Masuda Kaori, Haramaki Taishiro, Nakashima Satoru, Habert Bertrand, Martinez Isabelle, Kashiwabara Seiichi
Interactive Research Center of Science, Tokyo Institute of Technology, O-okayama 2-12-1, Meguro, Tokyo 152-8551, Japan.
Appl Spectrosc. 2003 Mar;57(3):274-81. doi: 10.1366/000370203321558173.
The attenuated total reflectance infrared (ATR-IR) spectra of several aqueous solutions have been measured by using a newly developed heatable rod-type ATR cell. The OH stretching bands showed systematic change with increasing solute concentrations and these changes can be explained by four different OH components based on curve-fitting results. NaCl solutions show longer H-bond distance character, while carbonate solutions present shorter ones. The Na2CO3 1 M solution conserves this shorter H-bond nature up to 100 degrees C. On the other hand, the loose nature of NaCl solutions becomes less pronounced at higher temperatures because of the dissociation of pure water clusters. These in situ observations of water structures are generally in agreement with the expected nature of fluids within the earth.
使用新开发的可加热棒型衰减全反射红外(ATR-IR)池测量了几种水溶液的衰减全反射红外光谱。OH伸缩带随溶质浓度增加呈现出系统性变化,基于曲线拟合结果,这些变化可用四种不同的OH组分来解释。NaCl溶液表现出较长的氢键距离特征,而碳酸盐溶液呈现较短的氢键距离特征。1 M的Na2CO3溶液在高达100℃时仍保持这种较短的氢键性质。另一方面,由于纯水团簇的解离,NaCl溶液在较高温度下的松散性质变得不那么明显。这些对水结构的原位观察总体上与地球内部流体的预期性质一致。