Abstract
According to liquid-liquid critical point hypothesis of water, liquid separates into low- and high-density liquid phases at low temperature and high pressure, and these liquid phases become known low- and high-density amorphous ices below their glass transition temperatures. An accumulation of experimental and theoretical results seems to support this hypothesis, and this hypothesis may virtually explain the mysteries of water including density maximum at 277 K. Aqueous solutions and confined appear to be readily interpreted on hypothesis.
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