DOI QR코드

DOI QR Code

A Study of the Prediction of Earthquake Occurrence by Detecting Radon Radioactivity

라돈방사능농도의 측정을 통한 지진발생 예측에 관한 연구

  • 김윤신 (한양대학교 환경 및 산업의학연구소) ;
  • 이철민 (한양대학교 환경 및 산업의학연구소) ;
  • 이승일 (서라벌대학 생명보건학부) ;
  • ;
  • Published : 2003.06.01

Abstract

The purpose of this study was to predict occurrence of earthquakes in Korea by measuring the concentration of radon radioactivity in the air and in the underground water. Two monitoring systems of radon concentration detection in the air were installed in Seoul, East Coast area, whereas of radon concentration in the underground water in Kyungju area during December, 1999 to June, 2001. The distribution of radon concentration in the air in Seoul is as follows Winter(10.10 $\pm$ 2.81 Bq/㎥), autumn(8.41 $\pm$ 1.35 Bq/㎥), summer(5.83 $\pm$ 0.05 Bq/㎥) and spring (5.34 $\pm$ 0.44 Bq/㎥), whereas the distribution of radon in the air in the East Coast area showed some difference as follows : autumn (14.08 $\pm$ 5.75 Bq/㎥), Summer (12.04 $\pm$ 0.53 Bq/㎥), Winter (12.02 $\pm$ 1.40 Bq/㎥) and spring (8.93 $\pm$ 0.91 Bq/㎥). In the meanwhile, the distribution of radon in the water is as follows : spring (123.59 $\pm$ 16.36count/10min), Winter (93.95 $\pm$ 79.69counter/10min), autumn (68.96 $\pm$ 37.53counter/10min) and spring (34.45 $\pm$ 9.69counter/10min). The daily range of the density of radon concentration in Seoul and East Coast area was between 5.51 Bq/㎥ - 9.44 Bq/㎥, 7.15 Bq/㎥ - 15.27 Bq/㎥, respectively. Correlation of the distributions of radon concentrations in the air and in underground water with earthquake showed considerable variations of radon concentration before the occurrence of the earthquake. The results suggested that radon radioactivity seemed to be helpful for the prediction of the occurrence of earthquake.

Keywords

References

  1. 변진섭, 1998, 우리 알아야할 지진, 경문사.
  2. Fujimori, K., T. Yamamoto, S. Otsuka and H. Ishii, 1995, Observations of crustal movements and discharge at Rokko-Takao station-Change associated with the 1995 Hyogo-ken Nanbu earthquake, Ann. Disas. Prev. Res. Inst., Kyoto Univ., 38, 287-296.
  3. King, C.Y., N. Kozumi and Y. Kitagawa, 1995, Hydrogeochemical anomalies and the 1995 Kobe earthquake, Science, 269, 38-39. https://doi.org/10.1126/science.269.5220.38
  4. Koizumi, N., Y. Kano, Y. Katagawa, T. Sato, M. Takaghashi, S. Nishinura and R. Nishida, 1996, Groundwater anomalies associated with the 1995 Hyogo-ken Nan-bu earthquake, J. Phys. Earth, 44, 373-380. https://doi.org/10.4294/jpe1952.44.373
  5. Tsunogai, U. and H. Wakita, 1995, Precursory chemical changes in ground water : Kobe earthquake, Japan, Science, 269, 61-63. https://doi.org/10.1126/science.269.5220.61
  6. Zhang, W. and X. Li, 1994, A survey of the hydrogeochemical observation network for earthquake prediction in China, Earthquake research in China, Edited by State Seismological Bureau, China, ALLERTON PRESS, ING/NEW YORK, 8(3), 337-386.
  7. Igarashi, G., S. Saeki, N. Takahata, K. Sumikawa, S. Tasaka, M. Takahashi, and Y. Sano, 1995, Groundwater radon anomaly before the Kobe earthquake in Japan, Science, 269, 38-39. https://doi.org/10.1126/science.269.5220.38
  8. Noguchi, M. and H. Wakita, 1977, A method for continuous measurement of radon in ground-water for earth-quake prediction, J. Goophys. Res., 42, 1353-1357.
  9. Okabe, S., 1953, Time variation of the atmospheric radon content near the ground surface with relation to some geophysical phenomena, Mem. Coll. Sci. Univ. Kyoto, Ser. A, 28, 99.
  10. 田阪茂樹, et al., 1994, 水中ラドン 險出器の 開發, Radioisotopes, 43, 125-133. https://doi.org/10.3769/radioisotopes.43.125
  11. Iida, T., Y. Ikebe and K. Tojo, 1991, An Electrostatic Radon Monitor for Measurements of Environmental Radon, Res. Lett. Atmos. Electr., 11, 55-59.
  12. Dua, S.K., P. Kotrappa and P.C. Gupta, 1983, Influence of relative humidity on the charged fraction of decay products of radon and thoron, Health Physics., 45, 152.
  13. Iida, T., Y. Ikebe, K. Suzuki, K. Ueno, Z. Wang and Y. Jin, 1996, Continuous measurement of outdoor radon concentrations at various locations in East Asia, Environment International, 22(1), S139-S147. https://doi.org/10.1016/S0160-4120(96)00102-X
  14. Iida, T., Y. Ikebe, K. Suzuki, K. Ueno, Z. Wang and Y. Jin, 1996, Continuous measurement of Outdoor Radon Concentrations at Various Locations in East Asia, Environment International, 22(1), 139-147. https://doi.org/10.1016/S0160-4120(96)00102-X
  15. Lee, K.H. and S.H. Na, 1983, A study of microearthquake activity of the yangsan fault, J. Geol. Soc. Korea, 19, 127-135.
  16. 김재록, 1998, 알기쉬운방사선이야기, 한국원자력문화재단.
  17. Sesana, L., E. Carprioli and G. M. Marcazzan, 2003, Long period study of outdoor radon concentration in Milan and correlation between its temporal variations and dispersion preperties of atmosphere, Journal of Environmental Radiactiveity, 65, 147-160. https://doi.org/10.1016/S0265-931X(02)00093-0
  18. Yoshioka, K., 1998, The vertical profile of 222Rn concentration in the lower atmospheric boundary layer at Shimane peninsula, in Radon and Thoron in the Human Environment, World Scientific publishing, Tokyo.
  19. Yoshioka, K. and T. Iida, The diurnal change in the vertical distribution of atmospheric 222Rn due to growth and rise of the stable stratification height, Environmental International, in press.
  20. 서울특별시 도시철도공사, 1999, 지하철 라돈농도 오염원 측정 및 저감방안 연구.