Indoor Radon in Larijan Buildings Affected by Geological Characteristics
سال انتشار: 1404
نوع سند: مقاله ژورنالی
زبان: انگلیسی
مشاهده: 65
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شناسه ملی سند علمی:
JR_JAEHR-13-4_002
تاریخ نمایه سازی: 5 بهمن 1404
چکیده مقاله:
Background: The decay of uranium and thorium is the primary source of radon emissions, a radioactive gas. The transfer and accumulation of this gas indoors pose serious health risks. Methods: This study investigated indoor radon concentrations in buildings located in areas with different geological characteristics. Thirty-six buildings were examined across three locations in Larijan, Iran, with samples collected from living rooms and bedrooms over a three-month period.Results: The average radon concentrations in bedrooms and living rooms were ۱۱۴.۴۰ Bq/m۳ and ۱۲۸.۳۵ Bq/m۳, respectively. Indoor radon levels in buildings near hot springs were ۲۴.۶۶% higher than those in buildings close to, and ۴۵.۳۱% higher than those in buildings far from, hot springs. Seasonal variation was also observed: the average concentration in winter was ۱۱۲.۰۵ Bq/m۳, compared with ۱۳۰.۸۹ Bq/m³ in summer. These findings indicate that both climatic and geological conditions significantly influence indoor radon levels. Conclusion: Since radon concentrations in most buildings exceeded the World Health Organization (WHO) guideline of ۱۰۰ Bq/m۳, implementing exposure control programs in residential buildings is essential.
کلیدواژه ها:
نویسندگان
Somayeh Dadashpoor
Department of Natural Resources and Environment, SR.C., Islamic Azad University, Tehran, Iran
Parvin Nassiri
School of Public Health, Tehran University of Medical Sciences, Tehran, Iran
Alireza Mirzahosseini
Department of Natural Resources and Environment, SR.C., Islamic Azad University, Tehran, Iran
Nabiollah Mansouri
Department of Natural Resources and Environment, SR.C., Islamic Azad University, Tehran, Iran
Zahra Azizi
Department of Geoinformation and Geomatics Engineering, Faculty of Civil, Water and Environmental Engineering, Shahid Beheshti University, Tehran, Iran
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