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Measurement of light absorption by aquatic particles: improvement of the quantitative filter technique by use of an integrating sphere approach

机译:测量水生颗粒的光吸收:使用积分球方法改进定量滤光片技术

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Determination of particulate absorption in natural waters is often made by measuring the transmittance of samples on glass-fiber filters with the so-called quantitative filter technique (QFT). The accuracy of this technique is limited due to variations in the optical properties of the sample/filter composite, and due to uncertainties in the path-length amplification induced by multiple scattering inside the filter. Some variations in the optical properties of the sample/filter composite can be compensated by additional measurements of the filter's reflectance (transmittance-reflectance method [T-R] [S. Tassan and G. M. Ferrari, Limnol. Oceanogr. 40, 1358 (1995)]). We propose a different, rarely used approach, namely to measure the filter's absorptance in the center of a large integrating sphere, to avoid problems with light losses due to scattering. A comparison with other QFTs includes a sensitivity study for different error sources and determination of path-length amplification factors for each measurement technique. Measurements with a point-source integrating-cavity absorption meter were therefore used to determine the true absorption. Filter to filter variability induced a much lower error in absorptance compared to a measured transmittance. This reduced error permits more accurate determination of the usually low absorption coefficient in the near IR spectral region. The error of the T-R method was lower than that of the transmittance measurement but slightly higher than that of an absorptance measurement. The mean path-length amplification was much higher for the absorptance measurement compared to the T-R method (4.50 versus 2.45) but was found to be largely independent of wavelength and optical density. With natural samples the path-length amplification was less variable for the absorptance measurement, reducing the overall error for absorption to less than +-14percent, compared to +-25percent for the T-R method.
机译:通常通过使用所谓的定量过滤技术(QFT)测量玻璃纤维过滤器上样品的透射率来确定天然水中的颗粒吸收率。由于样品/滤光片复合材料光学特性的变化,以及由于滤光片内部多次散射引起的光程长度放大的不确定性,该技术的准确性受到限制。样品/滤光片复合材料光学性能的一些变化可以通过滤光片反射率的其他测量方法来补偿(透射率-反射率方法[TR] [S. Tassan和GM Ferrari,Limnol。Oceanogr。40,1358(1995)]) 。我们提出了一种不同的,很少使用的方法,即在大积分球的中心测量滤光片的吸收率,以避免由于散射造成的光损耗问题。与其他QFT的比较包括针对不同误差源的灵敏度研究,以及针对每种测量技术确定路径长度放大因子。因此,使用点源积分腔吸收仪进行测量来确定真实吸收。与测量的透射率相比,滤波器到滤波器的可变性引起的吸收率误差要低得多。这种减小的误差允许更准确地确定在近红外光谱区域中通常较低的吸收系数。 T-R法的误差低于透射率测量的误差,但略高于吸收率测量的误差。与T-R方法相比,吸收率测量的平均光程长度放大倍数要高得多(4.50对2.45),但是发现它与波长和光密度基本无关。对于天然样品,吸收率测量的光程长度放大变化较小,与T-R方法的+ -25%相比,吸收的总误差降低到+ -14%以下。

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