Influence of CO2 on Nanoconfined Water in a Clay Mineral

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

Influence of CO2 on Nanoconfined Water in a Clay Mineral. / Hunvik, Kristoffer W. Bo; Lima, Rodrigo Jose da Silva; Kirch, Alexsandro; Loch, Patrick; Roren, Paul Monceyron; Petersen, Martin Hoffmann; Rudic, Svemir; Sakai, Victoria Garcia; Knudsen, Kenneth Dahl; Instituto, Caetano Rodrigues Miranda Materiais; Breu, Josef; Fossum, Jon Otto; Bordallo, Heloisa N.

In: Journal of Physical Chemistry C, Vol. 126, No. 40, 13.10.2022, p. 17243-17254.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Hunvik, KWB, Lima, RJDS, Kirch, A, Loch, P, Roren, PM, Petersen, MH, Rudic, S, Sakai, VG, Knudsen, KD, Instituto, CRMM, Breu, J, Fossum, JO & Bordallo, HN 2022, 'Influence of CO2 on Nanoconfined Water in a Clay Mineral', Journal of Physical Chemistry C, vol. 126, no. 40, pp. 17243-17254. https://doi.org/10.1021/acs.jpcc.2c03310

APA

Hunvik, K. W. B., Lima, R. J. D. S., Kirch, A., Loch, P., Roren, P. M., Petersen, M. H., Rudic, S., Sakai, V. G., Knudsen, K. D., Instituto, C. R. M. M., Breu, J., Fossum, J. O., & Bordallo, H. N. (2022). Influence of CO2 on Nanoconfined Water in a Clay Mineral. Journal of Physical Chemistry C, 126(40), 17243-17254. https://doi.org/10.1021/acs.jpcc.2c03310

Vancouver

Hunvik KWB, Lima RJDS, Kirch A, Loch P, Roren PM, Petersen MH et al. Influence of CO2 on Nanoconfined Water in a Clay Mineral. Journal of Physical Chemistry C. 2022 Oct 13;126(40):17243-17254. https://doi.org/10.1021/acs.jpcc.2c03310

Author

Hunvik, Kristoffer W. Bo ; Lima, Rodrigo Jose da Silva ; Kirch, Alexsandro ; Loch, Patrick ; Roren, Paul Monceyron ; Petersen, Martin Hoffmann ; Rudic, Svemir ; Sakai, Victoria Garcia ; Knudsen, Kenneth Dahl ; Instituto, Caetano Rodrigues Miranda Materiais ; Breu, Josef ; Fossum, Jon Otto ; Bordallo, Heloisa N. / Influence of CO2 on Nanoconfined Water in a Clay Mineral. In: Journal of Physical Chemistry C. 2022 ; Vol. 126, No. 40. pp. 17243-17254.

Bibtex

@article{e0a719f48f1341a5a2d0bb38f7fb889b,
title = "Influence of CO2 on Nanoconfined Water in a Clay Mineral",
abstract = "Developing new technologies for carbon sequestra-tion and long-term carbon storage is important. Clay minerals are interesting in this context as they are low-cost, naturally abundant, can adsorb considerable amounts of CO2, and are present in storage sites for anthropogenic carbon. Here, to better understand the intercalation mechanisms of CO2 in dehydrated and hydrated synthetic Na-fluorohectorite clay, we have combined powder X-ray diffraction, inelastic and quasi-elastic neutron scattering, and density functional theory calculations. For dehydrated Na-fluorohectorite, we observe no crystalline swelling or spectroscopic changes in response to CO2, whereas for the hydrated case, damping of the librational modes related to the intercalated water was clearly observed. These findings suggest the formation of a more disordered water coordination in the interlayer associated with highly confined water molecules. From the simulations, we conclude that intercalated water molecules decrease the layer-layer cohesion energy and create physical space for CO2 intercalation. Furthermore, we confirm that interlayer confinement reduces the Na+ hydration number when compared to that in bulk aqueous water, which may allow for proton transfer and hydroxide formation followed by CO2 adsorption in the form of carbonates. The experimental results are discussed in the context of previous and present observations on, a similar smectite, Ni-fluorohectorite, for which it is established that CO2 attaches to the edge of nickel hydroxide islands present in the interlayer.",
keywords = "INELASTIC NEUTRON-SCATTERING, CARBON-DIOXIDE, X-RAY, HYDRATION PROPERTIES, INTERCALATED WATER, MOLECULAR-DYNAMICS, SUPERCRITICAL CO2, SMECTITE CLAYS, ADSORPTION, INTERLAYER",
author = "Hunvik, {Kristoffer W. Bo} and Lima, {Rodrigo Jose da Silva} and Alexsandro Kirch and Patrick Loch and Roren, {Paul Monceyron} and Petersen, {Martin Hoffmann} and Svemir Rudic and Sakai, {Victoria Garcia} and Knudsen, {Kenneth Dahl} and Instituto, {Caetano Rodrigues Miranda Materiais} and Josef Breu and Fossum, {Jon Otto} and Bordallo, {Heloisa N.}",
year = "2022",
month = oct,
day = "13",
doi = "10.1021/acs.jpcc.2c03310",
language = "English",
volume = "126",
pages = "17243--17254",
journal = "The Journal of Physical Chemistry Part C",
issn = "1932-7447",
publisher = "American Chemical Society",
number = "40",

