2021
DOI: 10.1038/s41586-021-03504-4
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Asymmetric response of interfacial water to applied electric fields

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Cited by 109 publications
(95 citation statements)
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References 40 publications
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“…6 The apparently universal negative CME in metal-water interfaces is attributed to the oxygen end of water facing the electrode at the PZC, requiring a negative electrode charge to counter this preferential orientation and increase the entropy. 7 This asymmetry of interfacial water also agrees with recent spectroscopic evidence 15 and molecular dynamics (MD) studies on interfacial water dynamics 16 , prompting the question whether the inner layer capacitance is similarly asymmetric.…”
Section: Introductionsupporting
confidence: 77%
“…6 The apparently universal negative CME in metal-water interfaces is attributed to the oxygen end of water facing the electrode at the PZC, requiring a negative electrode charge to counter this preferential orientation and increase the entropy. 7 This asymmetry of interfacial water also agrees with recent spectroscopic evidence 15 and molecular dynamics (MD) studies on interfacial water dynamics 16 , prompting the question whether the inner layer capacitance is similarly asymmetric.…”
Section: Introductionsupporting
confidence: 77%
“…It should be noted that the net potential drop between the air–water interface and the monolayer surface is between 0.4 and 1.0 V. It is important to note that in the presence of interfacial potential, absorptive-dispersive mixing is crucial and controls the spectral line shapes of the VSFG spectra. Different groups have tried to quantify the χ (3) contribution to the total VSFG intensity and concluded that it is non-negligible in such systems because of the breaking of centro-symmetry at the interfaces and extended influence of the charged interfaces into the diffuse and bulk layers. The χ (3) contribution to the VSFG spectrum mainly emanates from the molecules in the diffuse layer. The potential contribution from the diffuse layers onto the interface can be extracted by applying the parallel capacitor principle, i.e ., by fitting a linear relation between the potential and the distance from the interface in the diffuse layer region and then extrapolating the same up to the interface.…”
Section: Resultsmentioning
confidence: 99%
“…The exact origin of the two peaks is still being investigated (Sovago et al, 2008;Myalitsin et al, 2016), but it is generally agreed that the lower the OH stretching frequency is, the stronger, and/or more ordered, H-bonding environment the corresponding moieties sense. On the bulk-SiO 2 /H 2 O interfaces, the 3,200 cm −1 mode (assigned to the topmost water layer (Urashima et al, 2018)) was found to grow more rapidly than the 3,400 cm −1 one (H-bonded to bulklike water molecules (Montenegro et al, 2021)) at increasing pH, which suggested a more ordered water structure near the more negatively charged surface. In contrast, in our case, when the SiO 2 surface bound charge evolved from positive to negative, the 3,400 cm −1 mode appeared to increase more rapidly.…”
Section: Sfvs In H 2 Omentioning
confidence: 94%
“…The rich phenomena and functionalities of oxide/water interfaces are largely based on their interfacial charging states and properties of EDLs (Brown, 2001;Putnis, 2014;Covert and Hore, 2016;Ohno et al, 2016;Schaefer et al, 2018). For example, the water electric dipole moment can be aligned by the electrostatic field in EDL and affect the interfacial chemistry (Brown, 2001;Nihonyanagi et al, 2004;Aragones et al, 2011;Saitta et al, 2012;Brown et al, 2016;Montenegro et al, 2021). In the case of ice, such field alignment could give rise to a ferroelectric state of highly oriented water molecules, which was readily probed using the surfacesensitive sum-frequency vibrational spectroscopy (SFVS) (Miranda et al, 1998;Verdaguer et al, 2006;Anim-Danso et al, 2016).…”
Section: Introductionmentioning
confidence: 99%