Araştırma Makalesi
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Yıl 2022, Cilt: 9 Sayı: 4, 194 - 206, 25.12.2022

Mutlu Zeybek Alican Kop

https://doi.org/10.30897/ijegeo.1122026

Öz

Destekleyen Kurum

TÜBİTAK

Teşekkür

Prof. Dr. Semih GÜRSU'ya teşekkür ederim.

Kaynakça

  • Al-Tamimi, M.H., Abumurad, K.M. (2001). Radon anomalies along faults in North of Jordan. Radiation Measurements 34, 397–400.
  • Askari, M., Hassanvand, M.S., Naddafi, K., Zarei, A., Yousefi, M., Alimohammadi, M. (2019). Assessment of indoor radon concentration in residential homes and public places in south of Tehran, Iran. Environmental Earth Sciences, 78(10), 1-10.
  • Bossew, P., Petermann, E. (2022). Radon hazard vs. radon risk – consequences for radon abatement policy, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-3145, https://doi.org/10.5194/egusphere-egu22-3145.
  • Bossew, P., Zunic, Z.S., Stojanovska, Z., Tollefsen, T., Carpentieri, C., Veselinovic, N., Komatina, S., Vaupotic, J., Simovic, R.D., Antignani, S., Bochicchio, F. (2014). Geographical distribution of the annual mean radon concentrations in primary schools of Southern Serbia - application of geostatistical methods. Journal of Environmental Radioactivity 127, 141-148.
  • Burghele, B., Ţenter, A., Cucoş, A., Dicu, T., Moldovan, M., Papp, B., Szacsvai, K., Neda, T., Suciu, L., Lupulescu, A., Maloş, C., Florică, Ş., Baciu, C., Sainz, C. (2019). The FIRST large-scale mapping of radon concentration in soil gas and water in Romania. Science of the Total Environment 669, 887–892.
  • Gürer, Ö.F., Yılmaz, Y. (2002). Geology of the Ören and surrounding areas, SW Anatolia. Turkish Journal of Earth Sciences, 11(1), 1-13.
  • Gürer, Ö.F., Sanğu, E., Özburan, M., Gürbüz, A., SaricaFiloreau, N. (2013). Complex basin evolution in the Gökova Gulf region: implications on the Late Cenozoic tectonics of southwest Turkey. International Journal of Earth Sciences, 102, 2199- 2221.
  • Ioannides, K., Papachristodoulou, C., Stamoulis, K., Karamanis, D., Pavlides, S., Chatzipetros, A., Karakala, E. (2003). Soil gas radon: a tool for exploring active fault zones. Applied Radiation and Isotopes 59, 205–213.
  • Kemski, J., Klingel, R., Siehl, A., Valdivia-Manchego, M. (2009). From radon hazard to risk predictionbased on geological maps, soil gas and indoor measurements in Germany. Environ Geol (2009) 56:1269–1279 doi.10.1007/s00254-008-1226-z.
  • Kuluöztürk, M.F., Büyüksaraç, A., Özbey, F., Yalçin, S., Doğru, M. (2019). Determination of indoor radon gas levels in some buildings constructed with Ahlat stone in Ahlat/Bitlis. International Journal of Environmental Science and Technology, 16(9), 5033- 5038.
  • Madureira, J., Paciencia, I., Rufo, J., Moreira, A., Fernandes, E.O., Pereira, A. (2016). Radon in indoor air of primary schools: determinant factors, their variability and effective dose. Environ Geochem Health, 38:523–533 doi.10.1007/s10653-015-9737-5.
  • Moreno, V., Baixeras, C., Font, L., Bach, J. (2008). Indoor radon levels and their dynamics in relation with the geological characteristics of La Garrotxa, Spain. Radiation Measurements 43, 1532–1540.
  • MTA, (2002). 1:500.000 scale Geological Inventory map Series of Turkey, DENIZLI, Maden Tetkik Arama Genel Mudurlugu, Ankara, Turkey.
  • MTA, (2011a). 1:250.000 scale Active Fault Map Series of Turkey, AYDIN (NJ35-11) quadrangle, serial no:7, Maden Tetkik Arama Genel Mudurlugu, Ankara, Turkey
  • MTA, (2011b). 1:250.000 scale Active Fault Map Series of Turkey, MARMARIS (NJ35-15) quadrangle, serial no:8, Maden Tetkik Arama Genel Mudurlugu, Ankara, Turkey
  • Neri, M., Giammanco, S., Leonardi, A. (2019). Preliminary Indoor Radon Measurements Near Faults Crossing Urban Areas of Mt. Etna Volcano (Italy). Front. Public Health 7:105. doi: 10.3389/fpubh.2019.00105.
  • Park, T.H., Kang, D.R., Park, S.H., Yoon, D.K., Lee, C.M. (2018). Indoor radon concentration in Korea residential environments. Environmental Science and Pollution Research 25:12678–12685, doi.org/ 10.1007/s11356-018-1531-3.
  • Pişkin, Ö., Bertrand, J. (1980). Les minéralisations de plomb, zinc et cuivre de Kadikalesi (Presqu'île de Bodrum - Turquie). In: Schweizerische mineralogische und petrographische Mitteilungen, 60(1), 45-68. doi: 10.5169/seals-46657.

