scholarly journals Distribution of radon activity in the atmosphere above Wzgórza Niemczansko-Strzelinskie (South-WestPoland) and its dependence on uranium and thorium content in the underlying rock and indirect ground basement

2009 ◽  
Vol 48 (1) ◽  
Author(s):  
A. A. Ochmann
Materials ◽  
2020 ◽  
Vol 13 (24) ◽  
pp. 5840
Author(s):  
Enver Faella ◽  
Simona Mancini ◽  
Michele Guida ◽  
Albina Cuomo ◽  
Domenico Guida

Radon is a naturally occurring radioactive gas present in the hydrosphere, lithosphere and atmosphere abundantly. Its ionizing radiation provides the largest human internal exposure by inhalation and ingestion to natural sources, constituting a serious health hazard. The contribution to total exposure is mainly due to inhalation, as ingestion by food or drinking water is typically very small. However, because of public health concerns, the contributions from all these sources are limited by regulations and remedial action should be taken in the event that the defined threshold values are overcome. In this paper, the first campaign of measurements to control the radon activity concentration in drinking water from public water supplies in the province of Salerno, south Italy, is described. The results represent a main reference for the area, as it was never investigated before. The purpose of this survey was to contribute to data compilation concerning the presence of radon-222 in groundwater in the Campania region and to determine the associated risk for different age groups. The maximum radon activity concentrations and the related total annual public effective dose turned out to be lower than the threshold values (100 Bq/l and 0.1 mSv/y, respectively) indicated by international guidelines and the national regulation, showing that the health risks for public consumption can be considered negligible.


2013 ◽  
Vol 8 (03) ◽  
pp. C03011-C03011 ◽  
Author(s):  
F Mamedov ◽  
P Čermák ◽  
J Jakůbek ◽  
K Smolek ◽  
I Štekl ◽  
...  
Keyword(s):  

2014 ◽  
Vol 160 (1-3) ◽  
pp. 222-225 ◽  
Author(s):  
M. M llerova ◽  
K. Holy ◽  
M. Bulko

Science ◽  
1958 ◽  
Vol 128 (3317) ◽  
pp. 204-205 ◽  
Author(s):  
W. M. SACKETT ◽  
H. A. POTRATZ ◽  
E. D. GOLDBERG
Keyword(s):  

Author(s):  
Jörg Dehnert ◽  
Diana Altendorf ◽  
Ralf Trabitzsch ◽  
Hannes Grünewald ◽  
Ralph Geisenhainer ◽  
...  

2012 ◽  
Vol 35 (2) ◽  
pp. 84
Author(s):  
Charles Kansaana ◽  
AndamBentil Aba ◽  
Eric KoteiT Addision ◽  
OscarKwaku Adukpo ◽  
EmmanuelOfori Darko ◽  
...  
Keyword(s):  

1968 ◽  
Vol 76 ◽  
pp. 1-51
Author(s):  
J Hansen

Radioactive veins containing the rare-earth minerals monazite and bastnaesite are found in tension joints in Precambrian sandstone, granite, lavas and dykes on the eastern side of the alkaline Ilímaussaq intrusion in South Greenland. The veins were formed in several phases. First, small cracks were mineralized with hematite, fluorite, quartz and radioactive material. This was followed by emplacement of brown albititic veins in which albite and opaque material predominate, green veins with a high content of ægirine, white albititic veins, carbonate veins and finally quartz veins. All the vein minerals may be coated by a late iron-manganese oxide. Most often the veins are separate, but they may also occur composite. The veins are from a few millimetres to about three metres wide; most commonly they are one to ten centimetres wide. The radioactivity is mostly due to thorium, but a few veins have a uranium content higher than that of thorium. The thorium content ranges from 60 to 4500 ppm, the uranium from 17 to 1500 ppm. The ratio thorium/uranium ranges from 0.1 to 57.2. The radioactivity is predominantly connected with pigmentary material, thorite, thorianite, monazite and bastnäsite. Other minerals identified in the vein are ægirine, acmite, albite, arfvedsonite, apatite, biotite, calcite, chlorite, eudialyte, fluorite, hematite, lithium mica, mesodialyte, microcline, neptunite, pyrite, quartz and sphalerite. The following constants were calculated from X-ray powder diagrams made with a Guinier-Hagg camera.Bastnäsite: a0 = 7.120 ± 7 x 10-3 Å; C0 = 9.77 ± 2 x 10-2 Å; c0/a0 = 1.372; V0 = 428.96 Å3. Monazite: a0 = 6.780 ± 5 x 10-3 Å; b0 = 7.025 ± 4 x 10-3 Å; C


2020 ◽  
Vol 35 (4) ◽  
pp. 339-346
Author(s):  
Mehmet Erdogan ◽  
Murat Abaka ◽  
Kaan Manisa ◽  
Hasan Bircan ◽  
Coskun Kus ◽  
...  

Indoor radon activity concentrations and radon doses on the ground floor and basement floor of 19 schools (kindergardens, primary schools, secondary schools, and high schools) and thermal spas of Ilgin district in Konya, have been measured using the AlphaGUARD PQ 2000PRO radon detector, for three days in the first half of 2016. According to the results, while the indoor radon concentration for only one location, in total, is above the Turkish action level of 400 Bqm?3, the values for 10 locations are above the reference level of 100 Bqm?3, recommended by WHO. The calculated annual effective doses for inhalation of the radon in indoor air were also found to be 0.26 ?Sv for the minimum and 4.36 ?Sv for the maximum. The parametric distribution analysis is also performed with 3-parameter Weibull distribution and some remarks are provided on radon concentration activity.


Science ◽  
1957 ◽  
Vol 126 (3274) ◽  
pp. 612-614
Author(s):  
George L. Bate ◽  
J. R. Huizenga ◽  
Herbert A. Potratz
Keyword(s):  

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