Studying natural Radionuclides in water and sediments of Tehran
Category | Environmetal Geology |
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Group | GSI.IR |
Location | The 25 Symposium of Geosciences |
Author | P.Pruzfar-F.Rahmani-A.Yaghub pour-A.Aftabi-R.Ata pour-N.Rastkhah-J.Amidi-P.Behnia-R.Nobari |
Holding Date | 02 July 2007 |
Studying natural Radionuclides in water and sediments of Tehran
1:100000 geologic maps (Tehran, Karaj, and Shahryar 1:50000 sheets)
Abstract:
The natural Radionuclides have Longley existed in the Earth and in environment around us such as Water, Soil, air and body. Now it's very important to study and understand Radionuclides resources. The surveyed region includes Tehran, Karaj, Shahryar 1:50000 sheets (located on geologic map of Tehran 1:100000).
Regarding close relation between water and sediment geochemistry and their direct effect on human and other creatures' health, water and sediment have been simultaneously studied here. samples were analyzed in Atomic Energy organization laboratory for measuring natural Radionuclides 40 K 226Ra 232 Th and The artificial Radio Nuclides 137Cs for sediments and elements such as 226Ra 137Cs 222Rn U total And ( β ، α) for water samples. The results were compared with EQGS Canada (2003), 1053 Iran, and EPA American standards. The results indicates that 232 Th in sediment sampels of karaj and shahryar in comparision with UNSCEAR standard is normal but the average of 40 K and 226Ra are greater than standard . existence of 137Cs in sediments is from antropogenic resources ( nuclear activities). It indicated that average amount of Radionuclides is very close to each other in ground and surfacial water. Comparing the average concentration of this radionuclide with existing standards revealed that all measured samples are for less than risk limit and aren't deemed as a threat.
It should be mentioned that existing research is the first researches with such a vast realm and various survey parameters. Needless to say that accessing more meticulous data and finding geogetic relation between Radionuclides and geological units require complementary studies in smaller scales.