Abstract

Wadi El Reddah, Egypt, is mostly enclosed by scattered exposure to the chronological sequence of a metavolcanic and metagabbro-diorite complex. There are radiological impacts due to internal and external exposure to the high natural background radiation caused by 226Ra, 232Th, and 40K in the Wadi El-Reddah stream sediments. 72 samples were collected and the activity concentration was measured using a NaI(Tl) gamma-spectroscopy system. The average activity concentration of 226Ra, 232Th and 40K was 215 ± 118 Bq kg−1, 131 ± 90 Bq kg−1 and 822 ± 125 Bq kg−1, respectively. Most of the studied samples had a higher activity concentration than the world average.

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