Although microporosity and surface area of natural organic matter (NOM) are crucial for mechanistic evaluation of the sorption process for nonpolar organic contaminants (NOCs), they have been underestimated by the N 2 adsorption technique. We investigated the CO 2 -derived internal hydrophobic microporosity (V o ) and specifi c surface area (SSA) obtained on dry samples and related them to sorption behaviors of NOCs in water for a wide range of condensed NOM samples. Th e V o is obtained from the total CO 2 -derived microporosity by subtracting out the contribution of the outer surfaces of minerals and NOM using N 2 adsorption-derived parameters. Th e correlation between V o or CO 2 -SSA and fractional organic carbon content (f OC ) is very signifi cant, demonstrating that much of the microporosity is associated with internal NOM matrices. Th e average V o and CO 2 -SSA are, respectively, 75.1 μL g −1 organic carbon (OC) and 185 m 2 g −1 OC from the correlation analysis. Th e rigid aliphatic carbon signifi cantly contributes to the microporosity of the Pahokee peat. A strong linear correlation is demonstrated between V 0 /f OC and the OC-normalized sorption capacity at the liquid or subcooled liquid-state water solubility calculated via the Freundlich equation for each of four NOCs (phenanthrene, naphthalene, 1,3,5-trichlorobenzene, and 1,2-dichlorobenzene). We concluded that micropore fi lling ("adsorption") contributes to NOC sorption by condensed NOM, but the exact contribution requires knowing the relationship between the dry-state, CO 2 -determined microporosity and the wet-state, NOC-available microporosity of the organic matter. Th e fi ndings off er new clues for explaining the nonideal sorption behaviors of NOCs.
Evidence of Micropore Filling for Sorption of Nonpolar Organic Contaminants by Condensed Organic MatterYong Ran,* Yu Yang, Baoshan Xing, Joseph J. Pignatello, Seokjoo Kwon, Wei Su, and Li Zhou S orption and sequestration of nonpolar organic contaminants (NOCs) by natural organic matter (NOM) associated with aquifers, soils, and sediments control the bioavailability, risk, and fate of NOCs (Pignatello and Xing, 1996;Luthy et al., 1997;Brusseau et al., 1991). However, the physicochemical mechanisms of sorption/desorption and reduced bioavailability for NOCs remain unclear. Some investigators have recognized the importance of organic matter porosity and surface properties in controlling the magnitude and rates of sorption (Pignatello and Xing, 1996;Kleineidam et al., 2002;Nam and Alexander, 1998;Li and Werth, 2001;Ran et al., 2002Ran et al., , 2004.Th e chemical, structural, and surface heterogeneity of NOM may strongly infl uence NOC sorption and desorption rates and equilibria in soils and sediments (Pignatello and Xing, 1996;Luthy et al., 1997;Ran et al., 2004). Natural organic matter has been characterized as comprising multiple domains or components, some of which can be characterized as partitioning phases and others as pore-fi lling phases (Xing and Pignatello, 1997;Weber and Huang, 1996;Ra...