The hydroxide anion OH−(aq) in homogeneous bulk water, that is, the solvated proton hole, is known to feature peculiar properties compared with excess protons solvated therein. In this work, it is disclosed that nanoconfinement of such alkaline aqueous solutions strongly affects the key structural and dynamical properties of OH−(aq) compared with the bulk limit. The combined effect of the preferred hypercoordinated solvation pattern of OH−(aq), its preferred perpendicular orientation relative to the confining surfaces, the pronounced layering of nanoconfined water and the topology of the hydrogen bond network required for proton hole transfer lead to major changes of the charge transport mechanism, in such a way that the proton hole migration mechanism depends exquisitely on the width of the confined space that hosts the water film. Moreover, the anionic Zundel complex, which is of transient nature in homogeneous bulk solutions, can be dynamically trapped as a shallow intermediate species by suitable nanoconfinement conditions.
The solvated hydroxide ion in water offers surprising features, both structural and dynamical, compared with what has been expected for a long time according to the naive ‘mirror image’ picture of the hydrated excess proton1. Based on extensive simulation work and subsequent experimental confirmation, it may be said that OH−(aq) is well understood in the limits of both bulk solvation and microsolvation1. However, the solvated hydroxide in inhomogeneous aqueous environments is still far from being understood, resulting in an ongoing and lively debate revolving around the properties of water’s two autoprotolysis products, H+(aq) and OH−(aq), in the context of interfacial water. One of the most elementary questions in this respect, ‘Is the water surface acidic or basic?’, is controversially discussed by different authors2,3,4,5,6. Although most studies report that water surfaces at water/air and water/oil interfaces are negatively charged7,8,9,10, quite different explanations for this have been proposed, several of them actually involving hydroxide ions, and there is also no consensus yet regarding the origin of this surface charge11,12,13,14,15,16,17,18,19. A summary of the different, mostly conflicting results—both from experiments and simulations—is provided in the introduction of ref. 20 including substantial referencing of earlier work. Clearly, more studies are needed to eventually settle this longstanding debate.
In the broader context of interfacial solutions beyond the simple water/vapour system, much interest in the OH−(aq) species in confined environments is arising, for instance as a consequence of recent developments in anionic exchange membranes21,22, which are gaining attention for their use in electrochemical devices such as fuel cells as an alternative to the more traditional proton exchange membranes. Especially alkaline aqueous solutions in reduced dimensionality and nanoconfinement are becoming highly relevant in view of the very distinct properties of nanoconfined water compared with the bulk. Thus, OH−(aq) has already been carefully studied in nanoconfined water wires23,24 and monolayer films25. In the realm of confinement, it is stressed that computer simulation is considered to be a valuable complement to experiment in view of challenges encountered when probing experimentally the acidic/basic character of interfacial versus bulk-like water in nanoconfinement26.
In this work, we uncover particularly surprising dynamical properties of OH−(aq) in nanoconfined water layers between mackinawite FeS sheets based on ab initio molecular dynamics simulations27 in conjunction with an elaborate model of this mineral-based slit pore. Mackinawite has been proposed as a putative nanoreactor and possibly even catalyst for prebiotic chemistry at elevated thermodynamic conditions close to deep-sea hydrothermal vents28, where high temperatures and pressures of typically ≈500 K and ≈20 MPa, respectively, are encountered. Its layered structure can be intercalated by water and it has been suggested that a primordial ‘pyrophosphate synthetase nanoengine’ could have emerged, thanks to the charge gradients that can be established along these nanochannels29,30. Because of these ramifications and as a prologue for an upcoming study of prebiotic reactions31,32 in such environments, we set out to investigate the properties of nanoconfined water in mackinawite at the relevant elevated temperature and pressure conditions33, and also those of the solvated excess proton therein34. Transcending previous work, we compare two different confinements of alkaline aqueous solutions in an overall realistic setup, one with extreme confinement where water forms a monolayer and another one where the aqueous phase is a water bilayer. Anticipating our core result, it is shown that these confinements imprint stark and unexpected differences on the structural diffusion mechanism of OH−(aq) unknown from H+(aq).
