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                           Table 4.2. Examples of correlations for the sorption of vapors at the water–gas interface
                           Equation               Nomenclature                 Reference  Ong
                             =−( p/RT)(dγ/dp)       – surface excess (mol cm −2 )  Gibbs equation (as
                                                  γ – surface tension          presented in Chattoraj
                                                  p – partial pressure         and Birdi, 1984)
                                                  R – universal gas constant
                                                  T – temperature
                           log K IW =−5.53 + 0.2735I x  K IW – water–gas partition coefficient,  Valsaraj (1988)
                                                  I x – first order molecular connectivity
                                                   index
                           log K IW =−8.58−0.769 log C s  K IW – water–gas partition coefficient  Hoff et al. (1993b)
                                               W
                                                   (m)
                                                  C s  – saturated solubility of the VOC
                                                    W
                                   ∗
                           ln K IW = A − ( H s /R)(1/T −  K IW – water–gas partition coefficient  Goss (1994)
                                  1/323.15) − C(100 −  (m), vp – vapor pressure (pascal), β –
                                  RH)(3) where     hydrogen bond acceptor, mR – molar
                             ∗                     refraction, µ – dipole momentum,
                            A =
                            −0.615 ln vp + 7.86ß − 5.80   H s – heat of adsorption (kJ mol −1 ) R
                            C =−0.054β − 0.00070 mR −  – universal gas constant (kJ
                                                        K
                            0.0041µ + 0.00061 H s =  mol −1 −1 )
                            3.20 ln vp − 50.2β − 55.0.


                           be a dominant retention mechanism depending on the moisture content (Costanza and
                           Brusseau, 2000). Obviously as the moisture content approaches saturation the water–
                           gas interface (A) available will be reduced resulting in insignificant sorption at the
                           water–gas interface. It must be pointed out that VOCs with high aqueous solubility
                           would prefer to be in the aqueous phase rather than at the water–gas interface. TCE
                           has an aqueous solubility of 1100 mg/L which is higher than the solubility of p-xylene
                           (198 mg/L). Therefore it is probable that because of the physical characteristic of the
                           TCE used by Ong and Lion (1991c), sorption at the water–gas interface was found to
                           be negligible.
                             Several researchers have proposed correlations for the estimation of mass sorbed
                           at the water–gas interface (see Table 4.2). Sorption at the water–gas interface can
                           be modeled using the Gibbs equation where the surface excess is determined by the
                           change in the surface tension with varying vapor pressure. The equations proposed
                           by Goss (1994) imply that for a VOC with high saturated solubility and high vapor
                           pressure vapors such as TCE, the air–water partition coefficients would be low and
                           that the VOC that are most likely to be sorbed at water–gas interface are those with
                           a high β, hydrogen bond acceptor, value.
                             MostvaporsorptionstudieswereconductedusingasingleVOCincompetitionwith
                           water for sorption sites. There are only a few studies investigating sorption of multiple
                           vapors under unsaturated zone conditions even though many different VOCs may be
                           found at a typical contaminated site. For simplicity sake, it is assumed that each VOC
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