Abstract
The adsorption of water vapor in silica nanopores with different pore morphologies and surface hydrophilicities was studied to quantify the densities and thicknesses of the water sorption layers and deduce their molecular structures. Water adsorption to surface hydroxyls is described by a multilayer sorption model. At low pressure, the water adsorption isotherms are largely independent of pore size and the adsorbed amounts scale with the surface hydroxyl density. Adsorbed-phase densities corresponding to the adsorption of two water molecules per surface hydroxyl group are found in the first adsorbed water layer for a wide range of surface hydroxyl densities. The densities and layer thickness values found in narrow pores indicate that patchy adsorbed layers form if not enough water molecules exist for a full layer, which coexist with dry pore surface regions. This behavior indicates cooperative adsorption effects, i.e., a preference for the formation of hydrogen bonds between water molecules bound to surface hydroxyls. In narrow pores, pore condensation limits further growth of the sorption layer, and in larger pores and at the planar quartz surface, a second adsorbed water layer is formed, which can hold up to approximately 4 additional water molecules per surface hydroxyl group. The water molecules in these thicker adsorption layers arrange such that the sorption layer density is similar to the bulk water density. Pore confinement limitations on the sorption layers are observed in pores with radii of as large as 8 nm. Molecular dynamics modeling reveals two preferential orientations for water molecules adsorbing to surface hydroxyl groups and suggests an intralayer structuring in the adsorbed monolayer. Adsorbed water molecules in the sorption layer are bonded to the surface hydroxyl group via the donation and acceptance of hydrogen bonds.
Original language | English |
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Pages (from-to) | 2885-2895 |
Number of pages | 11 |
Journal | Journal of Physical Chemistry C |
Volume | 126 |
Issue number | 5 |
DOIs | |
State | Published - Feb 10 2022 |
Funding
We thank Paul Fenter (Argonne National Laboratory) for providing recalculated data for water sorption to quartz and stimulating discussions. This material is based upon work supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences, and Biosciences Division. T.L., S.G., and D.R.C. acknowledge support from the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Geosciences Program under grant number DE-SC00067878. Simulations reported in this work were carried out at the College of Arts and Sciences (ASC) Unity Cluster of the Ohio State University and the Deep Carbon Observatory cluster hosted by Rensselaer Polytechnic Institute. The computational resources and support provided are gratefully acknowledged (Sandy Shew, Brent Curtiss, Keith Stewart, John Heimaster, Patrick West, and Peter Fox). This manuscript has been authored in part by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the U.S. Department of Energy (DOE). The U.S. government retains and the publisher, by accepting the article for publication, acknowledges that the U.S. government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for U.S. government purposes. The DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan (http://energy.gov/downloads/doe-public-access-plan). We thank Paul Fenter (Argonne National Laboratory) for providing recalculated data for water sorption to quartz and stimulating discussions. This material is based upon work supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences, and Biosciences Division. T.L., S.G., and D.R.C. acknowledge support from the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Geosciences Program under grant number DE-SC00067878. Simulations reported in this work were carried out at the College of Arts and Sciences (ASC) Unity Cluster of the Ohio State University and the Deep Carbon Observatory cluster hosted by Rensselaer Polytechnic Institute. The computational resources and support provided are gratefully acknowledged (Sandy Shew, Brent Curtiss, Keith Stewart, John Heimaster, Patrick West, and Peter Fox). This manuscript has been authored in part by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the U.S. Department of Energy (DOE). The U.S. government retains and the publisher, by accepting the article for publication, acknowledges that the U.S. government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for U.S. government purposes. The DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe-public-access-plan ).
Funders | Funder number |
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DOE Public Access Plan | |
Deep Carbon Observatory | |
Geosciences Program | DE-AC05-00OR22725, DE-SC00067878 |
U.S. Government | |
U.S. Department of Energy | |
Office of Science | |
Basic Energy Sciences | |
Argonne National Laboratory | |
Ohio State University | |
Adhesives and Sealant Council | |
Chemical Sciences, Geosciences, and Biosciences Division | |
College of Arts and Sciences, Boston University |