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indoor radon in larijan buildings affected by geological characteristics
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نویسنده
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dadashpoor somayeh ,nassiri parvin ,mirzahosseini alireza ,mansouri nabiollah ,azizi zahra
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منبع
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journal of advances in environmental health research - 2025 - دوره : 13 - شماره : 4 - صفحه:228 -232
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چکیده
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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 114.40 bq/m3 and 128.35 bq/m3, respectively. indoor radon levels in buildings near hot springs were 24.66% higher than those in buildings close to, and 45.31% higher than those in buildings far from, hot springs. seasonal variation was also observed: the average concentration in winter was 112.05 bq/m3, compared with 130.89 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 100 bq/m3, implementing exposure control programs in residential buildings is essential.
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کلیدواژه
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indoor air pollution ,radon ,hot spring
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آدرس
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islamic azad university, tehran branch, department of natural resources and environment, iran, tehran university of medical sciences, school of public health, iran, islamic azad university, tehran branch, department of natural resources and environment, iran, islamic azad university, tehran branch, department of natural resources and environment, iran, shahid beheshti university, faculty of civil, department of geoinformation and geomatics engineering, iran
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پست الکترونیکی
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zsazizi@yahoo.com
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Authors
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