Document Type

Article

Publication Date

2013

DOI

10.1016/j.geoderma.2013.04.008

Publication Title

Geoderma

Volume

204

Pages

68-74

Abstract

Although microporosity and surface area of natural organic matter (NOM) are crucial to mechanistic evaluation of the sorption process for nonpolar organic contaminants (NOCs), they have wrongly been estimated by the N2 adsorption technique. Nuclear magnetic resonance spectroscopy (13C NMR), and benzene, carbon dioxide, and nitrogen adsorption techniques were used to characterize structural and surface properties for different condensed NOM samples, which were related to the sorption behavior of phenanthrene (Phen). It was found that the revised Freundlich model by taking the chemical activity into account can well describe the isotherms for benzene and Phen. The benzene and Phen adsorption volumes for the coal samples are similar to or lower than the CO2-nanopore volumes. Adsorption volumes of both benzene and Phen are significantly related to the aliphatic carbon structure, and their correlation lines are nearly overlapped, suggesting that the nanopore filling for Phen and benzene on the investigated samples is the dominating mechanism, and also is not affected by water molecules. The entrapment of benzene and/or the pore deformation in the NOM nanopore are likely responsible for the observed hysteresis of benzene. The above results demonstrate that Phen and benzene adsorption on the condensed NOM is closely associated with the aliphatic carbon structure of the investigated samples.

Comments

Supported by a "Team Project" of the National Natural Science Foundation of China (41073082 and 41121063).

Per Sherpa Juliet, National Natural Science Foundation of China requires Open Access Archiving in appropriate institutional repository.

Original Publication Citation

Sun, K., Ran, Y., Yang, Y., Xing, B. S., & Mao, J. D. (2013). Interaction mechanism of benzene and phenanthrene in condensed organic matter: Importance of adsorption (nanopore-filling). Geoderma, 204, 68-74. doi:10.1016/j.geoderma.2013.04.008

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