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Sulfur dioxide dry deposition on the loess surface-surface reaction concept for measuring dry deposition flux

机译:黄土表面二氧化硫干沉降概念-用于测量干沉降通量

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As an effort to obtain more extensive data on sulfur dioxide dry deposition in northern China, experiments were carried out in Beijing by trying a new approach to the deposition flux determination. In this approach we determined the flux by a traditional concentration gradient method in the cases where the wind velocity profile conformed to the logarithmic law. In the cases outside the efficacy of the logarithmic law, in which considerable difficulty had been experienced in the traditional method, we resorted to a new concept of regarding the deposition as a reaction between sulfur dioxide and the ground surface. We introduced a mathematical model for the surface reaction, and, determining the reaction parameters on the basis of the logarithmic wind profile data, used the model to evaluate the flux in the non-logarithmic law cases. This method should enable us to obtain the dry deposition data for much more situations, including those which are difficult to be dealt with by the traditional method.
机译:为了获得有关中国北方地区二氧化硫干式沉积的更多数据,尝试在北京通过尝试一种新的沉积通量测定方法来进行实验。在这种方法中,在风速剖面符合对数律的情况下,我们通过传统的浓度梯度方法确定了通量。在对数定律无效的情况下,传统方法遇到了相当大的困难,我们诉诸了一种新的概念,将沉积视为二氧化硫与地面之间的反应。我们引入了表面反应的数学模型,并根据对数风廓线数据确定了反应参数,并使用该模型评估了非对数律情况下的通量。这种方法应该使我们能够获得更多情况下的干法沉积数据,包括那些传统方法难以处理的情况。

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