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Abstract The study of superionic (SI) water has been a highly active research area since its theoretical prediction. Despite significant experimental and computational efforts, its melting curve and the stability of different oxygen lattices remain debated, impacting our understanding of SI ice’s peculiar transport properties. Experimental results at lower pressures show disagreement, whereas data at higher pressures are scarce due to the extreme challenges of such experiments.
Since Bancroft1 first reported shock-induced polymorphism over fifty years ago, solid–solid and solid–liquid phase transitions have been the focus of innumerable shock-compression studies. Velocimetry techniques have been key diagnostic tools in the inference of such phase transitions, with plateaus in density interpreted as plastic deformation or phase transitions.
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