首页> 外文期刊>The Journal of Chemical Physics >Tetra point wetting of liquid K-KCl mixtures: Spectroscopic characterization of mesoscopic wetting and prewetting films
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Tetra point wetting of liquid K-KCl mixtures: Spectroscopic characterization of mesoscopic wetting and prewetting films

机译:液态K-KCl混合物的四点润湿:介观润湿和预润湿膜的光谱表征

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摘要

The wetting and prewetting transitions at the metal-rich K-KCl melt-sapphire interface have been investigated by spectroscopic ellipsometry in combination with normal incidence felectivity in the spectral range 0.8<=h#omega#<=2.2 eV temperatures up to 730 deg C. Along the coexistence curve a salt-rich liquid wetting film is observed which is identified by the spectral featurse of the liquid state F-center. Unusually thick wetting films are found ranging from 30 nm near 540 deg C to 300 nm approaching the monotectic temperature of 751 deg C. Their composition has been detrmined from the absorption coefficients of the F-center band and it corresponds to about 90 mole % salt. At conditions off coexistence and near the prewetting line, similar mesoscopically thick wetting fillms exist. Crossing the prewetting line towards metal-rich solutions, the optical properties at the interface agree with those of the nearly free electron metal. The high thickness of the prewetting films is qualitatively explainable by charging and double layer formation at the interface. The occurrence of liquid F-center-like states up to 200 K below the monotectic temperature gives evidence of a strong undercooling of the wetting films with respect to the bulk phase. These characteristics of the wetting transition in a metal-molten salt solution can be described by the tetra point wetting scenario for binary fluid mixturs.
机译:已经通过光谱椭圆偏振法结合法向入射折光率在高达730摄氏度的温度范围内0.8 <= h#omega#<= 2.2 eV的温度下研究了富金属K-KCl熔体-蓝宝石界面处的润湿和预润湿过渡沿着共存曲线观察到富含盐的液体润湿膜,该膜由液态F中心的光谱特征确定。发现异常厚的润湿膜的范围从540℃的30 nm到接近751℃的单晶温度的300 nm。其组成已从F中心谱带的吸收系数确定,它对应于约90摩尔%的盐。在不共存且接近预润湿线的条件下,存在类似的介观厚度的润湿填充物。将预润湿线与富金属溶液相交,界面处的光学特性与几乎自由的电子金属的光学特性一致。通过在界面处带电和形成双层,定性地解释了预湿膜的高厚度。在单晶温度以下高达200 K的液态F中心状态的出现,证明了润湿膜相对于本体相有很强的过冷度。金属熔融盐溶液中的润湿转变的这些特征可以通过二元流体混合物的四点润湿方案来描述。

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