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  1. Slow diffusional dynamics of water in cement nanopores: Multiscale challenges for atomistic modeling (topic leader)
    Erschienen: 2012
    Verlag:  HAL CCSD

    Molecular modeling of the properties of aqueous solutions confined in the nanopores and at the interfaces of cementitious materials is complicated by the significant structural and compositional heterogeneity of these phases and also by the fact that... mehr

     

    Molecular modeling of the properties of aqueous solutions confined in the nanopores and at the interfaces of cementitious materials is complicated by the significant structural and compositional heterogeneity of these phases and also by the fact that many of the important processes span several orders of magnitude both in time and in length. Here we present an attempt to quantify the diffusional dynamics of 0.25 M KCl aqueous solution in contact with a model C-S-H binding phase (tobermorite) on the basis of molecular dynamics computer simulations. At the (001) surface of tobermorite, two types of H2O molecules can be effectively distinguished: the ones that spend most of their time within channels between the drierketten chains of silica on the tobermorite surface, and the more mobile adsorbed molecules that reside right above the interface. Within the channels, H2O molecules donate H-bonds to both the bridging and non-bridging oxygens of the Si-tetrahedra as well as to other H2O. Some of these molecules form particularly strong H-bonds persisting well over 100 ps, but many others undergo frequent librational motions and occasional diffusional jumps from one surface site to another. The average diffusion coefficients of the surface-associated H2O molecules that spend most of their time in the channels and those that lie above the nominal interface differ by about one order of magnitude (DH2O[internal]=5.0×10−11 m2/s and DH2O[external]=6.0×10−10 m2/s, respectively). The average diffusion coefficient for all surface-associated H2O molecules is about 1.0×10−10 m2/s. All of these values are significantly less than the value of 2.3×10−9 m2/s, characteristic of H2O self-diffusion in bulk liquid water. The MD simulations provided an opportunity to further quantify these relatively slow diffusional motions of H2O at the tobermorite interface on the longer time- and length- scale in terms of the Van Hove self-correlation function (VHSCF). The emerging picture is in surprisingly good agreement with available experimental data on the dynamics of surface-associated water in similar cement materials obtained by 1H NMR [1,2]. 1. Korb J.P., Monteilhet L., McDonald P.J., Mitchell J., Microstructure and texture of hydrated cement-based materials: A proton field cycling relaxometry approach. Cement and Concrete Research, 37, 2007, 295-302. 2. Korb J.P., NMR and nuclear spin relaxation of cement and concrete materialsCurrent Opinion in Colloid & Interface Science, 14, 2009, 192-202.

     

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    Quelle: BASE Fachausschnitt AVL
    Sprache: Englisch
    Medientyp: Konferenzveröffentlichung
    Format: Online
    Übergeordneter Titel: International US-Poland Workshop "Multiscale Computational Modeling of Cementitious Materials" ; http://hal.in2p3.fr/in2p3-00769185 ; International US-Poland Workshop "Multiscale Computational Modeling of Cementitious Materials", Oct 2012, Kraków, Poland
    Schlagworte: [CHIM.THEO]Chemical Sciences/Theoretical and/or physical chemistry; [CHIM.MATE]Chemical Sciences/Material chemistry; [SDE.IE]Environmental Sciences/Environmental Engineering; [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; [SDE.MCG]Environmental Sciences/Global Changes; [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
  2. Structure and Energetics of Smectite Interlayer Hydration: Molecular Dynamics Investigations of Na- and Ca Hectorite

    Molecular-scale interactions present at mineral-water interfaces and in clay interlayer galleries control numerous environmental processes, including chemical interactions in soils and transport of nutrients and pollutants through them.[1-4]... mehr

     

    Molecular-scale interactions present at mineral-water interfaces and in clay interlayer galleries control numerous environmental processes, including chemical interactions in soils and transport of nutrients and pollutants through them.[1-4] Understanding these processes requires accurate knowledge of the structure, energetics, and dynamics of the interaction among the mineral substrate, ions, and water molecules.[5, 6] Challenges to this objective include experimental difficulties in probing these interfaces and interlayers at the molecular scale; fully characterizing the mineral substrate; and identifying how the mineral surface, ions, and water molecules each contribute to the overall structure, energetics, and dynamics of these systems.[6] Linked computational molecular dynamics (MD) simulations and experimental nuclear magnetic resonance (NMR) studies are particularly effective in addressing these issues.[7-9] Here we focus on MD studies of Na- and Ca-smectite (hectorite) interlayer galleries to provide a molecular-scale picture of the structure and dynamics of their hydration[9, 10] and to complement our earlier NMR investigations of these systems.[7-9] Classical MD simulations were undertaken in the NPT and NVT ensembles to determine the structural and energetic changes with increasing hydration with focus on the single- and double-layer hydrates. The results show substantial changes in the hydration of the interlayer cations, the orientations of the water molecules, the hydrogen bond network involving the water molecules and basal oxygen atoms, and the resulting potential energies as the interlayer gallery expands. [1] Scheidegger et al. (1996) Soil Science 161 813-831. [2] Stumm (1997) Colloids and Surfaces A-Physicochemical and Engineering Aspects 120 143-166. [3] O'Day (1999) Reviews of Geophysics 37 249-274. [4] Koretsky (2000) Journal of Hydrology 230 127-171. [5] Wang et al. (2001) Chemistry of Materials 13 145-150. [6] Wang et al. (2006) Geochimica et Cosmochimica Acta 70 562-582. [7] Bowers et al. (2008) Journal of Physical Chemistry C 112 6430-6438. [8] Bowers et al. (2011) Journal of Physical Chemistry C 115 23395-23407. [9] Bowers et al. (2012), unpublished. [10] Morrow et al. (2012) Journal of Physical Chemistry C, submitted.

     

    Export in Literaturverwaltung
    Quelle: BASE Fachausschnitt AVL
    Sprache: Englisch
    Medientyp: Konferenzveröffentlichung; Weitere
    Format: Online
    Übergeordneter Titel: Symposium 8g: Structure and dynamics of ions and water at mineral-water interfaces: insights from experimental and computational studies, 2012 Goldschmidt Conference ; http://hal.in2p3.fr/in2p3-00769208 ; Symposium 8g: Structure and dynamics of ions and water at mineral-water interfaces: insights from experimental and computational studies, 2012 Goldschmidt Conference, Jun 2012, Montreal, Canada
    Schlagworte: [CHIM.THEO]Chemical Sciences/Theoretical and/or physical chemistry; [CHIM.MATE]Chemical Sciences/Material chemistry; [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; [SDE.MCG]Environmental Sciences/Global Changes; [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy