An external electric field induces a reversible transition from mobile non-wetting water to an ordered hexagonal monolayer ice on graphite via interfacial charge redistribution, enabling deterministic nucleation, lattice strain, discrete conductance states, and collective dipolar switching.
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Increasing dipolar strength drives magnetic active matter from free swimming into clustered states, implying an upper bound on useful magnetosome-chain moments beyond which magnetotactic performance declines.
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Electric-field control of hydrogen bonding via interfacial charge at atomic resolution
An external electric field induces a reversible transition from mobile non-wetting water to an ordered hexagonal monolayer ice on graphite via interfacial charge redistribution, enabling deterministic nucleation, lattice strain, discrete conductance states, and collective dipolar switching.
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Macroscopic bioinspired magnetic active matter and the physical limits of magnetotaxis
Increasing dipolar strength drives magnetic active matter from free swimming into clustered states, implying an upper bound on useful magnetosome-chain moments beyond which magnetotactic performance declines.