Clarke A D
Appl Opt. 1982 Aug 15;21(16):3011-20. doi: 10.1364/AO.21.003011.
A new technique has been developed for determination of optical depths delta(a) as low as 0.0005 for thin layers of absorbing materials or particles. The measurement involves optical amplification of the absorption and is not affected by the scattering properties of the absorber. This is accomplished by introducing the absorber into the virtually isotropic radiation field between two high-reflectance diffusing wafers and measuring the resultant attenuation of the transmitted light. The technique has been directed toward determination of the absorption coefficient of atmospheric aerosols in remote and relatively unpolluted locations. Provided appropriate collection filters and sampling conditions are used, the method can establish an absorption coefficient for the aerosol as low as 5 x 10(-9) m(-1) within a 10-h sampling period. A proportionally higher absorption coefficient requires proportionally less sample time. This paper discusses instrument design, the theoretical optical model, laboratory calibration, and a field test of the technique.
已开发出一种新技术,用于测定吸收性材料或颗粒薄层的光学深度δ(a),低至0.0005。该测量涉及吸收的光学放大,且不受吸收体散射特性的影响。这是通过将吸收体引入两个高反射率漫射晶片之间的几乎各向同性辐射场,并测量透射光的衰减来实现的。该技术已用于测定偏远且相对未受污染地区大气气溶胶的吸收系数。如果使用适当的收集过滤器和采样条件,该方法可在10小时的采样期内确定低至5×10(-9) m(-1)的气溶胶吸收系数。成比例更高的吸收系数需要成比例更少的采样时间。本文讨论了该技术的仪器设计、理论光学模型、实验室校准和现场测试。