An X-ray and Neutron Scattering Study of Aqueous MgCl2 Solution in the Gigapascal Pressure Range

Author:

Yamaguchi Toshio12,Fukuyama Nami2,Yoshida Koji2ORCID,Katayama Yoshinori3,Machida Shinichi4,Hattori Takanori5ORCID

Affiliation:

1. Key Laboratory of Salt Lake Resources Chemistry of Qinghai Province, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China

2. Department of Chemistry, Faculty of Science, Fukuoka University, Jonan 814-0180, Fukuoka, Japan

3. Synchrotron Radiation Research Center, National Institutes for Quantum and Radiological Science and Technology, Sayo 679-5148, Hyogo, Japan

4. Neutron Science and Technology Center, Comprehensive Research Organization for Science and Society, 162-1, Shirakata 319-1106, Tokai, Japan

5. J-PARC Center, Japan Atomic Energy Agency, 2–4, Shirakata 319-1195, Tokai, Japan

Abstract

The structure of electrolyte solutions under pressure at a molecular level is a crucial issue in the fundamental science of understanding the nature of ion solvation and association and application fields, such as geological processes on the Earth, pressure-induced protein denaturation, and supercritical water technology. We report the structure of an aqueous 2 m (=mol kg−1) MgCl2 solution at pressures from 0.1 MPa to 4 GPa and temperatures from 300 to 500 K revealed by X-ray- and neutron-scattering measurements. The scattering data are analyzed by empirical potential structure refinement (EPSR) modeling to derive the pair distribution functions, coordination number distributions, angle distributions, and spatial density functions (3D structure) as a function of pressure and temperature. Mg2+ forms rigid solvation shells extended to the third shell; the first solvation shell of six-fold octahedral coordination with about six water molecules at 0 GPa transforms into about five water molecules and one Cl− due to the formation of the contact ion pairs in the GPa pressure range. The Cl− solvation shows a substantial pressure dependence; the coordination number of a water oxygen atom around Cl− increases from 8 at 0.1 MPa/300 K to 10 at 4 GPa/500 K. The solvent water transforms the tetrahedral network structure at 0.1 MPa/300 K to a densely packed structure in the GPa pressure range; the number of water oxygen atoms around a central water molecule gradually increases from 4.6 at 0.1 MPa/298 K to 8.4 at 4 GPa/500 K.

Funder

JSPS KAKENHI

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences,General Environmental Science

Cited by 2 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Development of 0.5 mm gauge size radial collimators for high-pressure neutron diffraction experiments at PLANET in J-PARC;Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment;2024-02

2. Historical development of a study of the structure and dynamics of liquids and solutions;Journal of Molecular Liquids;2024-02

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