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用反射增强二维红外光谱法观察空气/水界面的朗缪尔单层超快至超慢动力学。

Ultrafast to Ultraslow Dynamics of a Langmuir Monolayer at the Air/Water Interface Observed with Reflection Enhanced 2D IR Spectroscopy.

机构信息

Department of Chemistry, Stanford University , Stanford, California 94305, United States.

出版信息

J Am Chem Soc. 2017 Nov 22;139(46):16518-16527. doi: 10.1021/jacs.7b06602. Epub 2017 Nov 10.

Abstract

Monolayers play important roles in naturally occurring phenomena and technological processes. Monolayers at the air/water interface have received considerable attention, yet it has proven difficult to measure monolayer and interfacial molecular dynamics. Here we employ a new technique, reflection enhanced two-dimensional infrared (2D IR) spectroscopy, on a carbonyl stretching mode of tricarbonylchloro-9-octadecylamino-4,5-diazafluorenerhenium(I) (TReF18) monolayers at two surface densities. Comparison to experiments on a water-soluble version of the metal carbonyl headgroup shows that water hydrogen bond rearrangement dynamics slow from 1.5 ps in bulk water to 3.1 ps for interfacial water. Longer time scale fluctuations were also observed and attributed to fluctuations of the number of hydrogen bonds formed between water and the three carbonyls of TReF18. At the higher surface density, two types of TReF18 minor structures are observed in addition to the main structure. The reflection method can take usable 2D IR spectra on the monolayer within 8 s, enabling us to track the fluctuating minor structures' appearance and disappearance on a tens of seconds time scale. 2D IR chemical exchange spectroscopy further shows these structures interconvert in 30 ps. Finally, 2D spectral line shape evolution reveals that it takes the monolayers hours to reach macroscopic structural equilibrium.

摘要

单层在自然现象和技术过程中起着重要作用。空气/水界面上的单层受到了相当多的关注,但很难测量单层和界面分子动力学。在这里,我们在两个表面密度下,使用一种新的技术,即反射增强二维红外(2D IR)光谱,对三羰基氯-9-十八氨基-4,5-二氮杂氟烯钌(I)(TReF18)单层的羰基伸缩模式进行了研究。与金属羰基头基水溶性版本的实验相比,水氢键重排动力学从在体相水中的 1.5 ps 减慢到界面水中的 3.1 ps。还观察到更长时间尺度的波动,并归因于水和 TReF18 的三个羰基之间形成的氢键数量的波动。在较高的表面密度下,除了主要结构外,还观察到两种类型的 TReF18 次要结构。反射法可以在 8 s 内对单层获得可用的 2D IR 光谱,使我们能够跟踪几十秒时间尺度上波动的次要结构的出现和消失。二维红外化学交换光谱进一步表明,这些结构在 30 ps 内相互转换。最后,二维光谱线形状演化表明,单层需要数小时才能达到宏观结构平衡。

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