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Modelling Aqueous Solubility of Sodium Chloride in Clays at Thermodynamic Conditions of Hydraulic Fracturing by Molecular Simulations.

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    SYSNO ASEP0475871
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleModelling Aqueous Solubility of Sodium Chloride in Clays at Thermodynamic Conditions of Hydraulic Fracturing by Molecular Simulations.
    Author(s) Moučka, Filip (UCHP-M) RID, ORCID, SAI
    Svoboda, Martin (UCHP-M) RID, SAI, ORCID
    Lísal, Martin (UCHP-M) RID, ORCID, SAI
    Source TitlePhysical Chemistry Chemical Physics. - : Royal Society of Chemistry - ISSN 1463-9076
    Roč. 19, JUL 7 (2017), s. 16586-16599
    Number of pages14 s.
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsmolecular simulation ; Monte Carlo (GCMC) technique ; clay pores
    Subject RIVCF - Physical ; Theoretical Chemistry
    OECD categoryPhysical chemistry
    R&D ProjectsGA16-12291S GA ČR - Czech Science Foundation (CSF)
    Institutional supportUCHP-M - RVO:67985858
    UT WOS000404530600031
    EID SCOPUS85024120633
    DOI10.1039/c7cp02121f
    AnnotationTo address the high salinity of flow-back water during hydraulic fracturing, we have studied the equilibrium partitioning of NaCl and water between the bulk phase and clay pores. In shale rocks, such a partitioning can occur between fractures with a bulk-like phase and clay pores. We use an advanced Grand Canonical Monte Carlo (GCMC) technique based on fractional exchanges of dissolved ions and water molecules. We consider a typical shale gas reservoir condition of a temperature of 365 K and
    pressure of 275 bar, and we represent clay pores by pyrophyllite and Na-montmorillonite slits of a width ranging from about 7 to 28 Å, covering clay pores from dry clay to clay pores with a bulk-like layer in the middle of the pore. We employ the Joung–Cheatham model for ions, SPC/E model for water and CLAYFF for the clay pores. We first determine the chemical potentials for NaCl and water in the bulk phase using Osmotic Ensemble Monte Carlo simulations. The chemical potentials are then used in GCMC to simulate the adsorption of ions and water molecules in the clay pores, and in turn to predict the salt solubility in confined solutions. Besides the thermodynamic properties, we evaluate the structure and in-plane diffusion of the adsorbed fluids, and ion conductivities.
    WorkplaceInstitute of Chemical Process Fundamentals
    ContactEva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227
    Year of Publishing2018
Number of the records: 1  

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