Geological and Geostatistical Modeling of Geogenic Radon Potential of Minarets in Muğla Province (SW Turkey)

Yıl 2022, Cilt: 9 Sayı: 4, 194 - 206, 25.12.2022

Mutlu Zeybek Alican Kop

https://doi.org/10.30897/ijegeo.1122026

Öz

Radon (222Rn), derived from the Uranium (238U) series and emitted from Geological Formation (soil, rock) (Qg), Fault (Qf) and Construction Material (Qm), which cannot be detected by the five senses, is an inert radioactive gas. Radon negatively affects people's health (such as lung cancer) as a result of excessive (>200 Bq/m3) accumulation in buildings. The aim of this study is to measure the radon emission concentrations of the components (Qg, Qf, Qm) that make up the Total Radon Gas Concentration (Qt) in the building (for the purpose of this study, mosque minarets) close to the fault or the possible fault in Muğla province (SW Turkey) and order their sizes. The Indoor Radon Concentration (IRC) of 841 minarets in Muğla province was measured with a portable RadonEye device (made in South Korea). At least 5 Soil Radon Concentration (SRC) measurements were made perpendicular to the fault lines near 14 minarets with a portable Markus 10 device (made in Sweden). About 10% of the 841 minarets were found to be above the European Indoor Radon Reference Value (EIRRV) (200 Bq/m3). When evaluated according to the 13 districts, it is seen that the district with the highest IRC in the 841 minarets is Marmaris (Çetibeli town, 2809 Bq/m3), and the district with the lowest is Ula (Armutçuk town, 217 Bq/m3). The highest IRC was measured inside a minaret made of volcanic rocks in the Marmaris district (Çetibeli town, 2809 Bq/m3). The lowest SRC was obtained in Datça district (Kızlan town, 5830 Bq/m3) where serpentinites outcropped, and the highest SRC was found in Bodrum district (Gürece town, 120000 Bq/m3) where volcanic rocks outcropped. It has been determined that there is a Qf>Qg>Qm relationship between the magnitudes of the factors (Qg, Qf, Qm) affecting Qt in the minarets close to the fault and possible faults. As a result, IRC measurements in all buildings where people live should be done periodically and regularly by the relevant institutions.

