홍수시 대청호 유역에 발생하는 탁수의 물리적 특성

Characterization of Physical Properties of Turbid Flow in the Daecheong Reservoir Watershed dining Floods

  • 정세웅 (충북대학교 환경공학과) ;
  • 이흥수 (충북대학교 환경공학과) ;
  • 윤성완 (국립환경과학원 금강물환경연구소) ;
  • 예령 (충북대학교 환경공학과) ;
  • 이준호 (충주대학교 환경공학부) ;
  • 추창오 (경동정보대학 하천환경기술연구소)
  • Chung, Se Woong (Department of Environmental Engineering, Chungbuk National University) ;
  • Lee, Heung Soo (Department of Environmental Engineering, Chungbuk National University) ;
  • Yoon, Sung Wan (Geum River environment Research Center, National Institute of Environmental Research) ;
  • Ye, Lyeong (Department of Environmental Engineering, Chungbuk National University) ;
  • Lee, Jun Ho (Division of Environmental Engineering, Chungju National University) ;
  • Choo, Chang Oh (Ecological River Environments Technology Institute, Kyungdong College of Techno-Information)
  • 투고 : 2007.10.11
  • 심사 : 2007.11.09
  • 발행 : 2007.11.30

초록

Fine suspended solids (SS) induced into a reservoir after flood events play important ecological and water quality roles by presenting persistent turbidity and attenuating light. Thus the origin and physical features must be characterized to understand their transport processes and associated impacts, and for the establishment of watershed based prevention strategies. This study was aimed to characterize the physical properties of the SS sampled from Daecheong Reservoir and its upstream rivers during flood events. Extensive field and laboratory experiments were carried out to identify the turbidity-SS relationships, particle size distributions, settling velocity, and mineral compositions of the SS. Results showed that the turbidity-SS relationships are site-specific depending on the locations and flood events in the system. The turbidity measured within the reservoir was much greater than that measured in the upstream rivers for the same SS value. The effective diameters ($D_{50}$) in the rivers were in the range of $13.3{\sim}54.3{\mu}m$, while those in the reservoir were reduced to $2.5{\sim}14.0{\mu}m$ due to a fast settling of large particles in the rivers. The major minerals consisting of the SS were found to be Illite, Muscovite, Albite, and Quartz both in the rivers and reservoir. Their apparent settling velocities at various locations in the reservoir were in the range of 0.06~0.13 m/day. The research outcome provides a fundamental information for the fine suspended particles that cause persistent turbidity in the reservoir, and can be used as basic parameters for modeling study to search watershed based optimal control measures.

키워드

과제정보

연구 과제 주관 기관 : 한국학술진흥재단

참고문헌

  1. 김윤희, 김범철, 최광순, 서동일, CE-QUAL-W2를 이용한 소양호 수온 성층현상과 홍수기 밀도류 이동 현상의 모델링, 상하수도학회지, 15(1), pp. 40-49 (2001)
  2. 서동일, 대청호의 성층현상에 의한 부영양화 특성과 수질관리 방안에 관한 연구, 대한환경공학회지, 20(9), pp. 1219- 1234 (1998)
  3. 신재기, 허 진, 이흥수, 박재충, 황순진, 표층수를 방류하는 저수지(용담호)에서 몬순 탁수환경의 공간적 해석, 한국물환경학회지, 22(5), pp. 933-942 (2006)
  4. 이상욱, 김정곤, 노준우, 고익환, CE-QUAL-W2 모델을 이용한 임하호 선택배제시설의 효과분석, 한국물환경학회지, 23(2), pp. 228-235 (2007)
  5. 정세웅, 성층화된 저수지로 유입되는 탁류의 공간분포 특성 및 연직 2차원 모델링, 대한환경공학회지, 26(9), pp. 970-978 (2004)
  6. 정세웅, 박재호, 윤성완, 배정옥, 대청호 유입탁수의 수리 및 수질특성, 한국물환경학회.대한상하수도학회 공동춘계학술발표회 논문집, pp. 375-378 (2005a)
  7. 정세웅, 오정국, 고익환, CE-QUAL-W2를 이용한 저수지 탁수의 시공간분포 모의, 한국수자원학회지, 38(8), pp. 655-664 (2005b)
  8. 추창오, 고은영, 오수진, 이성우, 김병기, 이지은, 김영규, 2004년 가창댐 탁수의 원인과 부유물질의 환경지질학적 특정, 한국광물학회지, 19(1), pp. 49-61 (2006)
  9. 국가수자원관리종합정보시스템, http://www.wamis.go.kr (accessed May 2007)
  10. 한국수자원공사, 댐운영 실무편람 (2006)
  11. 한국수자원공사, 암하호 탁수저감 방안 수립 보고서 (2004)
  12. 황상구, 정기영, 안동 임하댐 유역의 지질과 임하호 고탁수의 원인, 자원환경지질학회지, 39(6), pp. 771-786 (2006)
  13. APHA, AWWA and WEF, Standard Methods for the Examination of Water and Wastewater, 20th ed., American Public Health Association, Washington, DC., USA (1998)
  14. Chapra, S. C., Surface Water-Quality Modeling, McGraw-Hill Inc., New York (1997)
  15. Dyson, M., Bergkamp, G. and Scanlon, J., Flow: The Essentials of Environmental Flows, IUCN, Gland, Switzerland and Cambridge, UK (2003)
  16. Effler, S. W., Matthews, D. A., Kaser, J. W., Prestigiacomo, A. R. and Smith, D. G., Runoff Event Impacts on a Water Supply Reservoir: Suspended Sediment Loading, Turbidity Plume Behavior, and Sediment Deposition, J of the American Water Resources Association, 42(6), pp. 1697-1710 (2006) https://doi.org/10.1111/j.1752-1688.2006.tb06030.x
  17. Jackson, M. L., Soil Chemical Analysis-Advanced Course., Department of Soil Science, University of Wisconsin, Madison (1969)
  18. Peng, F., Johnson, D. L. and Effler, S. W., Characterization of Inorganic Particles in Selected Reservoirs and Tributaries of the New York City Wate Supply, J of the American Water Resources Association, 40(3), pp. 663-676 (2004) https://doi.org/10.1111/j.1752-1688.2004.tb04451.x
  19. Shin, J. K., Jeong, S. A., Choi, I. H. and Hwang, S. J., Dynamics of Turbid Water in a Korean Reservoir with Selective Withdrawal Discharge, Korean Journal of Limnology, 37, pp. 423-430 (2004)
  20. Tattersall, G. R., Elliotta, A. J. and Lynn, N. M., Suspended sediment concentrations in the Tamar estuary, Estuarine, Coastal and Shelf Science, 57(4), pp. 679-688 (2003) https://doi.org/10.1016/S0272-7714(02)00408-0
  21. Uhrich, M. A., Determination of Total and Clay Suspended-Sediment Loads from Instream Turbidity Data in the North Santiam River Basin, Oregon; 1998-200, in the Proceeding of Turbidity and Other Sediment Surrogates Workshop, April 30-May 2, 2002, Reno, NV (2002)
  22. Wentworth, C. K., A scale of grade and class terms for clasticsediments, Journal of Geology, 30, pp. 377-392 (1922) https://doi.org/10.1086/622910
  23. World Commission on Dams, Dams and Development, Earthscan, London, UK (2000)