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Paper ID:IJSREM65175

GEOCHEMICAL EVOLUTION OF RADON GAS IN URBAN ENVIRONMENT

Stream/Area:

-

Subject:

-

Paper ID:

IJSREM65175

Volume:

10 |

6 |

Jun 2026

Pages:

1-12

Publication Frequency:

Monthly (12 issues per year)

DOI
Digital Object Identifier
10.55041/IJSREM65175

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.

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Authors

BP

Balasaraswathi P

Geography / Geospatial Science

Institute for Ocean Management, Anna University

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MBK

Manikanda Bharath K

Geography / Geospatial Science

Institute for Ocean Management, Anna University

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N

Naveenkumar

Geography / Geospatial Science

Institute for Ocean Management, Anna University

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Abstract

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

lung diseases airborne particles Technologically Enhanced Natural Radiation (TENR

Cite This Article

Balasaraswathi P, Manikanda Bharath K, Naveenkumar, "GEOCHEMICAL EVOLUTION OF RADON GAS IN URBAN ENVIRONMENT," International Journal of Scientific Research in Engineering and Management, vol. 10, no. 6, pp. 1-12, Jun 2026. https://doi.org/10.55041/IJSREM65175

Full Article/Conclusion

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.

References

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Publication Date

6/18/2026

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