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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 ASEP 0475871 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Modelling 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, SAISource Title Physical Chemistry Chemical Physics. - : Royal Society of Chemistry - ISSN 1463-9076
Roč. 19, JUL 7 (2017), s. 16586-16599Number of pages 14 s. Language eng - English Country GB - United Kingdom Keywords molecular simulation ; Monte Carlo (GCMC) technique ; clay pores Subject RIV CF - Physical ; Theoretical Chemistry OECD category Physical chemistry R&D Projects GA16-12291S GA ČR - Czech Science Foundation (CSF) Institutional support UCHP-M - RVO:67985858 UT WOS 000404530600031 EID SCOPUS 85024120633 DOI 10.1039/c7cp02121f Annotation To 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.Workplace Institute of Chemical Process Fundamentals Contact Eva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227 Year of Publishing 2018
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