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地面－大气界面的氡析出通量是为了环境目的和关于矿山前瞻性选址所共同需要的测量量之一。有许多方法可以进行这样的测量。通常使用“累积”技术。这种方法要求容器开口的一端朝下放在地面上，确定容器内给定时间的氡活度，用闪烁瓶取该容器内的空气样品估算氡浓度。本工作的目的是使用其他的氡浓度测量技术简化这一方法。用常规方法进行的通量测量，作为标准方法（定点取样）与使用硅探测器（连续测量）测量的结果和使用固态径迹探测器（累积测量）的测量结果作了比较。对后面两种方法，为了获得标准方法提供的２２２Ｒｎ析出通量的真实值，用了一个校正因子。
Radon flux at the ground-atmosphere interface is one of the measurements commonly needed for environmental purposes and for prospective sites in mines. There are many ways to make such a measurement. Usually use “cumulative” technology. This method requires that the open end of the container be placed on the ground with one end facing down, to determine the radon activity at a given time in the container, and to estimate the radon concentration using scintillation vials of the air sample in the container. The purpose of this work is to simplify this method using other radon concentration measurement techniques. Flux measurements using the conventional method were compared as a standard method (spot sampling) with the results measured using a silicon detector (continuous measurement) and the measurement using a solid state track detector (cumulative measurement). For the latter two methods, a correction factor is used in order to obtain the true value of the 222Rn precipitation flux provided by the standard method.