Department of Nuclear Science and Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139, USA.
Proc Natl Acad Sci U S A. 2011 Jul 26;108(30):12206-11. doi: 10.1073/pnas.1100238108. Epub 2011 Jul 11.
A neutron scattering technique was developed to measure the density of heavy water confined in a nanoporous silica matrix in a temperature-pressure range, from 300 to 130 K and from 1 to 2,900 bars, where bulk water will crystalize. We observed a prominent hysteresis phenomenon in the measured density profiles between warming and cooling scans above 1,000 bars. We interpret this hysteresis phenomenon as support (although not a proof) of the hypothetical existence of a first-order liquid-liquid phase transition of water that would exist in the macroscopic system if crystallization could be avoided in the relevant phase region. Moreover, the density data we obtained for the confined heavy water under these conditions are valuable to large communities in biology and earth and planetary sciences interested in phenomena in which nanometer-sized water layers are involved.
我们开发了一种中子散射技术,用于测量在温度-压力范围(300 至 130 K,1 至 2900 巴)内,重水在纳米多孔二氧化硅基质中被限制时的密度,在此温度-压力范围内,大部分水会结晶。我们在超过 1000 巴的升温扫描和降温扫描之间的测量密度曲线中观察到明显的滞后现象。我们将这种滞后现象解释为水存在一级液-液相转变的假设存在的支持(尽管不是证明),如果在相关的相区可以避免结晶,则这种相转变将存在于宏观系统中。此外,我们在这些条件下获得的受限重水的密度数据对于生物学、地球和行星科学领域中对涉及纳米级水层的现象感兴趣的大型社区具有重要价值。