}

RIS

TY - JOUR

T1 - Influence of CO2 on Nanoconfined Water in a Clay Mineral

AU - Hunvik, Kristoffer W. Bo

AU - Lima, Rodrigo Jose da Silva

AU - Kirch, Alexsandro

AU - Loch, Patrick

AU - Roren, Paul Monceyron

AU - Petersen, Martin Hoffmann

AU - Rudic, Svemir

AU - Sakai, Victoria Garcia

AU - Knudsen, Kenneth Dahl

AU - Instituto, Caetano Rodrigues Miranda Materiais

AU - Breu, Josef

AU - Fossum, Jon Otto

AU - Bordallo, Heloisa N.

PY - 2022/10/13

Y1 - 2022/10/13

N2 - Developing new technologies for carbon sequestra-tion and long-term carbon storage is important. Clay minerals are interesting in this context as they are low-cost, naturally abundant, can adsorb considerable amounts of CO2, and are present in storage sites for anthropogenic carbon. Here, to better understand the intercalation mechanisms of CO2 in dehydrated and hydrated synthetic Na-fluorohectorite clay, we have combined powder X-ray diffraction, inelastic and quasi-elastic neutron scattering, and density functional theory calculations. For dehydrated Na-fluorohectorite, we observe no crystalline swelling or spectroscopic changes in response to CO2, whereas for the hydrated case, damping of the librational modes related to the intercalated water was clearly observed. These findings suggest the formation of a more disordered water coordination in the interlayer associated with highly confined water molecules. From the simulations, we conclude that intercalated water molecules decrease the layer-layer cohesion energy and create physical space for CO2 intercalation. Furthermore, we confirm that interlayer confinement reduces the Na+ hydration number when compared to that in bulk aqueous water, which may allow for proton transfer and hydroxide formation followed by CO2 adsorption in the form of carbonates. The experimental results are discussed in the context of previous and present observations on, a similar smectite, Ni-fluorohectorite, for which it is established that CO2 attaches to the edge of nickel hydroxide islands present in the interlayer.

AB - Developing new technologies for carbon sequestra-tion and long-term carbon storage is important. Clay minerals are interesting in this context as they are low-cost, naturally abundant, can adsorb considerable amounts of CO2, and are present in storage sites for anthropogenic carbon. Here, to better understand the intercalation mechanisms of CO2 in dehydrated and hydrated synthetic Na-fluorohectorite clay, we have combined powder X-ray diffraction, inelastic and quasi-elastic neutron scattering, and density functional theory calculations. For dehydrated Na-fluorohectorite, we observe no crystalline swelling or spectroscopic changes in response to CO2, whereas for the hydrated case, damping of the librational modes related to the intercalated water was clearly observed. These findings suggest the formation of a more disordered water coordination in the interlayer associated with highly confined water molecules. From the simulations, we conclude that intercalated water molecules decrease the layer-layer cohesion energy and create physical space for CO2 intercalation. Furthermore, we confirm that interlayer confinement reduces the Na+ hydration number when compared to that in bulk aqueous water, which may allow for proton transfer and hydroxide formation followed by CO2 adsorption in the form of carbonates. The experimental results are discussed in the context of previous and present observations on, a similar smectite, Ni-fluorohectorite, for which it is established that CO2 attaches to the edge of nickel hydroxide islands present in the interlayer.

KW - INELASTIC NEUTRON-SCATTERING

KW - CARBON-DIOXIDE

KW - X-RAY

KW - HYDRATION PROPERTIES

KW - INTERCALATED WATER

KW - MOLECULAR-DYNAMICS

KW - SUPERCRITICAL CO2

KW - SMECTITE CLAYS

KW - ADSORPTION

KW - INTERLAYER

U2 - 10.1021/acs.jpcc.2c03310

DO - 10.1021/acs.jpcc.2c03310

M3 - Journal article

VL - 126

SP - 17243

EP - 17254

JO - The Journal of Physical Chemistry Part C

JF - The Journal of Physical Chemistry Part C

SN - 1932-7447

IS - 40

ER -

ID: 324368406