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Quantitative measurements of nanoscale thin frost layers using surface plasmon resonance imaging

机译:使用表面等离子共振成像定量测量纳米级薄霜层

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This study reports the presence of a nanoscale thin frost layer. During the frosting process, the surface plasmon resonance (SPR) imaging method can be used to overcome conventional optical limits and quantify this layer. The research outlined here also provides quantitative thickness measurement of the thin frost layer via a proposed calibration method based on the measured SPR intensity. The SPR system established in this study consists of a 50 nm gold-coated BK7 cover glass, a prism, a light source, a polarizer, a lens and a filter for the collimated light of a 600 +/- 5 nm wavelength, and a CCD camera. The SPR angle of the ice phase is 72, which corresponds to the ice refractive index of 1.307. The gold-glass specimen is cooled from room temperature (23 +/- 1 degrees C) to -4.0 +/- 0.8 degrees C by using a thermoelectric cooler to maintain the relative humidity of 20 +/- 3% (at the room temperature). As a result, it is found that the nanoscale thin frost layer between the frozen condensates exists on the surface. Also, the present study yields the spatial distribution of reflectance that is associated with the frost layer thickness, indicating that the local information about thin frost layer thickness can be obtained through this SPR imaging method. It is found that the SPR imaging method enables successful capture of the depthwise spatial variations of the thin frost layer, showing that the frost layer was grown over time as a result of the de-sublimation of water vapor. (C) 2018 Elsevier Ltd. All rights reserved.
机译:这项研究报告了纳米级薄霜层的存在。在结霜过程中,表面等离振子共振(SPR)成像方法可用于克服常规光学限制并量化该层。本文概述的研究还通过基于测得的SPR强度的建议校准方法,提供了薄霜层的定量厚度测量。本研究中建立的SPR系统由50 nm镀金BK7盖玻片,棱镜,光源,偏振镜,透镜和滤光片组成,用于600 +/- 5 nm波长的准直光,以及CCD相机。冰相的SPR角为72,对应于1.307的冰折射率。通过使用热电冷却器将金玻璃样品从室温(23 +/- 1摄氏度)冷却到-4.0 +/- 0.8摄氏度,以保持20 +/- 3%的相对湿度(在室温下) )。结果,发现在冷冻冷凝物之间的纳米级薄霜层存在于表面上。此外,本研究还得出了与霜层厚度相关的反射率的空间分布,这表明可以通过此SPR成像方法获得有关薄霜层厚度的局部信息。发现SPR成像方法能够成功捕获薄霜层的深度空间变化,表明霜层是由于水蒸气的升华而随时间增长的。 (C)2018 Elsevier Ltd.保留所有权利。

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