Komatsu Kazuki, Machida Shinichi, Noritake Fumiya, Hattori Takanori, Sano-Furukawa Asami, Yamane Ryo, Yamashita Keishiro, Kagi Hiroyuki
Geochemical Research Center, Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-0033, Japan.
Neutron Science and Technology Center, CROSS, 162-1 Shirakata, Tokai, Naka, Ibaraki, 319-1106, Japan.
Nat Commun. 2020 Feb 3;11(1):464. doi: 10.1038/s41467-020-14346-5.
Water freezes below 0 °C at ambient pressure ordinarily to ice I, with hexagonal stacking sequence. Under certain conditions, ice with a cubic stacking sequence can also be formed, but ideal ice I without stacking-disorder has never been formed until recently. Here we demonstrate a route to obtain ice I without stacking-disorder by degassing hydrogen from the high-pressure form of hydrogen hydrate, C, which has a host framework isostructural with ice I. The stacking-disorder free ice I is formed from C via an intermediate amorphous or nano-crystalline form under decompression, unlike the direct transformations occurring in ice XVI from neon hydrate, or ice XVII from hydrogen hydrate. The obtained ice I shows remarkable thermal stability, until the phase transition to ice I at 250 K, originating from the lack of dislocations. This discovery of ideal ice I will promote understanding of the role of stacking-disorder on the physical properties of ice as a counter end-member of ice I.
在环境压力下,水通常在0°C以下冻结成具有六方堆积序列的冰I。在某些条件下,也可以形成具有立方堆积序列的冰,但直到最近,从未形成过没有堆积无序的理想冰I。在这里,我们展示了一种通过从高压形式的水合氢C中脱除氢来获得没有堆积无序的冰I的方法,水合氢C具有与冰I同构的主体框架。与从氖水合物形成的冰XVI或从水合氢形成的冰XVII中发生的直接转变不同,在减压下,没有堆积无序的冰I是由C通过中间的非晶态或纳米晶态形成的。所获得的冰I显示出显著的热稳定性,直到在250K时发生向冰I的相变,这源于位错的缺乏。理想冰I的这一发现将促进对堆积无序在作为冰I的反端元的冰的物理性质上所起作用的理解。