Indoor and outdoor Radon concentration measurements in Sivas, Turkey, in comparison with geological setting.
Identifieur interne : 000713 ( Ncbi/Curation ); précédent : 000712; suivant : 000714Indoor and outdoor Radon concentration measurements in Sivas, Turkey, in comparison with geological setting.
Auteurs : Metin Mihci [Turquie] ; Aydin Buyuksarac ; Attila Aydemir ; Nilgun CelebiSource :
- Journal of environmental radioactivity ; 2010.
Descripteurs français
- Wicri :
- geographic : Turquie.
English descriptors
- KwdEn :
- MESH :
- chemical , analysis : Air Pollutants, Radioactive, Radon.
- geographic : Turkey.
- analysis : Air Pollution, Indoor.
- Geography, Radiation Monitoring, Seasons, Time Factors.
Abstract
Indoor and soil gas Radon ((222)Rn) concentration measurements were accomplished in two stages in Sivas, a central eastern city in Turkey. In the first stage, CR-39 passive nuclear track detectors supplied by the Turkish Atomic Energy Authority (TAEA) were placed in the selected houses throughout Sivas centrum in two seasons; summer and winter. Before the setup of detectors, a detailed questionnaire form was distributed to the inhabitants of selected houses to investigate construction parameters and properties of the houses, and living conditions of inhabitants. Detectors were collected back two months later and analysed at TAEA laboratories to obtain indoor (222)Rn gas concentration values. In the second stage, soil gas (222)Rn measurements were performed using an alphameter near the selected houses for the indoor measurements. Although (222)Rn concentrations in Sivas were quite low in relation with the allowable limits, they are higher than the average of Turkey. Indoor and soil gas (222)Rn concentration distribution maps were prepared seperately and these maps were applied onto the surface geological map. In this way, both surveys were correlated with the each other and they were interpreted in comparison with the answers of questionnaire and the geological setting of the Sivas centrum and the vicinity.
DOI: 10.1016/j.jenvrad.2010.06.013
PubMed: 20667631
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pubmed:20667631Le document en format XML
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<affiliation wicri:level="1"><nlm:affiliation>Iller Bankasi, Etud Plan ve Yol Dairesi, Opera, 06053 Ankara, Turkey.</nlm:affiliation>
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<author><name sortKey="Buyuksarac, Aydin" sort="Buyuksarac, Aydin" uniqKey="Buyuksarac A" first="Aydin" last="Buyuksarac">Aydin Buyuksarac</name>
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<author><name sortKey="Aydemir, Attila" sort="Aydemir, Attila" uniqKey="Aydemir A" first="Attila" last="Aydemir">Attila Aydemir</name>
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<author><name sortKey="Celebi, Nilgun" sort="Celebi, Nilgun" uniqKey="Celebi N" first="Nilgun" last="Celebi">Nilgun Celebi</name>
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<author><name sortKey="Aydemir, Attila" sort="Aydemir, Attila" uniqKey="Aydemir A" first="Attila" last="Aydemir">Attila Aydemir</name>
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<series><title level="j">Journal of environmental radioactivity</title>
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<term>Radon (analysis)</term>
<term>Seasons</term>
<term>Time Factors</term>
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<term>Radiation Monitoring</term>
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<front><div type="abstract" xml:lang="en">Indoor and soil gas Radon ((222)Rn) concentration measurements were accomplished in two stages in Sivas, a central eastern city in Turkey. In the first stage, CR-39 passive nuclear track detectors supplied by the Turkish Atomic Energy Authority (TAEA) were placed in the selected houses throughout Sivas centrum in two seasons; summer and winter. Before the setup of detectors, a detailed questionnaire form was distributed to the inhabitants of selected houses to investigate construction parameters and properties of the houses, and living conditions of inhabitants. Detectors were collected back two months later and analysed at TAEA laboratories to obtain indoor (222)Rn gas concentration values. In the second stage, soil gas (222)Rn measurements were performed using an alphameter near the selected houses for the indoor measurements. Although (222)Rn concentrations in Sivas were quite low in relation with the allowable limits, they are higher than the average of Turkey. Indoor and soil gas (222)Rn concentration distribution maps were prepared seperately and these maps were applied onto the surface geological map. In this way, both surveys were correlated with the each other and they were interpreted in comparison with the answers of questionnaire and the geological setting of the Sivas centrum and the vicinity.</div>
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