Nanostructured birnessite exhibits high specific capacitance and nearly ideal capacitive behaviour in aqueous electrolytes, rendering it an important electrode material for low-cost, high-power energy storage devices. The mechanism of electrochemical capacitance in birnessite has been described as both Faradaic (involving redox) and non-Faradaic (involving only electrostatic interactions). To clarify the capacitive mechanism, we characterized birnessite’s response to applied potential using ex situ X-ray diffraction, electrochemical quartz crystal microbalance, in situ Raman spectroscopy and operando atomic force microscope dilatometry to provide a holistic understanding of its structural, gravimetric and mechanical responses. These observations are supported by atomic-scale simulations using density functional theory for the cation-intercalated structure of birnessite, ReaxFF reactive force field-based molecular dynamics and ReaxFF-based grand canonical Monte Carlo simulations on the dynamics at the birnessite–water–electrolyte interface. We show that capacitive charge storage in birnessite is governed by interlayer cation intercalation. We conclude that the intercalation appears capacitive due to the presence of nanoconfined interlayer structural water, which mediates the interaction between the intercalated cation and the birnessite host and leads to minimal structural changes.
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Critical role of water structure around interlayer ions for ion storage in layered double hydroxides
Nature Communications Open Access 28 October 2022
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Experimental data (electrochemistry, Raman, XRD, EQCM and AFM) and simulation data (ReaxFF and DFT) are available in this repository: Boyd, S., Ganeshan, K., Tsai, W.-Y., Tao Wu, Saeed, S., Jiang, D., Balke, N., van Duin, A. & Augustyn, V. Effects of interlayer confinement and hydration on capacitive charge storage in birnessite. (Materials Cloud Archive 2021.X, 2021); https://doi.org/10.24435/materialscloud:kh-y2.
The DFT simulations were performed using VASP, which is available under license from VASP (https://www.vasp.at/). The ReaxFF simulations were performed using the ReaxFF module within the ADF code. ADF is available under license from SCM Amsterdam (https://www.scm.com/). Force fields and input files associated with this work can be obtained by a request through the Penn State Materials Computation Center website: https://www.mri.psu.edu/materials-computation-center/connect-mcc.
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This work was supported as part of the Fluid Interface Reactions, Structures and Transport, an Energy Frontier Research Center funded by the US Department of Energy, Office of Science, Basic Energy Sciences at Oak Ridge National Laboratory under contract no. DE-AC0500OR22725 with UT Battelle, LLC (V.A., N.B., D.-E.J. and A.C.T.v.D.). S.B. acknowledges a graduate fellowship through the National Science Foundation Graduate Research Fellowship Program under grant no. 571800. This work was performed in part at the Analytical Instrumentation Facility (AIF) at North Carolina State University, which is supported by the State of North Carolina and the National Science Foundation (award no. ECCS-1542015). The AIF is a member of the North Carolina Research Triangle Nanotechnology Network (RTNN), a site in the National Nanotechnology Coordinated Infrastructure (NNCI). Operando AFM was conducted at the Center for Nanophase Materials Sciences, which is a US Department of Energy Office of Science User Facility.
The authors declare no competing interests.
Peer review information Nature Materials thanks Thierry Brousse, Patrice Simon and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
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Supplementary Figs. 1–17, Tables 1 and 2, and Methods.
Supplementary Video 1
ReaxFF GCMC simulation intercalating K+ cations and H2O molecules in dry MnO2. The local inhomogeneity of species intercalation causes wrinkling of the MnO2 layers.
Supplementary Video 2
ReaxFF GCMC simulation intercalating K+ cations into MnO2·0.25(H2O).
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Boyd, S., Ganeshan, K., Tsai, WY. et al. Effects of interlayer confinement and hydration on capacitive charge storage in birnessite. Nat. Mater. 20, 1689–1694 (2021). https://doi.org/10.1038/s41563-021-01066-4
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