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<ArticleSet>
<Article>
<Journal>
				<PublisherName>Kurdistan University of Medical Sciences</PublisherName>
				<JournalTitle>Journal of Advances in Environmental Health Research</JournalTitle>
				<Issn>2676-3478</Issn>
				<Volume>13</Volume>
				<Issue>4</Issue>
				<PubDate PubStatus="epublish">
					<Year>2025</Year>
					<Month>11</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Indoor Radon in Larijan Buildings Affected by Geological Characteristics</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>228</FirstPage>
			<LastPage>232</LastPage>
			<ELocationID EIdType="pii">237203</ELocationID>
			
<ELocationID EIdType="doi">10.34172/jaehr.1403</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Somayeh</FirstName>
					<LastName>Dadashpoor</LastName>
<Affiliation>Department of Natural Resources and Environment, SR.C., Islamic Azad University, Tehran, Iran</Affiliation>
<Identifier Source="ORCID">0009-0000-3213-321X</Identifier>

</Author>
<Author>
					<FirstName>Parvin</FirstName>
					<LastName>Nassiri</LastName>
<Affiliation>School of Public Health, Tehran University of Medical Sciences, Tehran, Iran</Affiliation>
<Identifier Source="ORCID">0000-0002-3159-5356</Identifier>

</Author>
<Author>
					<FirstName>Alireza</FirstName>
					<LastName>Mirzahosseini</LastName>
<Affiliation>Department of Natural Resources and Environment, SR.C., Islamic Azad University, Tehran, Iran</Affiliation>
<Identifier Source="ORCID">0000-0002-7140-8308</Identifier>

</Author>
<Author>
					<FirstName>Nabiollah</FirstName>
					<LastName>Mansouri</LastName>
<Affiliation>Department of Natural Resources and Environment, SR.C., Islamic Azad University, Tehran, Iran</Affiliation>
<Identifier Source="ORCID">0000-0002-4228-6444</Identifier>

</Author>
<Author>
					<FirstName>Zahra</FirstName>
					<LastName>Azizi</LastName>
<Affiliation>Department of Geoinformation and Geomatics Engineering, Faculty of Civil, Water and Environmental Engineering, Shahid Beheshti University, Tehran, Iran</Affiliation>
<Identifier Source="ORCID">0000-0001-8572-7134</Identifier>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2024</Year>
					<Month>11</Month>
					<Day>18</Day>
				</PubDate>
			</History>
		<Abstract>&lt;strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;;&quot;&gt;Background:&lt;/span&gt;&lt;/strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;;&quot;&gt; 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. &lt;/span&gt;&lt;br&gt;&lt;strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;; mso-font-width: 99%;&quot;&gt;Methods:&lt;/span&gt;&lt;/strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;; mso-font-width: 99%;&quot;&gt; 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.&lt;/span&gt;&lt;br&gt;&lt;strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;;&quot;&gt;Results:&lt;/span&gt;&lt;/strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;;&quot;&gt; The average radon concentrations in bedrooms and living rooms were 114.40 Bq/m&lt;sup&gt;3&lt;/sup&gt; and 128.35 Bq/m&lt;sup&gt;3&lt;/sup&gt;, 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/m&lt;sup&gt;3&lt;/sup&gt;, compared with 130.89 Bq/m³ in summer. These findings indicate that both climatic and geological conditions significantly influence indoor radon levels. &lt;/span&gt;&lt;br&gt;&lt;strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;;&quot;&gt;Conclusion:&lt;/span&gt;&lt;/strong&gt;&lt;span style=&quot;font-family: &#039;ltr-font&#039;,serif; mso-bidi-font-family: &#039;Optima LT Std&#039;;&quot;&gt; Since radon concentrations in most buildings exceeded the World Health Organization (WHO) guideline of 100 Bq/m&lt;sup&gt;3&lt;/sup&gt;, implementing exposure control programs in residential buildings is essential. &lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Indoor air pollution</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">radon</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Hot Spring</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jaehr.muk.ac.ir/article_237203_1f543dd286d66fb0b3e0761227be90ca.pdf</ArchiveCopySource>
</Article>
</ArticleSet>
