AVS 65th International Symposium & Exhibition | |
Applied Surface Science Division | Wednesday Sessions |
Session AS+NS+SA-WeM |
Session: | Beyond Traditional Surface Analysis |
Presenter: | Caixia Bu, University of Virginia |
Authors: | C. Bu, University of Virginia C.A. Dukes, University of Virginia |
Correspondent: | Click to Email |
Amorphous solid water (ASW) formed by vapor deposition on substrates <~130 K is of interest for its abundance in Earth’s upper atmosphere, icy planetary bodies, and throughout the interstellar medium, as well as its use as model material in many disciplines. Two crucial characteristics of ASW are a self-induced negative surface potential and formation of nanopores [1]. Here, we examine the role of microstructure, including nanopores, on the spontaneous surface potential of ASW, and describe the complementary experimental techniques used, which have application for other microporous solids.
ASW films were deposited by directed vapor beams onto a He-cooled quartz-crystal microbalance (QCM) under ultra-high vacuum. The integrated pore volume (porosity) was calculated by combining the areal mass measured via QCM and thickness measured by UV-visible interferometry. The integrated surface area was indicative by the abundance of incompletely coordinated surface water molecules (H2O) on the pores, using the O-H dangling bonds (DBs) measured by FT-IR spectroscopy. An in-situ Kelvin probe measured film surface potential. A long-distance optical microscope monitored film morphology in vacuo. Annealing effects were investigated by heating the film at 1.8 K/min.
The magnitude of the negative surface potential (|Vs|) increased linearly with film thickness at rates (|ΔVs/ΔL|) that decreased with increasing growth temperature (Tg = 10–110 K), keeping deposition angle at θ = 0° (angle between vapor beam and QCM normal); at Tg = 30 K, the |ΔVs/ΔL| decreased with increasing θ (= 10−75°). ASW porosity showed no dependence on Tg at θ = 0°, but increased significantly with increasing θ. The H2O DBs decreased/increased with increasing Tg/θ, showing similar trends as the |ΔVs/ΔL|. Upon heating, the most striking result was that the DB at ~3720 cm−1 (from two-coordinated H2O) and the |Vs| had similar temperature-dependent evolutions. By correlating all measurements, we propose that the observed intrinsic ASW surface potential results from aligned incompletely-coordinated H2O on the pore surfaces [2].
The |Vs| decreased abruptly when ASW thickness exceeded a critical value (Lc), and cracks appeared in the optical images of the films. The Lc, ~1−5 µm (Tg = 10–50 K; θ = 0–55°), increased with Tg and θ, suggesting dependences on the microporous structure. We explain such dependences of Lc in the context of Griffith theory and estimate the tensile strength of ASW to be ~25–40 MPa [3].
We acknowledge support from the NASA LASER Program.
[1]Raut et al., J. Chem. Phys.127, 204713 (2007); [2]Bu et al., J. Chem. Phys.143, 074702 (2015); [3]Bu et al., Appl. Phys. Lett.109, 201902 (2016).