地表波谱比辐射率便携式测量的三种改进方法
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1. 中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室 2.中国科学院研究生院,中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室,中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室,中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室,中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室,1. 中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室 2.中国科学院研究生院

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自然科学基金项目(41171286)国家重点基础研究发展计划项目(2010CB428403);中科院知识创新工程重点项目(KZCX2-YW-326-1)和中科院百人计划项目


Three improved methods for measuring spectral emissivity based on the FTIR spectrometer
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1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS 2. Graduate University of Chinese Academy of Sciences,1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS,1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS,1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS,1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS,1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS 2. Graduate University of Chinese Academy of Sciences

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    摘要:

    针对便携式傅里叶变换红外光谱仪测量比辐射率的不确定性,提出了三种改进的波谱比辐射率测量方法.方法1和方法2借助于附加设备改变环境辐照度实现病态方程可解.方法3基于灰体假设,使用迭代求解获得最接近样品的真实温度的温度解,进而计算得到样品的比辐射率.使用温度测量和傅里叶光谱仪观测计算获得波谱比辐射率作为参考的比辐射率结果,对三种改进的方法进行对比和验证.结果表明,对于高比辐射率的石英板和纸板,三种改进方法的测量结果和参考值吻合较好.而对于低比辐射率的锈铁板和铝板,方法3最为接近参考比辐射率结果,而方法1,方法2由于需要过多的观测环节,存在一定的偏差.此三种方法将为改进便携式傅里叶变换红外光谱仪测量提供依据.

    Abstract:

    To minimize the uncertainties related to the FTIR spectrometer, three improved methods were proposed to measure the spectral emissivity. For method 1 (M1) and method 2 (M2), an invented device was used to change the environment radiation which makes the ill conditioned equation solvable. Method 3 (M3) is based on the gray body assumption, and an iterative procedure was applied to derive the temperature of samples, then the spectral emissivity can be retrieved based on this temperature and the FTIR measurements. In order to validate these methods, the emissivity derived from the measured temperature was used as a reference. The results indicate that for the samples with high emissivity, such as quartz plates and cardboard, three improved methods have comparable accuracy; while for the samples with low emissivity, such as rusty iron plate and aluminum plate, the M3 is more reliable than the other two methods. M1 and M2 need to go through more procedures than M3, and this may lead to some deviation from the reality. Overall, three improved methods greatly improved the spectral emissivity measurements with FTIR spectrometer.

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杨永民,张仁华,苏红波,田静,陈少辉,荣媛.地表波谱比辐射率便携式测量的三种改进方法[J].红外与毫米波学报,2013,32(4):366~371]. YANG Yong-Min, ZHANG Ren-Hua, SU Hong-Bo, TIAN Jing, CHEN Shao-Hui, RONG Yuan. Three improved methods for measuring spectral emissivity based on the FTIR spectrometer[J]. J. Infrared Millim. Waves,2013,32(4):366~371.]

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  • 收稿日期:2012-04-06
  • 最后修改日期:2012-10-24
  • 录用日期:2012-08-13
  • 在线发布日期: 2013-08-29
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