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.

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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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