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Titlebook: Radon: A Tracer for Geological, Geophysical and Geochemical Studies; Mark Baskaran Book 2016 Springer International Publishing Switzerland

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Mark Baskaran the past decade there has been a proliferation of programs, both hospital- and clinic-based, that provide rehabilitation, treatment, and treatment planning services. This encyclopedia will serve as a unified, comprehensive reference for professionals involved in the diagnosis, evaluation, and rehab
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Mechanisms of Radon Emanation and Long-Term Radon Flux Studies,erature, moisture, mineralogy and grain size affect the release rates of radon and its subsequent transport is presented. Large-scale well-coordinated efforts around the globe, both on continental and national scale, on radon flux measurements have been conducted and results from those efforts are s
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Applications of Radon Progeny in Atmospheric Studies, that of the ocean. This has led to distinctly higher .Pb activities in continental air masses compared to oceanic air masses. The highly varying activities of .Pb in air as well the depositional fluxes have yielded insights on the sources and transit times of aerosols. In an ideal enclosed air mass
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Radon: A Geochemical and Geophysical Tracer in Marine System,f 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 O., CO., N., etc. Vertical transport ra
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Radon in Groundwater System, the quantification of infiltration of meteoric water. Since almost all of the radon in groundwater is derived by recoil, from a comparison of the measured activities of .Rn and radium isotopes (.Ra), the rate constants of adsorption/desorption, and retardation factors have been determined for a few
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Radon: A Tracer for Geochemical Exploration,tion are summarized. One of the most commonly used techniques in oil industry is the gamma radiation intensity measurements (which is a measure of the concentrations of potassium, uranium and thorium and their progeny) to obtain information on lithology, variations in organic carbon, permeability, a
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