Abstract
The observed disequilibrium between 222Rn and 226Ra in aqueous system is one of the most widely used and successful applications of U-Th-series radionuclides. The observed radon concentration gradients at key interfaces such as sediment-water and air-water have been widely utilized for the past five decades to investigate several geochemical and geophysical processes in marine and lacustrine environments. In this chapter, the most important applications of radon as a tracer in aqueous system are reviewed and presented. Those include: i) determination of gas exchange rate coefficient at air-sea interface; ii) estimation of isopycnal and diapcynal mixing coefficients in the upper ocean as well as the bottom ~200 m of the water column; and iii) quantification of amount of groundwater discharge in rivers, coastal ocean, and lake water using a mass balance approach of 222Rn. From the measurements of nutrients and other key trace metals in the advecting fluids, the fluxes of these species to aqueous systems can also be quantified. Radon-derived exchange rate coefficient can also serve as a proxy to determine exchange coefficient for other gases including O2, CO2, N2, etc. Vertical transport rates of 222Rn can be utilized to deduce the transport rates of other tracers as well as estimation of buoyance fluxes or heat flux rates. The excess inventory of 222Rn in the water column provides direct information on the rates of sedimentation, including possible information on the boundary scavenging.
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Acknowledgments
This chapter greatly benefited from an in-depth review by Doug Hammond. Thanks to Katie Krupp for a final editorial review of this chapter. The work synthesized in this chapter was partially supported by NSF Grants (OCE-1237059 and PLR-1434578).
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Baskaran, M. (2016). Radon: A Geochemical and Geophysical Tracer in Marine System. In: Radon: A Tracer for Geological, Geophysical and Geochemical Studies. Springer Geochemistry. Springer, Cham. https://doi.org/10.1007/978-3-319-21329-3_6
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