Relationship between the effective diffusion coefficient of soil radon and groundwater recharge in semi-arid areas |
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Authors: | N M Ershaidat N S Abu-Jaber B A Al-Bataina J M Shobaki A S Jaradat |
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Institution: | (1) Physics Department, Yarmouk University, Irbid, 21163, Jordan;(2) Department of Earth and Environmental Science, Yarmouk University, Irbid, 21163, Jordan;(3) Dean of Graduate Studies, German Jordanian University, P.O. Box 35247, Amman, 11180, Jordan;(4) Princess Sumaya University for Technology, Amman, Jordan |
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Abstract: | 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. |
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