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

ABSTRACT The stabilizing effect of water molecule bridges on polar regions in humic substances (HSs) has been investigated by means of molecular dynamics (MD) simulations. The purpose of these investigations was to show the effect of water molecular bridges (WAMB) for cross-linking distant locations of hydrophilic groups. For this purpose, a tetramer of undecanoid fatty acids connected to a network of water molecules has been constructed, which serve as a model for spatially fixed aliphatic chains in HSs terminated by a polar (carboxyl) group. The effect of environmental polarity has been investigated by using solvents of low and medium polarity in force-field MD. A nonpolar environment simulated by n-hexane was chosen to mimic the stability of WAMB in a hydrophilic hotspot surrounded by a nonpolar environment, while the more polar acetonitrile environment was chosen to simulate a more even distribution of polarity around the carboxylic groups and the water molecules. The dynamics simulations show that the rigidity of the oligomer chains is significantly enhanced as soon as the water cluster is large enough to comprise all four carboxyl groups. Increasing the temperature leads to evaporization processes which destabilize the rigidity of the tetramer-water cluster. Embedding it into the nonpolar environment introduces a pronounced cage effect which significantly impedes removal of water molecules from the cluster region. On the other hand, a polar environment facilitates their diffusion from the polar region. One important consequence of these simulations is that although the local water network is the stabilizing factor for the organic matter matrix, the degree of stabilization is additionally affected by the presence of nonpolar surroundings.

0 0
 · 
0 Bookmarks
 · 
63 Views
  • Article: Sorption equilibrium of a wide spectrum of organic vapors in Leonardite humic acid: experimental setup and experimental data.
    [show abstract] [hide abstract]
    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
  • Source
    Article: The air/surface adsorption equilibrium of organic compounds under ambient conditions
    [show abstract] [hide abstract]
    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
    [show abstract] [hide abstract]
    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;

Full-text

View
1 Download
Available from

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