Influence of the accumulation chamber insertion depth to measure surface radon exhalation rates
- 1Integrated Sciences Department, Research Centre of Natural Resources, Health and the Environment (RENSMA), University of Huelva, Huelva, Spain (isidoro.gutierrez@dfa.uhu.es)
- 2Atmospheric Sounding Station – El Arenosillo, Atmospheric Research and Instrumentation Branch, National Institute for Aerospace Technology. INTA, Mazagón-Huelva, Spain
A common method to measure radon exhalation rates relies on the accumulation chamber technique. Usually, this approach only considers one-dimensional gas transport within the soil that neglects lateral diffusion. However, this lateral transport could reduce the reliability of the method. In this work, several cylindrical- shaped accumulation chambers were built with different heights to test if the insertion depth of the chamber into the soil improves the reliability of the method and, in that case, if it could limit the radon lateral diffusion effects. To check this hypothesis in laboratory, two reference exhalation boxes were manufactured using phospho- gypsum from a repository located nearby the city of Huelva, in the southwest of Spain. Laboratory experiments showed that insertion depth had a deep impact in reducing the effective decay constant of the system, extending the interval where the linear fitting can be applied, and consistently obtaining reliable exhalation measurements once a minimum insertion depth is employed. Field experiments carried out in the phosphogypsum repository showed that increasing the insertion depth could reduce the influence of external effects, increasing the re- peatability of the method. These experiments provided a method to obtain consistent radon exhalation mea- surements over the phosphogypsum repository.
How to cite: Gutiérrez Álvarez, I., Guerrero, J. L., Martín, J. E., Adame, J. A., and Bolívar, J. P.: Influence of the accumulation chamber insertion depth to measure surface radon exhalation rates, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-4222, https://doi.org/10.5194/egusphere-egu21-4222, 2021.