Article
Molecular dynamics simulations of water molecule-bridges in polar domains of humic acids.
Institute of Soil Research, University of Natural Resources and Applied Life Sciences Vienna , Peter-Jordan-Strasse 82, A-1190 Vienna, Austria.
Environmental Science & Technology (impact factor:
4.8).
08/2011;
45(19):8411-9.
DOI:10.1021/es201831g
pp.8411-9
Source: PubMed
- Citations (40)
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Cited In (0)
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Article: Sorption equilibrium of a wide spectrum of organic vapors in Leonardite humic acid: experimental setup and experimental data.
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ABSTRACT: The environmental fate of volatile and semivolatile organic compounds is determined by their partitioning between air and soil constituents, in particular soil organic matter (SOM). While there are many studies on the partitioning of nonpolar compounds between water and SOM, data on sorption of polar compounds and data for sorption from the gas phase are rather limited. In this study, Leonardite humic acid/air partition coefficients for 188 polar and nonpolar organic compounds at temperatures between 5 and 75 degrees C and relative humidities between < 0.01% and 98% have been determined using a dynamic flow-through technique. To the best of our knowledge, this is by far the largest and most diverse and consistent data set for sorption into humic material published so far. The major results are as follows: the relative humidity affected the experimental partition coefficients by up to a factor of 3; polar compounds generally sorbed more strongly than nonpolar compounds due to H-bonding (electron donor/ acceptor interactions) with the humic acid; no glass transitions in the range of 5-75 degrees C that would be relevant with respect to the sorption behavior of hydrated Leonardite humic acid were observed; our experimental data agree well with experimental partition coefficients from various literature sources.Environmental Science and Technology 10/2006; 40(17):5368-73. · 5.23 Impact Factor -
Article: The air/surface adsorption equilibrium of organic compounds under ambient conditions
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ABSTRACT: The environmental fate of volatile and semivolatile organic pollu-tants strongly depends on their partitioning between the gas phase and condensed phases. This partitioning includes absorption in bulk phases like water or organic matter and adsorption on ambi-ent surfaces. Often, the latter process is neglected due to the limited knowledge of adsorption as compared to absorption. The first part of this work discusses how the adsorption equilibrium can be assessed as a function of surface and adsorbate properties, temperature, and relative humidity. It is shown that the traditional approach of correlating adsorption constants with the volatility of the con-sidered compounds or with their octanol/air partitioning does not provide a reasonable understanding of the experimental data. In-stead, a model is needed that is based on a simple description of the relevant intermolecular interactions. The second part of this work analyses the relative importance of adsorption to surfaces for the overall sorption of airborne organic compounds in the environ-ment. This discussion is focused on gas/particle partitioning and on the exchange between soil surfaces and the atmosphere.Critical Reviews in Environmental Science and Technology 05/2004; 1346(34):339-389. · 4.84 Impact Factor -
Article: A Distributed Reactivity Model for Sorption by Soils and Sediments. 8. Sorbent Organic Domains: Discovery of a Humic Acid Glass Transition and an Argument for a Polymer-Based Model
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ABSTRACT: Analysis of a humic acid by differential scanning calorimetry has revealed the existence of a glass transition point. Glass transition temperatures, Tg, of water-wet and desiccator-dry specimens were found to range from 43 °C for water-wet humic acid to 62 °C for dry samples. Phenanthrene sorption isotherms for these and other natural and synthetic organic matrices having known glass transition tempera tures were determined to exhibit linearity and nonlinearity corresponding respectively to the rubbery (expanded) and glassy (condensed) states of the sorbent. Invoking a limiting case of the distributed reactivity model based on polymer sorption theory, we explain the observed sorption behavior as comprised in each case by a linear phase-partitioning component and a Langmuir-like nonlinear adsorption component. We conclude that polymer sorption theory provides a useful context in which to assess sorption phenomena associated with soil and sediment organic matter, providing more accurate projections of contaminant behavior in environmental systems and better informed specifications of appropriate remediation measures.05/1997;
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Keywords
aliphatic chains
carboxylic groups
cluster region
cross-linking distant locations
force-field MD
four carboxyl groups
humic substances
hydrophilic groups
impedes removal
local water network
molecular dynamics
oligomer chains
organic matter matrix
polar region
pronounced cage effect
stabilizing factor
tetramer-water cluster
undecanoid fatty acids
water cluster
water molecules