General features of nanoconfined alkaline water lamellae
We have studied OH−(aq) in nanoconfined water between mackinawite sheets using our well-validated setups33,34, namely the systems N (narrow slit pore, Fig. 1) and W (wide slit pore). In extreme confinement, system N, where water forms a single-layer hydrogen-bonded network (Fig. 2 top), the dynamics of the basic solution is not liquid-like, as the water molecules are ‘arrested’ at certain preferred positions, which is consistent with what was observed for both neutral33 and acidic34 water lamellae. On the other hand, the most interesting aspect in system W is the stratified structure of the alkaline aqueous phase, where a water bilayer is clearly formed (Fig. 2 bottom and Fig. 3). The water dynamics in this case is liquid-like and again this is consistent with our previous simulations of neutral and acidic nanoconfined water33,34.
Structure and orientation of the OH−(aq) complex
In the homogeneous bulk water environment, OH− is known to preferentially accept four hydrogen bonds in a square-planar arrangement, while H′ donates none, that is, OH−(H2O)4 as depicted in Fig. 4f including standard notation, which is called the ‘hypercoordinated’ resting or majority state according to the dynamical hypercoordination mechanism1 of hydroxide structural diffusion in the bulk limit. When one of these accepted hydrogen bonds is broken because of suitable thermal fluctuations of the hydrogen bond network and OH− is transiently donating a hydrogen bond via its hydrogen H′, then the OH− is properly ‘presolvated’35 in a topology similar to the ideal tetrahedral coordination of a H2O molecule in bulk water. In such favourable configurations, proton hole transfer along the most active accepted hydrogen bond, that is, O*··· H*–Õ, readily occurs to O*, thus forming a water molecule H′H*O* in its ideal solvation structure. This leads to the concurrent displacement of the charge defect to the previous first neighbour site Õ, which quantitatively explains the full proton hole transfer kinetics36,37.
In the inhomogeneous, nanoconfined water environment, the first striking feature of OH−(aq) can be extracted from the number density profiles normal to the water/mineral interface (Fig. 2) together with the joint probability of the position and angle of the OH− unit relative to the confining solid surfaces (Fig. 5a), which discloses pronounced spatial and orientational preferences. The results for the narrow pore, system N, agree with similar calculations for solvated OH− between graphene slabs25; we also find the O–H− unit to be oriented perpendicular to the confining surfaces and coordinated to four water molecules (Fig. 1). In our case, the ‘eggbox’ corrugation of the mackinawite surface imprints a superstructure on the nanoconfined water monolayer and the OH− unit is displaced towards the midplane, which minimizes the distortion of the square-planar OH−(H2O)4 complexes.
In stark contrast, the profiles for the wide system W show remarkable peculiarities. Here, the OH− is nicely integrated into either one of the water layers, but the only hydrogen of the OH−, H′, is preferentially located close to the confining surface instead of being buried in the water bilayer. Close inspection of the trajectories reveals that the OH− anion is in about half of the time fourfold coordinated in a square-planar configuration, where all the waters of the first hydration shell are in the same water layer, but oriented such that the H′ atom points to the confining mineral surface as depicted in Fig. 3a. Other possible configurations—yet less probable−feature the OH− pointing to the neighbouring water layer where it gets ‘buried’ (Fig. 3b), or being ‘tilted’ such that its first solvation shell belongs to both water layers (Fig. 3c). The relative probability of these configurations can be easily extracted quantitatively from Fig. 5a.
