DOI QR코드

DOI QR Code

낙동강 하구역의 홍수기 방류에 의한 수로별 유속 잔차 및 염분 분포

Spatial and Temporal Variability of Residual Current and Salinity Distribution according to Freshwater Discharge during Monsoon in Nakdong River Estuary

  • Song, Jin Il (Department of Oceanography, College of Natural Science, Inha University) ;
  • Yoon, Byung Il (Department of Oceanography, College of Natural Science, Inha University) ;
  • Kim, Jong-Wook (Department of Oceanography, College of Natural Science, Inha University) ;
  • Lim, Chae Wook (Department of Oceanography, College of Natural Science, Inha University) ;
  • Woo, Seung-Buhm (Department of Oceanography, College of Natural Science, Inha University)
  • 투고 : 2014.01.03
  • 심사 : 2014.06.27
  • 발행 : 2014.06.30

초록

낙동강 하구역은 하구둑이 건설된 이후, 담수는 갑문 개폐에 의해서 인위적으로 방출되고 해수유입은 하구둑에 의해 억제되어왔다. 이로 인해 인위적인 수문 개방에 의한 해수와 담수의 수렴 및 혼합은 낙동강 하구역의 해수순환에 큰 영향을 미치는 것으로 나타났다. 홍수기 방류 중 낙동강 하구역의 수로별 유동 환경과 하구 흐름 특성을 조사하기 위해 유속 및 염분 관측을 수행하였다. 분석 결과 지형적 특징 및 방류의 영향에 의해 수로별 유속 및 염분 분포 특징이 상이하게 나타났다. 낙동강 하구역의 홍수기 방류에 의한 영향은 각 수로별 잔차유속 및 염분 수직분포에 다르게 작용하며, 지형적 특징은 염분침투 범위에 영향을 미침으로써 상대적으로 고염의 물이 정체되는 구간이 존재한다.

After building the dyke in Nakdong River Estuary, mixing of freshwater inflow to ocean and seawater to upstream is controlled by operating the sluice gates. Mixing and convergence of seawater and freshwater by opening the sluice gates, have a major impact on the circulation of seawater in the Nakdong River Estuary. Field measurement was carried out to study the characteristics of the estuary flow and environment of each channel of the Nakdong River Estuary. Vertical salinity distribution and residual current is different from each channel by the river discharge and topographic changes.

키워드

참고문헌

  1. Choi N. Y., Yoon B. I., Kim J. W., Song J. I., Lim E. P., Woo S. B. (2012). The Relation of Cross-sectional Residual Current and Stratification during Spring and Neap Tidal Cycle at Seokmo Channel, Han River Estuary Located at South Korea. J. Kor. Soc. Coast. Ocean Eng, 24(3), 149-158. https://doi.org/10.9765/KSCOE.2012.24.3.149
  2. Han K. M., Kim K. C., Kim J. J. (1993). A Study on the Flow Patterns on the Myunggi-Noksan Region due to Reclamation. Journal of Ocean Engineering and Technology, 7(1), 441-454.
  3. Han J. S., Park S. K., Jung S. W., Roh T. Y. (2011), The Study of Salinity Distribution at Nakdong River Estuary. J. Kor. Soc. Coast. Ocean Eng, 23(1), 101-108. https://doi.org/10.9765/KSCOE.2011.23.1.101
  4. Jang S. T., Kim K. C. (2006). Change of Oceanographic Environment in the Nakdong Estuary. Journal of the Korean Society of Oceanography, 11(1), 11-20.
  5. Joyce, T.M.(1989). On In Situ "Calibration" of Shipboard ADCPs. J.Atmos. Oceanic Technol., 6, 169-172. https://doi.org/10.1175/1520-0426(1989)006<0169:OISOSA>2.0.CO;2
  6. Kim J. W., Yoon B. I., Song J. I., Lim C. W., Woo S. B. (2013). Spatial and Temporal Variability of Residual Current and Salinity according to Freshwater Discharge in Yeoungsal River Estuary. J. Kor. Soc. Coast. Ocean Eng, 25(2), 103-111. https://doi.org/10.9765/KSCOE.2013.25.2.103
  7. Kim, K.C., Kim, J.J., Kim, Y.E., Han, K.M., Choi, K.K. and Jang, S.T. (1996). Outflow characteristics of Nakdong River plume. J. Kor. Soc. Coast. Ocean Eng., 8(4), 305-313.
  8. Kim, Y. E. (1992). Hydrological research of Nakdong river estuary. Institute for Environmental Studies, Inje University, Vol 1. 77-86.
  9. Kim, Y. J. (2004). study on the characteristics of seawater movement and diffusion of pollutants due to the freshwater inflow in the Nakdong estuary. MS Thesis, Inje University.
  10. Kreeke, J. van de (1992). Residual flow in Naples Bay and its effect on constituent concentration, constituent flux and residence time. Dynamics and Exchanges in Estuaries and the Coastal Zone (D. Prandle, Ed.), AGU, 117-133.
  11. Lee D. H., Yoon B. I., Kim J. W., Gu B. H., Woo S. B. (2012). The Cross-sectional Mass Flux Observation at Yeomha Channel, Gyeonggi Bay at Spring Tide During Dry and Flood Season. J. Kor. Soc. Coast. Ocean Eng, 24(1), 16-25. https://doi.org/10.9765/KSCOE.2012.24.1.016
  12. Lwiza, K. M. M., D. G. Bowers, and J. H. Simpson (1991). Residual and tidal flow at a tidal mixing front in the North Sea, Continental Shelf Research, 11(11), 1379-1395. https://doi.org/10.1016/0278-4343(91)90041-4
  13. Preisendorfer, R. W. and C. D. Mobley (1988). Principal Component Analysis in Meteorology and Oceanography. Elsevier,425p.
  14. Ryu C. R., Chang S. D. (1979). Tide and Tidal Current in the Estuary of The Nakdong River. Journal of The Korean Society of Oceanography, 14, 71-77.
  15. Valle-Levinson, A (1999). Spatial gradients in the flow over an estuarine channel. Estuaries, 22, 179-193. https://doi.org/10.2307/1352975
  16. Yanagi, T., Manabu, M., Nomuram M. and Furukawa, K. (2003). Spring-neap tidal variation of residual flow in Tokyo Bay, Japan. Continental Shelf Research, 23, 1087-1097. https://doi.org/10.1016/S0278-4343(03)00102-X
  17. Yu, H. S. and Lee, J., Kang, H.J., Kang, S.R., Shoi, K. S. and Kim, J. S. (1993). Lateral spreading of a river plume and transport of suspended sediments in the Nakdong estuary. J. Kor. Soc. Coast. Ocean Eng., 5(4), 296-301.

피인용 문헌

  1. Enhanced monitoring of water quality variation in Nakdong River downstream using multivariate statistical techniques vol.57, pp.27, 2016, https://doi.org/10.1080/19443994.2015.1049963