| Abstract: | Soil-gas radon concentrations are controlled seasonally by factors of climate and pedology. In a swelling soil of the semiarid Western United States, soil-gas radon concentrations at 100 cm depth increase in winter and spring due to increased emanation with higher soil moisture and the capping effect of surface water or ice. Radon concentrations in soil drop markedly through the summer and fall. The increased insolation of spring and summer warms and dries the soil, limiting the amount of water that reaches 100 cm. Probable controls on the distribution of uranium within the soil column include its downward leaching, its precipitation or adsorption onto B-horizon clays, concretions, or cement, and the uranium content and mineralogy of the soil‘s granitic and gneissic precursors. -from Authors |
| Genre: | Article |
| ProdID: | 70016293 |
| Citation Author: | Asher-Bolinder, S.; Owen, D. E.; Schumann, R. R. |
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| Citation End Page: | 828 |
| Citation Issue: | 6 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geophysical Research Letters |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Pedologic and climatic controls on Rn-222 concentrations in soil gas, Denver, Colorado; 1990; Article; Journal; Geophysical Research Letters; Asher-Bolinder, S.; Owen, D. E.; Schumann, R. R. |
| Citation Start Page: | 825 |
| Citation Volume: | 17 |
| Citation Year: | 1990 |
| Type: | citation/reference |
| Text: | Pedologic and climatic controls on Rn-222 concentrations in soil gas, Denver, Colorado; 1990; Article; Journal; Geophysical Research Letters; Asher-Bolinder, S.; Owen, D. E.; Schumann, R. R. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Mon, 1 Jan 1990 00:00 -0600 |
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