Proton hole transfer and structural diffusion mechanisms
The free-energy profiles for proton hole transfer (Fig. 6a), as obtained by considering the well-established generalized coordinate , yield barriers of roughly 0.5 kcal mol−1 (≈(1/2)kBT500) in both systems, N and W, which is slightly above the corresponding barrier in bulk water. However, is the proton hole migration mechanism in nanoconfined water lamellae the same as in the homogeneous bulk environment? In the narrow system N, which is characterized by a single water layer, OH−(aq) is preferentially coordinated to four water molecules and, moreover, most probably points with its H′ towards either the ‘upper’ or ‘lower’ confining surface—being key to charge migration. This so-called ‘exposed’ (E) interfacial state in the inhomogeneous environment corresponds to the hypercoordinated resting state with respect to proton migration as depicted by the leftmost structure of Fig. 4a and indicated by high probabilities in Fig. 5. Next, the loss of one of its four hydrogen bonds leaves the OH− accepting three hydrogen bonds. This state, on proton transfer of H* from a water molecule H*HÕ in the first solvation shell (see Fig. 4f for site labelling), results into the formation of a water molecule H′H*O* that is accepting two hydrogen bonds and donating one (to Õ), which agrees substantially with recent simulations of an alkaline water monolayer between graphene sheets25.
The striking difference with hydroxide migration in bulk water1 is that it is not possible for the nascent water molecule, H′H*O*, being necessarily located right at the interface, to achieve the ideal tetrahedral coordination with two donor and two acceptor hydrogen bonds. However, importantly, the O*H′ bond of the nascent water molecule is a ‘dangling’ OH bond (also called free OH or single-donor species), which is one out of several ideal hydrogen bond arrangements that can terminate planar water interfaces38. Indeed, there is now solid evidence accumulated that the preferred termination of the water surface in contact with vapour occurs via such dangling OH bonds, which implies that these water molecules donate only a single hydrogen bond towards the interior39. This is exactly the situation met in the centre panel of Fig. 4a, where this donated hydrogen bond is accepted by the nascent OH− defect after proton hole transfer. Thus, taking that viewpoint, it is evident that not being able to form the weak donor hydrogen bond via H′, which ensures fourfold hydrogen bonding of the nascent water H′H*O* as observed in bulk migration processes1, should not block the proton transfer event towards O* if that occurs right at an interface, in full accord with the presolvation concept35. Moreover, our reference calculations of OH− in bulk water (see ‘Methods’ section) showed a further weakening of the donor bond via H′ at the relevant high temperature and pressure conditions compared with ambient, while still adhering to the dynamical hypercoordination mechanism1 of hydroxide structural diffusion. This supports our observation that the absence of this bond should not hinder proton hole transfer in nanoconfined water at these elevated conditions.
Yet, there is an intricate geometric constraint that is imposed by the planar monolayer confinement in the narrow system N. This comes because the water molecule that turns into the new OH−(aq), that is, ÕH−, must be oriented such that its O–H axis is also perpendicular to the surface. Otherwise, the formation of the preferred resting state would not be possible and the very same proton that has just been transferred would immediately rattle back, thus reforming the previous OH−, that is, O*H′ and therefore not leading to any charge transport. Indeed, these rattling events in system N are very frequent and it has been suggested that the additional time necessary for reaching this proper arrangement of the proton donating water molecule is the reason for the slower diffusion rate of OH−(aq) in monolayers25 compared with the bulk. In addition to that, we observe in our simulations that the nascent OH−(aq) will point overwhelmingly with its H′ towards the opposite surface of that pore, see Fig. 4a. This phenomenon is the result of an intricate interplay of extreme nanoconfinement in the monolayer limit, the preferred orientation of interfacial OH− species and the essentially tetrahedral topology of the hydrogen bond network. The net outcome is that proton hole transfer in the narrow slit pore limit preferentially follows a zig-zag migration path where OH− jumps between the two opposing planar surfaces, thereby reorienting its dipole moment in each such step as illustrated by Fig. 4a. This scenario is fully consistent with the respective statistical analyses in Figs 5a and 6a.
