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Stream/Area:
-
Subject:
-
Paper ID:
IJSREM65175
Volume:
10 |
6 |
Jun 2026
Pages:
1-12
Publication Frequency:
Monthly (12 issues per year)
License:International Journal of Scientific Research in Engineering and Management follows the Creative Commons Attribution 4.0 (CC BY 4.0) License, allowing free use and distribution with proper attribution.
Geography / Geospatial Science
Institute for Ocean Management, Anna University
Geography / Geospatial Science
Institute for Ocean Management, Anna University
Geography / Geospatial Science
Institute for Ocean Management, Anna University
Natural background radiation is the major source of radiation exposure to humans, with radon (^222Rn) and thoron (^220Rn) contributing significantly to inhalation doses. These radioactive gases originate from the decay of uranium and thorium present in soils, rocks, and building materials. Radon and thoron decay products attach to airborne particles and, when inhaled, can deposit in the respiratory tract, increasing the risk of lung diseases. While radon has been extensively studied, thoron is often neglected due to its short half-life. However, recent studies indicate that thoron may contribute substantially to radiation exposure in certain environments. This study evaluates the concentrations of radon, thoron, and their progeny in various indoor environments and examines the influence of floor and wall covering materials. Special attention is given to coastal regions such as Chennai, where geological conditions may affect radionuclide levels. The findings provide valuable baseline data for environmental radiation monitoring, radiological impact assessment, and public health studies related to low-dose radiation exposure.
KEYWORDS
The in-situ gamma radiation levels measured in the coastal sediments of Chennai ranged from 5.6 to 7.5 µR h⁻¹, which are considerably lower than the background radiation levels reported from several other coastal regions of Tamil Nadu. This observation suggests that the concentration of naturally occurring radioactive minerals in the Chennai coastal sediments is relatively low compared to other parts of the state's coastline. Airborne radon and thoron concentrations were evaluated to assess the emanation of radioactive gases from geological materials and indoor environments. Radon concentrations ranged from 0.36 to 8.94 Bq m⁻³, while thoron concentrations varied between 0.12 and 2.90 Bq m⁻³. Higher concentrations were observed in closed and air-conditioned rooms compared to naturally ventilated spaces, indicating the accumulation of these gases under restricted ventilation conditions. Nevertheless, all measured values remained within the limits recommended by the World Health Organization (WHO). Groundwater radon concentrations were found to be strongly influenced by the geological characteristics of the host rocks. Bore wells located in charnockite formations exhibited relatively higher radon concentrations, reflecting the presence of radioactive minerals within the bedrock. In contrast, coastal aquifers showed comparatively lower radon levels. Open wells generally recorded lower radon concentrations than bore wells, as dissolved radon can readily escape into the atmosphere from open water surfaces, whereas it tends to accumulate in confined groundwater systems. The measured radon concentration in groundwater along the Chennai coastal region ranged from 2.1 to 28.4 Bq L⁻¹. Inland groundwater sources generally exhibited higher radon concentrations than coastal aquifers, with values ranging from 2.1 to 13.86 Bq L⁻¹. These variations highlight the significant role of lithology, groundwater circulation, and well type in controlling radon distribution within the study area. Overall, the results indicate that the levels of gamma radiation, airborne radon, thoron, and groundwater radon in the Chennai coastal environment remain within acceptable safety limits and do not pose significant radiological risks to the local population.
Anbazhagan, P & Sitharam, T G 2008 ‘Seismic microzonation of Bangalore, India’, Journal of Earth System Science, Vol.117, S2, pp. 833–852. Balakrishna, M T, Sathish, L A, Sundareshan, S & Ramachandran, T V 2010 ‘Study of indoor radon and thoron levels in Vijayanagar, Bangalore, India’, Environmental Science, Vol. 5(1), pp. 73-79. Doi, M & Kobayashi, S 1994 ‘The passive radon-thoron discriminative dosimeter forpractical use’, Hoken Butsuri, Vol. 29, pp. 155 - 166. Doi, M, Fugimoto, K, Koyabshi, S & Yenhara, H 1994 ‘Spatial distribution of thoron and radon concentrations in the indoor air of a traditional Japanese wooden house’, Health Physics, Vol. 66, pp. 43 - 49. Hunse, T M, Md Najeeb, K, Rajarajan, K & Muthukkannan, M 2010 ‘Presence of Radon in Groundwater in Parts of Bangalore’, Journal of Geological Society of India, Vol.75, pp. 704-708. Erling Stranden (1980) A two-count filter method formeasurements of 220Rn and 222Rndaughters in air.Health Physics, 38: 73-76. Jyoti, S, Mahur, A K, Rupesh, K, Rati, V, Sonkawade, R G, Swarup, R, Singh, H & Rajendra Prasad 2012 ‘Comparative study of indoor radon, thoron with radon exhalation rate in soil samples in some historical places at Jaipur, Rajasthan, India’, Advances in Applied Science Research, Vol. 3 (2), pp. 1085-1091 Levin, I, Born, M, Cuntz, M, Langendorfer, M, Mantsch, S, Naegler, T, Schmidt, M, Varlagin, A, Verclas, S & Wagenbach, D 2002 ‘ Observations of atmospheric variability and soil exhalation rate of radon-222 at a Russian forest site’, Tellus, Vol. 54B, pp. 462–475Lubin, J H, John, D, Boice & Jr Jonathan Megumi, K & Mamuro, T 1974 ‘Emanation and exhalation of radon and thoron gas from soil particles’, Journal of Geophysics Research, Vol. 79, pp. 3357-3360. Mishra, U C & Sadasivan, S 1971 ‘ Natural radioactivity levels in Indian soil, Journal of Scientific and Industry Research, Vol. 30(2),pp. 59-62.
Publication Date
6/18/2026
Peer Review Type
Double-Blind Peer Review
Review Rounds: 2
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