• Title/Summary/Keyword: Radioactive isotope tracer experiment

Search Result 3, Processing Time 0.017 seconds

Analysis of a Pollutant Flow Tracer Test in River using Radioactive Isotope (하천에서 추적자를 이용한 오염물질 거동분석)

  • Kim, Ki-Chul;Lee, Jong-Seok
    • The Journal of the Korea Contents Association
    • /
    • v.9 no.1
    • /
    • pp.400-406
    • /
    • 2009
  • In this study, in order to find the movement of polluted substance that is flown into the river and the characteristics of dispersion, the experiment that used the RI (Radioactive Isotope) tracer in the river was undertaken, and by using the experiment result, the figure modelling was undertaken to analyze the general type of pollutant dispersion. In addition, in order to calculate more accurate dispersion range and moving time, the experiment was done in about 2km from the measuring points of Namdae Stream around the Yongdam Dam of the upper Geum River to the lower stream. In order to find out the flow of river and dispersion of polluted substance, RMA (Resource Modeling Associates)-2 and RMA-4 program are used in study. The site experiment using the RI was implemented for the experiment in the applied area and the same area, and the distance between each zone was set for 1km with the slight difference for site situation and measured the density date of one second distance through the NaI apparatus to measure the density data of one second interval. On the basis of this measured data, it is compared and analyzed with the result of figure copy of the models to make the comparison and analysis of density distribution following the change in expansion coefficient that makes great influence on expansion range and dispersion in natural rivers.

Characteristics of Seasonal Wave, Wave-Induced Current and Sediment Transport in Haeundae Beach (해운대 해수욕장의 계절별 파랑, 해빈류 및 퇴적물이동 특성)

  • Lee, Jong-Sup;Tac, Dae-Ho;Woo, Jin-Gap
    • Journal of Korean Society of Coastal and Ocean Engineers
    • /
    • v.19 no.6
    • /
    • pp.574-585
    • /
    • 2007
  • To analyze the incident wave characteristics around Haeundae beach the long-term deep water wave data computed by wave hindcast method were used and a continuous wave observation was carried out for 1 year at the 20 m of water depth in front of Haeundae beach. Wave observation data showd that the prevalent wave direction was SSW-S in spring and summer seasons while E-SE in autumn and winter. A numerical modeling shows that the waves from E-SE are refracted strongly due to the shoal developed at the south-east side of Haeundae beach. The simulation also shows inflowing nearshore current along the east coast of the beach develops strongly in autumn and winter. Radioactive isotope tracer experiment for 155 days indicated that the tracers moves to the on-shore direction in the 1st and 2nd tracking then dispersed to the E-W direction along the shore.

추적자를 이용한 오염물질 거동분석

  • Kim, Gi-Cheol;Lee, Jong-Seok;Lee, Jae-Cheol;Kim, Yun-Ho;Yeon, Gi-Heum
    • Proceedings of the Korea Contents Association Conference
    • /
    • 2008.05a
    • /
    • pp.289-293
    • /
    • 2008
  • In this study, in order to find out the movement of polluted substance that is flown into the river and the characteristics of dispersion, the experiment that used the RI (Radio Isotope) tracer in the river was undertaken, and by using the experiment result, the figure modelling was undertaken to analyze the general type of pollutant dispersion. In addition, in order to calculate more accurate dispersion range and moving time, the experiment was done in about 2km from the measuring points of Namdaecheon around the Yongdam Dam of the upper Geum River to the lower stream, and modeling was undertaken for the 20km zone from the measuring points to the lower stream. In order to find out the flow of river and dispersion of polluted substance, RMA (Resource Modeling Associates)-2 and RMA-4 program are used in study. The site experiment using the RI was implemented for the experiment in the applied area and the same area, and the distance between each zone was set for 1㎞ with the slight difference for site situation and measured the density date of one second distance through the NaI apparatus to measure the density data of one second interval. On the basis of this measured data, it is compared and analyzed with the result of figure copy of RMA-2 and RMA-4 models to make the comparison and analysis of density distribution following the change in expansion coefficient that makes great influence on expansion range and dispersion in natural rivers. The influence of expansion coefficient on river can be researched and the measured density data, the maximum and minimum density time, and the basic data to calculate the expansion coefficient was prepared in this study.

  • PDF