In the wide slit pore W, the mechanism for proton hole transfer and subsequent structural diffusion is found to be even more intricate as a consequence of the bilayer sub-structure of the water lamella. The hypercoordinated resting state of the OH−(aq) complex at the interface is of course identical to that in the N system (Fig. 3a), which is the ‘exposed’ configuration E. As in the previous case, the loss of one of these hydrogen bonds leaves the OH− in a properly presolvated state that, on proton transfer from one of the surrounding waters, forms an interfacial ‘single-donor’ water molecule that donates one hydrogen bond and accepts two. Now, the key distinction is that the nascent OH− almost always finds itself in a qualitatively different solvation environment from the narrow pore scenario: either this new OH− species is pointing with its H′ hydrogen towards the other water layer of the bilayer film as depicted in Fig. 3b, which is what we call the ‘buried’ configuration B, or it is in a ‘tilted’ situation T as illustrated by Fig. 3c; see Fig. 5 for the definitions of the E/B/T states. Both the ‘buried’ and ‘tilted’ arrangements make it easy for the nascent OH− unit to reach the ideal tetrahedral solvation state of a water molecule in bulk. Hence, the newly formed OH− is prone to receive a proton via any of the hydrogen bonds that are donated to it, which is however most likely to be the same hydrogen bond along which the previous proton transfer took place! This leads to confinement-induced rattling as visualized schematically in Fig. 4b and corresponds to interconversions between Fig. 3a–c without any net charge transport.
The striking difference between the initial ‘exposed’ state and the most unstable ‘tilted’/‘buried’ configurations is clearly revealed if we analyse separately these limiting cases in terms of the joint probabilities as depicted in Fig. 5b,c. This analysis makes clear that the resting state with respect to proton transfer (that is, δ>0.5) coincides with OH−(aq) being ‘exposed’, whereas active states with centred hydrogen bonds (δ>0.1) go hand in hand with OH−, finding itself in either ‘buried’ or ‘tilted’ configurations. This structural cross-correlation can be immediately linked to free-energy profiles for proton hole transfer once separated in terms of the ‘exposed’ and ‘tilted’/‘buried’ scenarios (Fig. 6a). The proton hole transfer barrier involving only ‘exposed’ states is found to be dramatically higher, by roughly a factor of 4, relative to those situations where OH−(aq) is initially in either a ‘buried’ or ‘tilted’ arrangement. This facile proton transfer for T/B configurations in the wide slit pore correlates nicely with formation of the donated hydrogen bond via H′ in active complexes (δ<0.1), which on detailed analysis of conditional radial distribution functions together with their running coordination numbers is revealed to be more pronounced than in the corresponding bulk regime (whereas this H′ bond is essentially absent both in E configurations in the W system, as well as in the narrow pore confinement). We infer that, although the presence of this bond donated by OH− is not strictly necessary for proton (hole) transfer to occur at all, it greatly facilitates this process when the structural constraints imprinted by the confinement allow for or even favour its formation.
These different solvation environments, which can be reached on proton hole transfer from ‘exposed’ to ‘buried’/‘tilted’ configurations and vice versa only in the wide pore, are the reason of frequent proton rattling events. In this case, a specific OH− receives and back transfers a proton involving exclusively water molecules in its first solvation shell, see Fig. 4b. Hence, for structural diffusion and thus charge migration to happen, some additional condition must be met that avoids the reformation of the initial OH− unit. On carefully analysing our trajectories, we have identified three distinct events that can avoid this: (i) a proton hole transfer event is followed by the reorientation of the nascent water molecule so the eventual rattling of the just transferred proton would not lead to reformation of an OH− species pointing to the surface (as illustrated by the mechanism in Fig. 4c); (ii) the OH− unit itself reorients so that the H′ points away from the confining surface, which can happen via changes in the first solvation shell or vehicular (Stokes) diffusion of the entire complex caused by thermal fluctuation (Fig. 4d); (iii) a change in the second solvation shell makes possible fast Grotthuss-like proton transfer across a water wire so the newly formed OH− is no longer the first neighbour of the former resting state, thus suppressing the probability of a rattling event that will lead to its reformation (not depicted).
