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Testing the radon-in-water probe set-up for the measurement of radon in water bodies

机译:测试水体中氡测量的氡水探针设置

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Naturally occurring Rn-222 is increasingly recognized as a powerful environmental tracer in hydrology. Radon-in-water concentrations can be measured in the field by stripping radon from a water sample into a gas volume and measuring the respective radon-in-gas concentration using a portable radon-in-gas monitor. Alternatively, radon is firstly extracted from the water body by diffusion through a radon exchanger such as polypropylene (PP) tubing and then is measured using a radon-in-gas monitor, connected in closed-loop to the PP membrane. The paper discusses results of field experiments in which the Radon-in-Water Probe (Durridge co.), a 2.2 m long PP tubing, connected to a RAD7 monitor (method A), is used to determine dissolved radon concentration in four water bodies characterised by different water flow velocity and radon concentration. The efficiency of this method is validated by comparison with two established methods, gamma-ray spectrometer + charcoal canister (method B) and RAD7 monitor + Big Bottle RAD H20 accessory (method C). Relative efficiency of method A is directly proportional to water flow velocity, ranging from about 0.50 +/- 0.05 at 0.01 m/s to about 0.92 +/- 0.08 at 0.57 m/s. A minimum of 2-3 h are needed to collect enough records to asymptotically fit radonin-gas data and obtain equilibrium radon concentration, which is then converted into radon-in water concentration, considering the temperature-dependency of radon partition coefficient between water and air. Equilibrium condition is reached after about 6-8 h. No correlation was found between relative efficiency and radon concentration. An equation is proposed to correct radon data as a function of water flow velocity, even for poorly moving water bodies. The DURRIDGE Water Probe is useful to monitor radon-in-water levels, without the potential risk of radon loss during water sampling and sample handling. However, it must be pointed out that duplicate or triplicate sampling using other methods similarly permit to evaluate whether radon loss is an issue.
机译:当然,当时的RN-222越来越被认为是水文中强大的环境示踪剂。可以通过将氡从水样中剥离到气体体积并使用便携式氡气监测器测量相应的氡气浓度来测量氡水浓度。或者,通过通过扩散通过诸如聚丙烯(PP)管的氡交换器的扩散从水体中从水体中提取氡,然后使用氡气监视器以闭环连接到PP膜。本文讨论了现场实验的结果,其中氡水探针(Durridge Co.),连接到Rad7监测器(方法A)的2.2M长的PP管道,用于确定四个水体中的溶解氡浓度以不同的水流速度和氡浓度为特征。通过与两种建立的方法,伽马射线光谱仪+木炭罐(方法B)和RAD7监测+大瓶RAD H20附件(方法C),通过比较验证该方法的效率。方法A的相对效率与水流速成比例,范围为0.01m / s的0.01m / s至约0.92 +/- 0.08,0.57m / s。需要至少2-3小时来收集足够的记录到渐近贴合的氡气数据,并获得平衡氡浓度,然后将其转化为氡水浓度,考虑到水和空气之间的氡分配系数的温度依赖性。大约6-8小时后达到平衡条件。在相对效率和氡浓度之间没有发现相关性。提出了一种等式,以将氡数据校正作为水流速的函数,即使对于移动的水体不良。 Durridge水探针可用于监测水氡水平,而无需在水采样过程中氡损失的潜在风险和样品处理。但是,必须指出使用其他方法的重复或三份抽样类似地允许评估氡损失是否是一个问题。

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