Abstract
Pressure-induced formation of amorphous ices and the low-density amorphous (LDA) to high-density amorphous (HDA) transition have been believed to occur kinetically below a crossover temperature () above which thermodynamically driven crystalline-crystalline (e.g., ice -to-II) transitions and crystallization of HDA and LDA are dominant. Here we show compression-rate-dependent formation of a high-density noncrystalline (HDN) phase transformed from ice above , bypassing crystalline-crystalline transitions under rapid compression. Rapid decompression above transforms HDN to a low-density noncrystalline (LDN) phase which crystallizes spontaneously into ice , whereas slow decompression of HDN leads to direct crystallization. The results indicate the formation of HDA and the HDN-to-LDN transition above are results of competition between (de)compression rate, energy barrier, and temperature. The crossover temperature is shown to have an exponential relationship with the threshold compression rate. The present results provide important insight into the dynamic property of the phase transitions in addition to the static study.
- Received 11 June 2018
DOI:https://doi.org/10.1103/PhysRevLett.121.225703
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