It is observed that structural diffusion in the wide slit pore mostly occurs via mechanisms (i) or (ii): once the preferred orientation of the former O*H′ bond is lost, the formation of the same initial ‘exposed’ state after proton rattling is no longer possible and subsequent proton hole transfer events follow until a new ‘exposed’ configuration is reached. This can occur in only two steps, that is, in a ‘exposed’–‘buried’–‘exposed’ or a ‘tilted’–‘buried’–‘exposed’ sequence (sketched in Fig. 4c,d, respectively). Yet, it can be the case that the ‘exposed’ configuration is not easily reachable, because a water molecule with a dangling bond exposed to the surface is not coordinated to the OH−. Such situation, illustrated in Fig. 4e, leads to a superposition of ‘tilted’ and ‘buried’ structures. This effect imprints the shallow local free-energy minimum at δ≈0 in the free-energy profile (Fig. 6a), which implies that the Zundel-like proton hole complex [HO H OH]− is not anymore a transient structure but rather an intermediate species. This trapping of the anionic Zundel complex due to nanoconfinement is in stark contrast to the transient Zundel-like transition state in homogeneous bulk environments as predicted by ab initio path integral simulations as a feature of the dynamical hypercoordination mechanism40 and confirmed by time-resolved spectroscopy41 for OH−(aq).
Finally, we provide some qualitative insights into both diffusion properties and reorientation behaviour (which are not directly accessible from our NVT simulations due to the required heavy thermostatting33, see Methods). Towards structural diffusion of OH−(aq), we have computed conditional free-energy profiles where proton hole rattling has been approximately excluded; here, rattling events are simply identified by searching for proton hole transfer events of the kind and excluding the contribution from to the P(δ) probability distribution, to provide qualitative trends and, therefore, we do not claim these conditional profiles to be the proper free-energy profiles for proton (hole) diffusion. The resulting conditional free-energy barrier for system N, ≈1.3 kcal mol−1, is a bit higher compared with that of the bulk and W systems, being both ≈1.1 kcal mol−1, according to Fig. 6b. Assuming that these conditional free-energy barriers are correlated with the diffusion coefficient of OH−(aq), they suggest that structural diffusion of the proton hole should be slightly less efficient in the narrow slit pore than in the W system, which in turn is essentially identical to that in the respective bulk limit. Indeed, this inference for the N system is in accord with the recent finding that OH− structural diffusion in a water monolayer confined between two graphene slabs is slowed down compared with the corresponding bulk environment as obtained from proper dynamical analyses25.
Concerning the reorientation dynamics, it has been shown previously that there is a close connection between increased reorientation times and suppressed structural diffusion for hydroxide in bulk water, thus establishing a close link between proton (hole) transfer and OH− orientational relaxation42. To qualitatively disclose the relationship between these two processes in nanoconfined water in the absence of having access to any time evolution, we computed the probability distribution function for the reorientation angle on proton transfer, being similar in spirit to our indirect approach to the diffusion properties. Interestingly, the data in Fig. 7 unveil that the reorientation properties are remarkably different for system N compared with system W and bulk water. A proton hole transfer event has a probability of roughly 70% of causing a significant reorientation >120° in system N, whereas that probability is only roughly 40% for the W and bulk systems. This clearly reflects the peculiar migration mechanism sketched in Fig. 4: extreme confinement in system N imposes that proton (hole) migration occurs via a zig-zag mechanism, which requires significant reorientational motion of the OH−, whereas moderate confinement allows for smaller reorientations, in that sense being more similar to the bulk regime. Thus, the intimate connection between proton hole diffusion and OH− reorientation dynamics in the bulk42 seems to hold also in nanoconfined water.
