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改进天然水中氡(222Rn)和钍(220Rn)的自动化分析。

Improved automated analysis of radon (222Rn) and thoron (220Rn) in natural waters.

机构信息

Department of Oceanography, Florida State University, Tallahassee, Florida 32306, USA.

出版信息

Environ Sci Technol. 2009 Nov 15;43(22):8599-603. doi: 10.1021/es902045c.

Abstract

Natural radon ((222)Rn) and thoron ((220)Rn) can be used as tracers of various chemical and physical processes in the environment. We present here results from an extended series of laboratory experiments intended to improve the automated analysis of (222)Rn and (220)Rn in water using a modified RAD AQUA (Durridge Inc.) system. Previous experience with similar equipment showed that it takes about 30-40 min for the system to equilibrate to radon-in-water concentration increases and even longer for the response to return to baseline after a sharp spike. While the original water/gas exchanger setup was built only for radon-in-water measurement, our goal here is to provide an automated system capable of high resolution and good sensitivity for both radon- and thoron-in-water detections. We found that faster water flow rates substantially improved the response for both isotopes while thoron is detected most efficiently at airflow rates of 3 L/min. Our results show that the optimum conditions for fastest response and sensitivity for both isotopes are at water flow rates up to 17 L/min and an airflow rate of 3 L/min through the detector. Applications for such measurements include prospecting for naturally occurring radioactive material (NORM) in pipelines and locating points of groundwater/surface water interaction.

摘要

天然氡 ((222)Rn) 和钍 ((220)Rn) 可作为环境中各种化学和物理过程的示踪剂。我们在此展示了一系列扩展的实验室实验结果,旨在改进使用改良 RAD AQUA(Durridge Inc.)系统自动分析水中 (222)Rn 和 (220)Rn 的方法。使用类似设备的先前经验表明,系统需要大约 30-40 分钟才能达到水中氡浓度增加的平衡,并且在尖锐峰值后响应恢复基线需要更长的时间。虽然原始的水/气交换器设置仅用于水中氡测量,但我们的目标是提供一种自动化系统,能够对水中的氡和钍进行高分辨率和高灵敏度的检测。我们发现,更快的水流速度可大大改善两种同位素的响应,而在 3 L/min 的气流速率下,钍的检测效率最高。我们的结果表明,对于两种同位素,最快响应和灵敏度的最佳条件是在水流量高达 17 L/min 和通过探测器的气流速率为 3 L/min 的情况下。这种测量的应用包括在管道中探测天然放射性物质 (NORM) 和定位地下水/地表水相互作用的点。

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