Abstract
The growing interest in potassium ion battery systems is predominantly motivated by the natural abundance of potassium as well as its promising high energy densities ascribed from a low K+/K redox potential. Among the many intercalation hosts, Prussian blue (PB) and its analogues (PBAs) are the most favorable and intriguing earth-abundant hosts for potassium ions. Nickel hexacyanoferrate (NiHCF) is particularly promising due to its low strain and high cycling stability in potassium systems. The exact insertion and de-insertion mechanism of K+ ions into PBA has not yet been fully identified, thus the charge storage mechanism remains poorly understood. This work uses a multiscale investigation strategy highlighted by an in-situ multi-harmonics electrochemical quartz crystal microbalance with dissipation monitoring (EQCM-D) to uncover the dynamic, reversible K+ insertion into NiHCF. Findings reveal an electrolyte concentration dependent stoichiometry for a water-participated K+ insertion and de-insertion. The NiHCF material is subject to a dramatic restructuring merely at high potassium salt concentrations, while a high charge retention is observed through various K salt concentrations. A complicated and dynamic cation-water exchange mechanism is observed pointing to a salt concentration governed microstructural evolution of NiHCF.



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