| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1881697 | Radiation Measurements | 2010 | 4 Pages |
222Rn concentrations were measured in the bubble gases, spring waters, soil gases and in ambient air around the thermal springs at Bakreswar in West Bengal, India. This group of springs lies within a geothermal zone having exceptionally high heat flow about 230 mW/m2, resembling young oceanic ridges. The spring gas has a high radon activity (∼885 kBq/m3) and is rich in helium (∼1.4 vol. %) with appreciably large flow rate. The measured radon exhalation rates in the soils of the spring area show extensive variations from 831 to 4550/mBqm2 h while 222Rn concentrations in the different spring waters vary from 3.18 to 46.9 kBq/m3. Surface air at a radius of 40 m around the springs, within which is situated the Bakreswar temple complex and a group of dwellings, has radon concentration between 450 and 500 Bq/m3. In the present paper we assess the radon activity background in and around the spring area due to the different contributing sources and its possible effect on visiting pilgrims and the people who reside close to the springs.