Our ab initio simulations of alkaline aqueous solutions subject to nanoconfinement reveal an unexpectedly rich dynamical landscape for proton hole transfer and thus for the migration of negative charge defects in terms of solvated hydroxide species, OH−(aq). Although the free-energy barriers for proton hole transfer in the narrow and wide slit pore systems N and W are remarkably similar, both to each other and compared with bulk water, the extracted mechanisms for structural diffusion of proton holes in these nanoconfined aqueous environments reveal major differences not only with reference to the bulk, but also between the two confinement scenarios. In particular, our results show that the diffusion regime is indeed qualitatively dependent on the degree of confinement, resulting in a monolayer or bilayer structuring of the water lamellae in the narrow and wide scenario, respectively. In the narrow pore, the interplay of nanoconfinement due to planar surfaces, fourfold hypercoordination and preferred perpendicular orientation of interfacial OH−(aq) species with respect to the surfaces, and the topology of the hydrogen-bonded water network that hosts the defect imprints a zig-zag charge migration pathway. As a result, the proton hole necessarily must jump between the two surfaces in each step, thereby reversing the orientation of the hydroxide’s dipole moment, which should be detectable by suitable dielectric spectroscopy techniques.
Charge transport in the basic solution confined by a wider slit pore is not only distinctly different from the monolayer limit, but allows for a multitude of different migration and trapping mechanisms, which is traced back to the bilayer sub-structure of the confined water film in this case. First of all, the OH−(aq) defect can stay for a short time trapped at the interface in its preferred perpendicular hypercoordinated state due to a suppressed probability, to find a hydrogen bonded water molecule that can become a stable defect site after proton hole transfer, which results in pronounced rattling with respect to the trapped interfacial defect. Next, it is found that the hydroxide anion can be even stabilized in terms of an anionic Zundel-like intermediate with its characteristic centred hydrogen bond, [HO···H···OH]−, instead of this Zundel complex being a transition state and thus a transient species as encountered in bulk alkaline solutions. Last but not the least, several distinct charge transport scenarios have been observed that indeed lead to net defect displacements and thus contribute to long-range structural diffusion.
Capitalizing on all these observations, it should be possible to rationally design different nanostructures that will allow for different charge transport rates of confined alkaline aqueous solutions. This is much more promising compared with acidic solutions, as no differences regarding proton transfer or structural diffusion depending on the extent of nanoconfinement have been found for the hydrated excess proton H+(aq), observing that the standard Grotthuss diffusion mechanism is not at all hindered in any of the systems compared with the bulk. These facts put together open up very suggestive questions and ideas towards potential applications of nanoconfined alkaline water films in layered materials, especially concerning rational design of ion exchange membranes where the diffusion rate of OH− and thus charge transport can be tuned by controlling the degree of confinement imposed by the slit pores, while keeping the diffusion rate of H+ unchanged.
In addition, our results are expected to add new insights, ideas and stimulation to the ongoing extensive debate about the molecular character of the water/air interface. Athough it is obviously out of the scope of this investigation—our system being subject to two-sided confinement inside a layered mineral—to directly address this controversy, we think that the now clearly revealed asymmetry between the diffusion mechanism of OH− versus H+ species in interfacial water films can be a valuable piece of information for solving the puzzle of the origin of the observed charge in interfacial water.
Let us close our discussion by addressing more fundamental issues. Based on the multitude of predicted charge transport channels, including various forms of trapped defects, it is predicted that analyses of the long-time dynamics, which is accessible via empirical valence bond or neural network representations of OH− in water, will lead to the so-called ‘broad’ waiting time distributions in the sense of Lévy flights and non-Gaussian fluctuations. Here, systematic variation of the slit pore width will be the key control parameter that determines the particular dynamical scenario. Depending on that control parameter, it might be possible to switch in a well-defined manner between sub- and superdiffusive structural charge transport and thus to probe strongly fractional dynamics with long-memory effects.
