Shi Rui, Tanaka Hajime
Department of Physics, Zhejiang University, Hangzhou 310027, China.
Department of Fundamental Engineering, Institute of Industrial Science, University of Tokyo, Tokyo 153-8505, Japan.
Proc Natl Acad Sci U S A. 2020 Oct 27;117(43):26591-26599. doi: 10.1073/pnas.2008426117. Epub 2020 Oct 15.
The origin of water's anomalies has been a matter of long-standing debate. A two-state model, dating back to Röntgen, relies on the dynamical coexistence of two types of local structures-locally favored tetrahedral structure (LFTS) and disordered normal-liquid structure (DNLS)-in liquid water. Phenomenologically, this model not only explains water's thermodynamic anomalies but also can rationalize the existence of a liquid-liquid critical point (LLCP) if there is a cooperative formation of LFTS. We recently found direct evidence for the coexistence of LFTS and DNLS in the experimental structure factor of liquid water. However, the existence of the LLCP and its impact on water's properties has remained elusive, leaving the origin of water's anomalies unclear. Here we propose a unique strategy to locate the LLCP of liquid water. First, we make a comprehensive analysis of a large set of experimental structural, thermodynamic, and dynamic data based on our hierarchical two-state model. This model predicts that the two thermodynamic and dynamical fluctuation maxima lines should cross at the LLCP if it exists, which we confirm by hundred-microsecond simulations for model waters. Based on recent experimental results of the compressibility and diffusivity measurements in the no man's land, we reveal that the two lines cross around 184 K and 173 MPa for real water, suggesting the presence of the LLCP around there. Nevertheless, we find that the criticality is almost negligible in the experimentally accessible region of liquid water because it is too far from the LLCP. Our findings would provide a clue to settle the long-standing debate.
水的异常现象的起源一直是长期争论的话题。一个可追溯到伦琴的双态模型,依赖于液态水中两种局部结构——局部有利的四面体结构(LFTS)和无序的正常液体结构(DNLS)——的动态共存。从现象学角度来看,该模型不仅解释了水的热力学异常现象,而且如果存在LFTS的协同形成,还能解释液-液临界点(LLCP)的存在。我们最近在液态水的实验结构因子中发现了LFTS和DNLS共存的直接证据。然而,LLCP的存在及其对水性质的影响仍然难以捉摸,这使得水异常现象的起源尚不清楚。在此,我们提出一种独特的策略来确定液态水的LLCP。首先,我们基于分层双态模型对大量实验结构、热力学和动力学数据进行全面分析。该模型预测,如果存在LLCP,两条热力学和动力学涨落最大值线应该在LLCP处相交,我们通过对模型水进行的百微秒模拟证实了这一点。基于最近在“无人区”进行的压缩性和扩散率测量的实验结果,我们发现对于真实的水,这两条线在184 K和173 MPa左右相交,表明在该区域附近存在LLCP。然而,我们发现,在液态水的实验可及区域内,临界性几乎可以忽略不计,因为它离LLCP太远了。我们的发现将为解决长期存在的争论提供线索。