Relationship between the effective diffusion coefficient of soil radon and groundwater recharge in semi-arid areas

• Published in: Environmental earth sciences Vol. 59; no. 2; pp. 261 - 268
• Main Authors: Ershaidat, N. M., Abu-Jaber, N. S., Al-Bataina, B. A., Shobaki, J. M., Jaradat, A. S.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer-Verlag 01.11.2009; Springer; Springer Nature B.V
• Subjects: Arid zones; Biogeosciences; Diffusion; Diffusion coefficient; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental Science and Engineering; Exact sciences and technology; Geochemistry; Geology; Groundwater; Groundwater recharge; Hydrogeology; Hydrology. Hydrogeology; Hydrology/Water Resources; Original Article; Pollution, environment geology; Porosity; Radon; Soil types; Soils; Surficial geology; Terrestrial Pollution; Middle East; Jordan; Asia; Jordan (country); Semi-arid; Water recharge; Soil gas; Jordan; Radon; Hosha; radon; diffusion; rainfall; soil moisture; porosity; sampling; ground water; gaseous phase; ground-water recharge; concentration; slopes; pollution; depth; correlation; Hosa; hills; soils; semi-arid environment; seasonal variations
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-009-0023-7

Herein, the relationship between soil radon behavior and groundwater recharge in the town of Hosha, a semi-arid area of Jordan is explored. The annual rainfall average in this area is between 60–100 mm year −1 . Soil radon concentration levels, using CR-39 detectors, have been measured at several depths. Nine sampling sites on a hill slope, in the summer and winter 2006 were chosen. Other soil parameters such as moisture, soil type and porosity were also measured. Correlation between the latter and the calculated effective diffusion coefficients, based on a linear approximation, was done in order to explore water movement. A weak correlation between the soil radon concentration and water recharge in this particular semi-arid area is observed. The results show that water recharge takes place vertically, i.e., water moves downward and in one of the nine sampling sites this movement seems to be more rapid compared to the other sites.