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2016 | OriginalPaper | Chapter

1. Physical, Chemical and Nuclear Properties of Radon: An Introduction

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Abstract

Radon is the heaviest of all noble gases and has a total of 36 isotopes ranging from 193Rn to 228Rn all of which are radioactive. Over a large portion of the past 115 years since its first discovery in 1900, radon has been widely studied including for its impact on human health. The three naturally-occurring radon isotopes (222Rn, 220Rn and 219Rn) with half-lives varying over 3 orders of magnitude are useful as a tracer in several branches of geosciences. A thorough understanding of its physical, chemical and nuclear properties are required for its effective use as an environmental tracer. For example, the radon partition coefficient between water and air and the octanol-water partition coefficient (Kow) are reported to be 0.2395 and 32.4, respectively. This chapter lays the foundation for the utility of radon as a geochemical tool.

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Footnotes
1
Throughout the book, three terms are synonymously used to represent the concentration of radon in environmental samples, as done in most published literature. Those are: concentration, activity, and specific activity. The units are: for fluids (liquid and gas): Bq L-1/Bq m-3 or pCi L-1/pCi m-3; for solids: Bq g-1/Bq kg-1 or pCi g-1 or pCi kg-1
 
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Metadata
Title
Physical, Chemical and Nuclear Properties of Radon: An Introduction
Author
Mark Baskaran
Copyright Year
2016
DOI
https://doi.org/10.1007/978-3-319-21329-3_1