“…Values of V 1 2 =V Ã 1 for aqueous CO 2 , evaluated from EoS (Duan and Zhang, 2006), see text. Alexander and Hill, 1965;Friedman and Scheraga, 1965;Franks and Smith, 1968;Neal and Goring, 1970;Nakajima et al, 1975;Høiland and Vikingstad, 1976;Moriyoshi et al, 1977;Benson and Kiyohara, 1980;Høiland, 1980;Nakagawa et al, 1983;Easteal and Woolf, 1985;Makhatadze and Privalov, 1989;Makhatadze et al, 1990Makhatadze et al, , 1997Ott et al, 1993;Alauddin et al, 1994;Sakurai et al, 1994;Kaulgud et al, 1995;Criss and Wood, 1996;Hynek et al, 1997;Xiao et al, 1997;Degrange, 1998;Hnědkovský et al, 1998;Saleh et al, 1998;Schulte et al, 1999;Origlia and Woolley, 2001;Kukuljan et al, 2003;Hynćica et al, 2004Hynćica et al, , 2006aStříteská et al, 2004;Č enský et al, 2007;Cibulka and Hnědkovský, 2009). Here and in all later cases only data at T > 293 K were used, because results at lower temperatures and atmospheric pressure complicate the dependence (those practically isochoric data demonstrate an appreciable temperature dependence, contrary to data at higher temperatures).…”