We employed the well-validated methods and system setups as in our previous studies of neutral and acidic water nanoconfined between mackinawite sheets33,34. We used the Perdew-Burke-Ernzerhof (PBE) density functional43 with a plane wave cutoff of 25 Ry and ultrasoft pseudopotentials44 containing d-projectors for sulfur and semicore states, as well as scalar relativistic corrections for iron. The ab initio molecular dynamics simulations27 were carried out with the Car–Parrinello method as implemented in CPMD45. Massive Nosé–Hoover chain thermostats46 were used for controlling the temperature of nuclei (at 500 K) and electrons, with a fictitious orbital mass of 700 a.u., a timestep of 2 a.u., substituting D for H masses and employing a very high-order Suzuki–Yoshida algorithm to properly integrate these thermostat equations of motion. Such unusually aggressive thermostatting was found to be necessary, to enforce stable Car–Parrinello propagation for these slit pore systems subject to metallic mineral confinement33, which strictly prevents the calculation of time-correlation functions and thus of any dynamical properties. The systems were equilibrated for 5 ps, after which 40 ps of production runs were collected.
We studied the alkaline solution in ‘extreme’ and ‘moderate’ nanoconfinements due to mackinawite sheets33,34 denoted as the narrow and wide slit pore systems N and W, respectively. They consist of two Fe32S32 parallel layers situated at the top and bottom of a tetragonal supercell with a=b=14.69 Å. The ideal spacing of 5.03 Å is kept between the top and bottom layers of the two distinct mineral sheets, where the top- and bottom-most S atoms of the top and bottom layers are frozen at their ideal crystal positions, thus keeping all atoms at the water/mineral interface mobile. In system N, c=13.82 Å and the interlayer space is filled with 31 H2O molecules plus 1 OH−, whereas in system W, c=16.73 Å and the interlayer contains 48 H2O molecules plus 1 OH−. This roughly corresponds to an estimated pressure of ≈20 MPa at T=500 K, thus approximately mimicking elevated temperature and pressure conditions. For the corresponding reference simulations for OH− in homogeneous bulk water, we used accordingly a cubic cell of a=10.415 Å containing 31 H2O and 1 OH− unit.
Validation of the approach
The computational approach and model setup have been extensively validated in our previous studies33,34. In particular, it was checked34 that the fictitious orbital mass yields stable Car–Parrinello propagation and tests with both lower and higher values (of 500 and 900 a.u.) yielded similarly stable integration. We note that even though it is possible to find some debate in the literature concerning possible artefacts in non-dynamical properties as a consequence of using large fictitious orbital masses in Car–Parrinello simulations, these concerns have already been properly addressed (as discussed for instance in Section 2.4.9 of ref. 27). Another note concerns our choice of the exchange-correlation functional. Plain PBE has been shown to broadly yield accurate and robust results without the need of adding dispersion corrections and in particular for hydrogen-bonded systems the inclusion of (D2 or D3) dispersion corrections has been demonstrated to even significantly increase the average error47. In addition, we carefully checked that the plain PBE functional generates the correct dynamical hypercoordination mechanism1 for structural diffusion of OH− in bulk water at ambient conditions. Moreover, on increasing temperature and pressure of bulk water to 500 K and ≈20 MPa, the essential features of this mechanism were observed to remain unchanged based on carefully analysing the active and resting states in terms of conditional radial distribution functions and the corresponding running coordination numbers in the limits δ<0.1 and δ<0.5 Å, respectively. The only difference worth noting was a slight weakening of the weak hydrogen bond that can be donated via H′ in the active state as revealed by a shoulder instead of a small peak at ≈2 Å. Finally, bonding charge analyses carried out for alkaline solutions revealed no net charge transfer between the mineral layers and the liquid phase across the interface, which is consistent with previous findings for the nanoconfined excess proton34.
The data that support the findings of this study are available from the corresponding author upon request.
How to cite this article: Muñoz-Santiburcio, D. & Marx, D. On the complex structural diffusion of proton holes in nanoconfined alkaline solutions within slit pores. Nat. Commun. 7:12625 doi: 10.1038/ncomms12625 (2016).
This work has been supported by the German Research Foundation (DFG) via the Cluster of Excellence EXC 1069 ‘RESOLV’. We also gratefully acknowledge the Gauss Centre for Supercomputing (GCS) for providing computing time for a GCS Large Scale Project on the IBM Blue Gene/Q system Juqueen48 at Jülich Supercomputing Centre (JSC) as well as HPC-RESOLV and BOVILAB@RUB.