Anahtar Kelimeler

Markus 10 Minaret Muğla RadonEye

Kaynakça

  • Al-Tamimi, M.H., Abumurad, K.M. (2001). Radon anomalies along faults in North of Jordan. Radiation Measurements 34, 397–400.
  • Askari, M., Hassanvand, M.S., Naddafi, K., Zarei, A., Yousefi, M., Alimohammadi, M. (2019). Assessment of indoor radon concentration in residential homes and public places in south of Tehran, Iran. Environmental Earth Sciences, 78(10), 1-10.
  • Bossew, P., Petermann, E. (2022). Radon hazard vs. radon risk – consequences for radon abatement policy, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-3145, https://doi.org/10.5194/egusphere-egu22-3145.
  • Bossew, P., Zunic, Z.S., Stojanovska, Z., Tollefsen, T., Carpentieri, C., Veselinovic, N., Komatina, S., Vaupotic, J., Simovic, R.D., Antignani, S., Bochicchio, F. (2014). Geographical distribution of the annual mean radon concentrations in primary schools of Southern Serbia - application of geostatistical methods. Journal of Environmental Radioactivity 127, 141-148.
  • Burghele, B., Ţenter, A., Cucoş, A., Dicu, T., Moldovan, M., Papp, B., Szacsvai, K., Neda, T., Suciu, L., Lupulescu, A., Maloş, C., Florică, Ş., Baciu, C., Sainz, C. (2019). The FIRST large-scale mapping of radon concentration in soil gas and water in Romania. Science of the Total Environment 669, 887–892.
  • Gürer, Ö.F., Yılmaz, Y. (2002). Geology of the Ören and surrounding areas, SW Anatolia. Turkish Journal of Earth Sciences, 11(1), 1-13.
  • Gürer, Ö.F., Sanğu, E., Özburan, M., Gürbüz, A., SaricaFiloreau, N. (2013). Complex basin evolution in the Gökova Gulf region: implications on the Late Cenozoic tectonics of southwest Turkey. International Journal of Earth Sciences, 102, 2199- 2221.
  • Ioannides, K., Papachristodoulou, C., Stamoulis, K., Karamanis, D., Pavlides, S., Chatzipetros, A., Karakala, E. (2003). Soil gas radon: a tool for exploring active fault zones. Applied Radiation and Isotopes 59, 205–213.
  • Kemski, J., Klingel, R., Siehl, A., Valdivia-Manchego, M. (2009). From radon hazard to risk predictionbased on geological maps, soil gas and indoor measurements in Germany. Environ Geol (2009) 56:1269–1279 doi.10.1007/s00254-008-1226-z.
  • Kuluöztürk, M.F., Büyüksaraç, A., Özbey, F., Yalçin, S., Doğru, M. (2019). Determination of indoor radon gas levels in some buildings constructed with Ahlat stone in Ahlat/Bitlis. International Journal of Environmental Science and Technology, 16(9), 5033- 5038.
  • Madureira, J., Paciencia, I., Rufo, J., Moreira, A., Fernandes, E.O., Pereira, A. (2016). Radon in indoor air of primary schools: determinant factors, their variability and effective dose. Environ Geochem Health, 38:523–533 doi.10.1007/s10653-015-9737-5.
  • Moreno, V., Baixeras, C., Font, L., Bach, J. (2008). Indoor radon levels and their dynamics in relation with the geological characteristics of La Garrotxa, Spain. Radiation Measurements 43, 1532–1540.
  • MTA, (2002). 1:500.000 scale Geological Inventory map Series of Turkey, DENIZLI, Maden Tetkik Arama Genel Mudurlugu, Ankara, Turkey.
  • MTA, (2011a). 1:250.000 scale Active Fault Map Series of Turkey, AYDIN (NJ35-11) quadrangle, serial no:7, Maden Tetkik Arama Genel Mudurlugu, Ankara, Turkey
  • MTA, (2011b). 1:250.000 scale Active Fault Map Series of Turkey, MARMARIS (NJ35-15) quadrangle, serial no:8, Maden Tetkik Arama Genel Mudurlugu, Ankara, Turkey
  • Neri, M., Giammanco, S., Leonardi, A. (2019). Preliminary Indoor Radon Measurements Near Faults Crossing Urban Areas of Mt. Etna Volcano (Italy). Front. Public Health 7:105. doi: 10.3389/fpubh.2019.00105.
  • Park, T.H., Kang, D.R., Park, S.H., Yoon, D.K., Lee, C.M. (2018). Indoor radon concentration in Korea residential environments. Environmental Science and Pollution Research 25:12678–12685, doi.org/ 10.1007/s11356-018-1531-3.
  • Pişkin, Ö., Bertrand, J. (1980). Les minéralisations de plomb, zinc et cuivre de Kadikalesi (Presqu'île de Bodrum - Turquie). In: Schweizerische mineralogische und petrographische Mitteilungen, 60(1), 45-68. doi: 10.5169/seals-46657.
Toplam 18 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Çevre Bilimleri
Bölüm Research Articles
Yazarlar

Mutlu Zeybek 0000-0002-1943-8497

Alican Kop 0000-0002-1420-4042

Yayımlanma Tarihi 25 Aralık 2022
Yayımlandığı Sayı Yıl 2022 Cilt: 9 Sayı: 4

Kaynak Göster

APA Zeybek, M., & Kop, A. (2022). Geological and Geostatistical Modeling of Geogenic Radon Potential of Minarets in Muğla Province (SW Turkey). International Journal of Environment and Geoinformatics, 9(4), 194-206. https://doi.org/10.30897/ijegeo.1122026

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