scholarly journals Radon concentration assessment in water sources of public drinking of Covilhã's county, Portugal

2017 ◽  
Vol 10 (2) ◽  
pp. 135-139 ◽  
Author(s):  
M. Inácio ◽  
S. Soares ◽  
P. Almeida
2012 ◽  
Vol 138 (1) ◽  
pp. 48-57 ◽  
Author(s):  
Craig Patterson ◽  
Anita Anderson ◽  
Rajib Sinha ◽  
Nur Muhammad ◽  
David Pearson

2019 ◽  
Vol 38 (4) ◽  
pp. 957
Author(s):  
I.K. Adegun ◽  
B.E. Anyaegbuna ◽  
O.A. Olayemi ◽  
T.S. Jolayemi ◽  
M.O. Ibiwoye

2012 ◽  
Vol 27 (4) ◽  
pp. 399-403 ◽  
Author(s):  
Mehrdad Amirzadi ◽  
Pooya Hosseini ◽  
Mehran Taheri ◽  
Asad Babakhani

Tonekabon is a big city in the vicinity of the high level natural radiation area of Ramsar, Iran. Natural exposure due to gamma and radon concentration in 100 dwellings in the city has been measured using a thermoluminescent dosimeter and a radon diffusion chamber, respectively, over four seasons. Using active and passive methods (i. e. ZnS scintillation detectors and homemade radon diffusion chambers), the concentration of dissolved radon in water sources has been measured in both cities and frequency distributions of doses studied for radon measurements. Results show a daily average gamma dose of 4.2 ? 0.8 ?Sv and an average radon concentration in air of 232.5 ? 187 Bq/m3 in dwellings. Frequency distributions show that 85% of the dwellings have an average radon concentration of 100 to 300 Bq/m3 per year and that 80% have a maximum seasonal radon concentration of up to 400 Bq/m3. The maximum concentrations of dissolved radon in water in Ramsar and Tonekabon have been measured as 198 ? 30 and 109 ? 16 BqL-1, respectively.


2020 ◽  
Vol 326 (2) ◽  
pp. 1437-1446
Author(s):  
Mostafa Shamsaddini ◽  
Ali Negarestani ◽  
Mohammad Malakootian ◽  
Neda Javid

2016 ◽  
Vol 27 (5) ◽  
pp. 682-689 ◽  
Author(s):  
F. Khan ◽  
Z. Wazir ◽  
N. Ali ◽  
S. A. Khattak

In-situ measurement of radon concentration was carried out in three types of drinking water sources (spring, surface and bore/well). Water samples from all three sources were collected from the city of Abbottabad and its surroundings. Radon concentrations were measured through active technique, using the AB-5 series of portable radiation monitor (Pylon). The mean concentrations (ranges) of radon in the phosphate region were 13.4 ± 2.0 (9.1–23.6), 11.2 ± 1.5 (6.2–20.1) and 7.1 ± 0.9 (4.3–14) kBq m−3 in well, spring and surface waters, respectively. Similarly, the mean concentrations (ranges) of radon outside the phosphate region were 7.2 ± 1.0 (3.4–11.5), 5.4 ± 0.7 (2.5–8.9) and 3.1 ± 0.4 (1.7–5.8) kBq m−3 in well, spring and surface waters, respectively. The arithmetic mean values of radon concentration in drinking waters in the phosphate and non-phosphate parts or rocks were 10.76 ± 1.5 and 5.10 ± 0.70 kBq m−3, respectively. Respective doses of radon taken in by the people via water ingestion and inhalation were calculated as 0.029 ± 0.004 and 0.014 ± 0.002 mSv. The mean values of radon concentrations in drinking water samples collected from Abbottabad phosphate and non-phosphate rocks were below the US EPA Maximum Contamination Level (MCL) of 11.1 kBq m−3. The annual mean effective doses of all samples are lower than the reference level of 0.1 mSv a−1 for drinking water as recommended by WHO. Thus, the drinking water of Abbottabad and its surroundings is generally below the recommended levels as regards to radon-related health hazards.


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