Public Health

Radon: A Tracer for Geological, Geophysical and Geochemical by Mark Baskaran

By Mark Baskaran

This publication studies all of the significant examine accomplishments and summarizes the several purposes of radon. It serves as a superb reference ebook for researchers who're attracted to the U-series radionuclides and noble gases as tracers and chronometers. Radon has been greatly applied as a strong tracer to quantify a couple of strategies that come with fuel alternate charges among air and water, submarine groundwater discharge in coastal waters, water alternate among rivers and lakes, ocean circulate, hydrocarbon and uranium exploration. it's also used as an atmospheric tracer for the id and quantification of air lots and as a device for earthquake prediction, and so forth. a good portion of the booklet provides state-of-the wisdom on indoor-radon-related healthiness concerns. purposes of the decay-series of Rn-222 are provided in a bankruptcy. It serves as a reference and a cutting-edge source for researchers who are looking to research different functions of radon in Earth systems.

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Additional resources for Radon: A Tracer for Geological, Geophysical and Geochemical Studies

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5) analyses 222Rn from a constant stream of water passing through an air-water exchanger (“RAD-AQUA”) that distributes radon from the running water to a closed air loop. The air stream is fed to a RAD7 that determines the activity of 222Rn by electrostatic collection and measurement of the α-emitting daughters, 214Po and 218Po (220Rn, if present, may be detected by integrating counts in the 216Po region; Burnett et al. 2007; Dimova et al. 2009). Since the distribution of radon at equilibrium between the air and water phases is governed by a now well-known temperature and salinity dependence (Schubert et al.

The passive detectors, which are quite inexpensive, are examples of integrating techniques. Such devices are useful to assess the effectiveness of remedial techniques to alleviate indoor radon problems. Additionally, integrated results can also be determined from continuous long-term measurement records. A review of the most commonly utilized 222Rn measurement techniques are reviewed in this chapter. Furthermore, wherever applicable, the sensitivity and quality assurance/quality control (QA/QC) aspects of these techniques are also explored.

When an alpha particle decays in the detector chamber, ionization of the air takes place leading to a decrease in the total charge on the electret. The decrease in the total charge results in the voltage drop (charge, Q = capacitance, C* potential difference, V) over the measurement period and is used to quantify the 222Rn concentration. 3 Determination of 222 Rn Using Beta Counter Radon concentrations can be determined by measuring the beta activity of 214Pb and 214Bi collected on filter papers, assuming secular equilibrium between 222Rn and its progeny in the air.

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