{"refrec":{"BRefID":219531,"RR":"<b>Geilfus, N.-X.; Delille, B.; Verbeke, V.; Tison, J.-L.</b> (2012). Towards a method for high vertical resolution measurements of the partial pressure of CO<sub>2</sub> within bulk sea ice. <i>J. Glaciol. 58(208)</i>: 287-300. <a href=\"https://dx.doi.org/10.3189/2012JoG11J071\" target=\"_blank\">https://dx.doi.org/10.3189/2012JoG11J071</a>","BEntID":211265,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Glaciol. 58(208)</i>: 287-300. <a href=\"https://dx.doi.org/10.3189/2012JoG11J071\" target=\"_blank\">https://dx.doi.org/10.3189/2012JoG11J071</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Geilfus, N.-X.; Delille, B.; Verbeke, V.; Tison, J.-L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Geilfus, N.-X. <i>et al.</i>","Englishabstract":"Fluxes of atmospheric CO<SUB>2</SUB> have been reported over sea ice during winter and spring. These fluxes are partly driven by the gradient of the CO<SUB>2</SUB> concentration between sea ice and the atmosphere. We present a new non-destructive method to measure the pCO<SUB>2</SUB> of bulk sea ice at its in situ temperature. This method is based on an equilibration procedure between sea ice and a standard gas of known CO<SUB>2</SUB> concentration. The concentration is measured by gas chromatography with a precision of 5%. Tests were performed on artificial standard sea ice and confirmed the reproducibility of the technique in the range of precision of the gas chromatograph. 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