The effect of CO2 on the measurement of 220Rn and 222Rn with instruments utilising electrostatic precipitation
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geophysics
Link
http://link.springer.com/content/pdf/10.2478/s11600-013-0107-3.pdf
Reference13 articles.
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2. D’Amore, F., and J.C. Sabroux (1976), Signification de la présence de radon 222dans le fluides géothermiques, B. Volcanol. 40,2, 106–115, DOI: 10.1007/BF02599855 (in French).
3. Giammanco, S., K.W.W. Sims, and M. Neri (2007), Measurements of 220Rn and 222Rn and CO2 emissions in soil and fumarole gases on Mt. Etna volcano (Italy): Implications for gas transport and shallow ground fracture, Geochem. Geophys. Geosys. 8,10, Q10001, DOI: 10.1029/2007GC001644.
4. Giammanco, S., G. Immè, G. Mangano, D. Morelli, and M. Neri (2009), Comparison between different methodologies for detecting radon in soil along an active fault: The case of the Pernicana fault system, Mt. Etna (Italy), Appl. Radiat. Isotopes 67,1, 178–185, DOI: 10.1016/j.apradiso.2008.09.007.
5. Huxol, S., M.S. Brenwald, E. Hoehn, and R. Kipfer (2012), On the fate of 220Rn in soil material in dependence of water content: Implications from field and laboratory experiments, Chem. Geol. 298–299, 116–122, DOI: 10.1016/j.chemgeo.2012.01.002.
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