首页> 外文期刊>The Journal of Chemical Physics >Evidence for a liquid-liquid critical point in supercooled water within the E3B3 model and a possible interpretation of the kink in the homogeneous nucleation line
【24h】

Evidence for a liquid-liquid critical point in supercooled water within the E3B3 model and a possible interpretation of the kink in the homogeneous nucleation line

机译:E3B3模型中过冷水中液-液临界点的证据以及均相成核线中的扭结的可能解释

获取原文
获取原文并翻译 | 示例
           

摘要

Supercooled water exhibits many thermodynamic anomalies, and several scenarios have been proposed to interpret them, among which the liquid-liquid critical point (LLCP) hypothesis is the most commonly discussed. We investigated Widom lines and the LLCP of deeply supercooled water, by using molecular dynamics simulation with a newly reparameterized water model that explicitly includes three-body interactions. Seven isobars are studied from ambient pressure to 2.5 kbar, and Widom lines are identified by calculating maxima in the coefficient of thermal expansion and the isothermal compressibility (both with respect to temperature). From these data we estimate that the LLCP of the new water model is at 180 K and 2.1 kbar. The oxygen radial distribution function is calculated along the 2 kbar isobar. It shows a steep change in the height of its second peak between 180 and 185 K, which indicates a transition between the high-density liquid and low-density liquid phases and which is consistent with the ascribed location of the critical point. The good agreement of the height of the second peak of the radial distribution function between simulation and experiment at 1 bar, as a function of temperature, supports the validity of the model. The location of the LLCP within the model is close to the kink in the experimental homogeneous nucleation line. We use existing experimental data to argue that the experimental LLCP is at 168 K and 1.95 kbar and speculate how this LLCP and its Widom line might be responsible for the kink in the homogeneous nucleation line. Published by AIP Publishing.
机译:过冷水表现出许多热力学异常,并提出了几种方案来解释它们,其中最常讨论的是液-液临界点(LLCP)假设。我们通过使用分子动力学模拟以及新近重新参数化的水模型来研究Widom线和深冷水的LLCP,该模型明确包括三体相互作用。研究了从环境压力到2.5 kbar的七个等压线,并通过计算热膨胀系数和等温可压缩性(相对于温度)的最大值来识别Widom线。根据这些数据,我们估计新水模型的LLCP为180 K和2.1 kbar。沿2 kbar等压线计算氧径向分布函数。它显示出其第二个峰的高度在180至185 K之间发生了急剧变化,这表明高密度液相和低密度液相之间存在过渡,并且与临界点的指定位置一致。模拟和实验在1 bar下径向分布函数第二个峰的高度与温度的关系很好,证明了模型的有效性。 LLCP在模型内的位置靠近实验均匀成核线中的扭结。我们使用现有的实验数据来论证实验LLCP处于168 K和1.95 kbar,并推测该LLCP及其Widom线可能如何造成均相成核线中的扭结。由AIP Publishing发布。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号