|
|
||||||||
a Dep. of Geology and Geophysics, Texas A&M Univ., College Station, TX 77843
b Dep. of Agricultural and Biological Engineering, Clemson Univ., Clemson, SC 29634-0357, and Dep. of Environmental Toxicology and the Clemson Institute of Environmental Toxicology, Clemson Univ., Pendleton, SC 29670
* Corresponding author (Don.Zhu{at}po.state.ct.us)
Received for publication April 22, 2002.
Molecular-level sorption behavior of monoaromatic compounds in suspensions of water-dispersable clay components was studied by measuring 2H nuclear magnetic resonance (NMR) spinspin relaxation times (T2). In general, decreased T2 values indicate stronger solutesorbent interactions and increased sorption of the solute. A decreasing trend for T2 values in the order benzene > fluorobenzene > toluene (-C6D5 moiety) was observed, which was probably caused by the hydrophobic effect. The T2 values for benzene and the -C6D5 moiety of toluene increased with increasing pH, whereas the trend with pH was much weaker and less consistent for fluorobenzene and the methyl group of toluene. Conversely, no clear relationship was found between T2 values and pH for dichloromethane. These contrasting results cannot be explained by the pH-dependent self-assembly and hydrophobicity of humics. Instead, directed specific forces, including hydrogen bonding, cation
interactions, and aromaticaromatic interactions, are proposed between the benzene ring of monoaromatic solutes and soil organic matter (SOM). Substituents of benzene affect these interactions by varying the
electron density. When the soil fraction was treated with NaOH to remove humic and fulvic acids, T2 values for the different monoaromatic solutes were surprisingly lower compared with those for the untreated soil fraction. This result is probably caused by the increased ratio of solutes adsorbed to "hard" or "glassy" SOM components, which leads to less mobile sorbed solute molecules, after removing NaOH-extractable humics that contain more "soft" or "rubbery" SOM components.
Abbreviations: NMR, nuclear magnetic resonance NOC, nonionic organic chemical PAH, polycyclic aromatic hydrocarbon SOM, soil organic matter T1, spinlattice relaxation times T2, spinspin relaxation times
This article has been cited by other articles:
![]() |
D. Zhu, B. E. Herbert, M. A. Schlautman, E. R. Carraway, and J. Hur Cation-{pi} Bonding: A New Perspective on the Sorption of Polycyclic Aromatic Hydrocarbons to Mineral Surfaces J. Environ. Qual., July 1, 2004; 33(4): 1322 - 1330. [Abstract] [Full Text] [PDF] |
||||
![]() |
D. Zhu, B. E. Herbert, M. A. Schlautman, and E. R. Carraway Characterization of Cation-{pi} Interactions in Aqueous Solution Using Deuterium Nuclear Magnetic Resonance Spectroscopy J. Environ. Qual., January 1, 2004; 33(1): 276 - 284. [Abstract] [Full Text] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Soil Science Society of America Journal | Journal of Plant Registrations | The Plant Genome | |||