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受限过冷水的振动动力学

Vibrational dynamics of confined supercooled water.

作者信息

Stefanutti E, Bove L E, Alabarse F G, Lelong G, Bruni F, Ricci M A

机构信息

Sorbonne Université, Muséum National d'Histoire Naturelle, UMR CNRS 7590, IRD, Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, IMPMC, 4 Place Jussieu, 75005 Paris, France.

Dipartimento di Scienze, Università Degli Studi Roma Tre, Via della Vasca Navale 84, 00146 Roma, Italy.

出版信息

J Chem Phys. 2019 Jun 14;150(22):224504. doi: 10.1063/1.5094147.

Abstract

The quest for a possible liquid-liquid coexistence line in supercooled water below its homogeneous nucleation temperature is faced by confining water within a porous silica substrate (MCM-41). This system is investigated by synchrotron radiation infrared spectroscopy, exploring both the intramolecular and the intermolecular vibrational dynamics, in the temperature range from ambient down to ∼120 K, along several isobaric paths between 0.7 kbar and 3.0 kbar. Upon lowering the temperature, the OH-stretching band shows that the intramolecular vibrational dynamics continuously evolves from predominantly liquidlike to predominantly icelike. An abrupt change in the line shape of the intermolecular vibrational band between 220 K and 240 K, depending on the pressure, is the signature of nucleation of ice within the MCM-41 pores. These findings do not support the presence of two liquid phases and provide evidence for the coexistence of liquid water and ice in water confined in MCM-41.

摘要

在低于其均匀成核温度的过冷水体系中探寻可能存在的液 - 液共存线时,是将水限制在多孔二氧化硅基质(MCM - 41)中进行研究的。通过同步辐射红外光谱对该体系进行研究,在0.7千巴至3.0千巴之间的几条等压路径上,探索了从环境温度到约120 K温度范围内分子内和分子间的振动动力学。随着温度降低,OH伸缩带表明分子内振动动力学从主要类似液态持续演变为主要类似冰态。分子间振动带在220 K至240 K之间的线形突然变化(取决于压力),是MCM - 41孔隙内冰成核的特征。这些发现不支持存在两个液相,并为限制在MCM - 41中的水中液态水和冰的共存提供了证据。

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