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Bathymetric Changes in the Nakdong River Estuary owing to Discharge from the Nakdong River Barrier and Environmental Factors

하구둑 방류와 환경적 인자에 따른 낙동강 하구 지역 해저 지형변화 연구

  • Kim, Ki-cheol (College of General Education, Dong-A University) ;
  • Kim, Sung-Bo (Department of Drone and Transportation Engineering, Young-San University)
  • 김기철 (동아대학교 융합교양대학) ;
  • 김성보 (영산대학교 드론교통공학과)
  • Received : 2021.01.03
  • Accepted : 2021.07.05
  • Published : 2021.07.31

Abstract

In this study, the bathymetric data acquired from 2018 to 2020 and the precipitation and suspended sediment data were analyzed for changes in bathymetry owing to the discharge from the Nakdong River barrier and environmental factors, especially the torrential rain in 2020. Sediment erosion and deposition processes are repeated because of complex environmental factors such as discharge from the Nakdong River barrier and the influence of waves generated from the external sea. In the first half of the year after the dry season, bathymetric data showed relative erosion trends, whereas in the second half after the flood season, deposition trends were identified owing to the increase in sediment transport. However, the data from the second half of 2020 showed a large amount of erosion, resulting in tendencies different to those of erosion in the first half and deposition in the second half of the year. This result is judged to be influenced by the weather in the summer of 2020. The torrential rain in the summer of 2020 resulted in a higher force of erosion than that of deposition. In summary, the tendency for erosion is more significant than that of sedimentation, especially in the main channel area of the Nakdong River.

Keywords

References

  1. ALLEN, J. R. L., 1973, Phase differences between bed configuration and flow in natural environments, and their geological relevance, Sedimentology, 20(2), 323-329. https://doi.org/10.1111/j.1365-3091.1973.tb02054.x
  2. Baily, B., Nowell, D., 1996, Techniques for monitoring coastal change: a review and case study, Ocean and Coastal Management, 32(2), 85-95. https://doi.org/10.1016/S0964-5691(96)00058-0
  3. Busan Development Institute, 2008, Ecological Monitoring of the Nakdong River Estuary (2007~2008).
  4. Davis, R. A., Hayes, M. O., 1984, What is a wave-dominated coast?, Marine Geology, 60(1), 313-329. https://doi.org/10.1016/0025-3227(84)90155-5
  5. Gao, S., Collins, M. B., 1994, Analysis of grain size trends, for defining sediment transport pathways in marine environments, Journal of Coastal Research, 10(1), 70-78.
  6. Hayes, M. O., 1979, Barrier island morphology as a function of tidal and wave regime. In: Leatherman SP(ed) Barrier Islands, Academic Press, New York, l-27.
  7. Jang, S. T., Kim, K. C., 2006, Change of oceanographic environment in the Nakdong Estuary, The Korean Society Of Oceangraphy, 11(1), 11-20.
  8. Jung, S. H., Khim, B. K., Kim, B. O., Lee, S. R., 2013, Shoreline-change rates of the barrier islands in Nakdong river estuary using aerial photography and SPOT-5 image, Ocean and Polar Research, 35(1), 1-14. https://doi.org/10.4217/OPR.2013.35.1.001
  9. K-water, Information about quality of water at a multipurpose dam, 2020, http://www.kwater.or.kr/.
  10. Kim, B. O., Khim, B. K., Lee, S. R., 2005, Development of mosaic aerial photographs for shoreline change study in Nakdong estuary, Ocean and Polar Research, 27(4), 497-507. https://doi.org/10.4217/OPR.2005.27.4.497
  11. Kim, K. C., Kim, S. B., 2014, Characteristics of the plume formed by the buoyant discharges from the river, Journal of the Korean Society of Marine Engineering, 38(8), 988-1001.
  12. Kim, K. C., Yang, H. S., Kim, C. K., Moon, C. H., Jang, S. T., 1999, Variations of physical oceanographic environment caused by opening and closing the floodgate in Nakdong Estuary, Journal of the Korean Society for Marine Environmental Engineering, 2(2), 49-59.
  13. Korea Meteorological Administration (KMA), 2020, http://typ.kma.go.kr/
  14. Le Roux, J. P., 1994, A Spreadsheet template for determining sediment transport vectors from grain-size parameters, Computers and Geosciences, 20(3), 433-440. https://doi.org/10.1016/0098-3004(94)90051-5
  15. Le Roux, J. P., O'Brien, R. D., Rios, F., Cisternas, M., 2002, Analysis of sediment transport paths using grain-size parameters, Computers and Geosciences, 28(5), 717-721. https://doi.org/10.1016/S0098-3004(01)00074-7
  16. McLaren, P., 1981, An Interpretation of trends in grain size measures, Journal of Sedimentary Petrology, 51(2), 611-624.
  17. Park, B. W., Kim, S. B., Kim, J. J., Kim, K. C., 2016, Bathymetric changes off the sea south of Jinwoo-do Island in the Nakdong River estuary, Journal of the Korean Society of Marine Engineering, 40(1), 69-74. https://doi.org/10.5916/jkosme.2016.40.1.69
  18. Park, J. K., Khim, B. K., Lee, H. J., Lee, S. R., 2014, Recent morphological changes off the shoreface of Jinwoodo and Sinjado in the Nakdong river estuary: 2007-2012, Ocean and Polar Research, 36(2), 87-101. https://doi.org/10.4217/OPR.2014.36.2.087
  19. Stutz, M. L., Pilkey, O. H., 2002, Global distribution and morphology of deltaic barrier island systems, Proceedings of 6th International Coastal Symposium, 25-29.