO2 concentrations were by chemical analysis of dried atmospheric air through absorption by alkalis such as Ba(OH)2 and subsequent titration. A known volume of air was usually dried by passing it through U-tubes of concentrated H2SO4 before entering the main flask where the CO2 was to be absorbed by the alkali.

Hlasiwetz (1856) Ueber Kohlensäure-Bestimmungen der Atmosphärischen Luft (link given below) mentions the possibility that some of the CO2 might be absorbed by the H2SO4 before entering the flask; this would obviously make the determination of the CO2 concentration unreliably low.

I have consulted the IUPAC-NIST Solubility Database http://srdata.nist.gov/solubility/ , entered the search menu on the left-hand side, and then chose the two system component sub-menu http://srdata.nist.gov/solubility/comp2MolFmls.aspx , entering the two search strings: CO2 and H2SO4.

The result http://srdata.nist.gov/solubility/sol_2casno.aspx?STR1=CO2&STR2=H2SO4&OPTION=MOL gives seven possible hits (click on the "system", not on the CAS No.), but two of them also involve Na2SO4, and so are probably not relevant. The remaining five are the results of five different investigations carried out between 1877 and 1957, but I cannot understand any of them (my knowledge of the topic/terminology is insufficient at this level!)

Can someone help me to understand what they mean? Is CO2 likely to be absorbed into concentrated H2SO4 from air at typical ambient temperatures and humidities, and if so, to what extent? How might this absorption vary with different conditions (temp., pressure, etc) How might this have compromised the accuracy of the determinations of [CO2]?

http://books.google.co.uk/books?hl=en&lr=&id=gJo5AAAAcAAJ&oi=fnd&pg=PA1&dq=hlasiwetz+kohlensaurebestimmungen&ots=eft7yDl2pE&sig=p7QuBnmSNsYaD0w_u-AyPw6qC0Y#v=onepage&q&f=false

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