• 제목/요약/키워드: sediment distribution

검색결과 842건 처리시간 0.027초

ENTRAINMENT OF SEDIMENT PARTICLES FROM SCOUR HOLE BY TURBULENT VORTICES DOWNSTREAM OF HYDRAULIC STRUCTURE

  • Kim, Jin-Hong;Lee, Sam-Hee
    • Water Engineering Research
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    • 제2권4호
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    • pp.261-268
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    • 2001
  • This study presents the estimation of the entrainment velocity of sediment particles from the scour hole. Sediment particles are entrained from the scour hole downstream of hydraulic structures by the turbulent vortices. Mathematical form of the entrainment velocity of sediment particles from the scour hole was obtained using the impulse-momentum equation with given value of the vertical component of turbulent velocity of the line vortex. Also, its probability density distribution was obtained with the results that the probability density distribution of the vertical turbulent velocity followed the normal distribution. Experimental results of the entrainment velocity of sediment particles showed relatively good agreements with theoretical ones.

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낙동강 진우도 주변 해역의 모래입도 분포 (Grain size distribution of sediment around Jinudo in Nakdong River Estuary)

  • 유창일;윤한삼;이인철;류청로
    • 한국해양공학회:학술대회논문집
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    • 한국해양공학회 2006년 창립20주년기념 정기학술대회 및 국제워크샵
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    • pp.441-444
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    • 2006
  • Nakdong river estuary is located at south-eastern coast if the Korea. Especially, Complicating topography change is generated by interaction of much sediment, wave and tide. This study is investigated into observation data of grading size distribution in the post and surface sediment characteristics is investigated into grading size analysis using sieve analysis in Nakong river estuary. As a result, mean diameter of surface sediment is distributed to front of shoal as a size with 0.1~0.2 mm and mean diameter of the last generated shoal is about 0.2~0.3 mm.

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경기만 퇴적물의 중금속 분포 특성 (Characteristics of Metal Distribution in the Sediment in Kyeonggi Bay, Korea)

  • 이종현;이정석;김범수;이창복;고철환
    • 한국해양학회지:바다
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    • 제3권3호
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    • pp.103-111
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    • 1998
  • 본 연구는 경기만 표층 퇴적물의 지화학적 특징과 입도분포와의 관계를 조사하기 위해서 수행되었다. 1995년 12월에 채집한 총 90 개 퇴적물 시료를 대상으로 입도분포, 유기탄소와 중금속 함량(Al, Fe, Mn, V, Co, Ni, Cr, Zn, Cu)을 분석하였다. 또한 1981년에 조사된 자료와 비교함으로써 그 동안의 변화를 파악하고자 하였다. 퇴적물 입자의 크기는 몇몇 지역에서 1981년과는 다른 양상을 보였다. 1994년에 완공된 시화방조제 부근의 퇴적물은 이전에 비해서 세립해졌다. 공항건설을 위한 매립공사가 진행되고 있는 영종도 부근의 퇴적물의 경우 세립한 퇴적상에서 혼합 퇴적상으로 변하였다. 유기물과 중금속 함량은 전반적으로 입도에 의존적인 분포를 보이고 있지만, 인천북항의 퇴적물에서는 입도와 무관하게 유기물과 Ni, Cr, Zn 그리고 Cu 등의 중금속이 높은 농도로 농축되어 있었다.

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Sediment Erosion and Transport Experiments in Laboratory using Artificial Rainfall Simulator

  • Regmi, Ram Krishna;Jung, Kwansue;Nakagawa, Hajime;Kang, Jaewon;Lee, Giha
    • 한국지반환경공학회 논문집
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    • 제15권4호
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    • pp.13-27
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    • 2014
  • Catchments soil erosion, one of the most serious problems in the mountainous environment of the world, consists of a complex phenomenon involving the detachment of individual soil particles from the soil mass and their transport, storage and overland flow of rainfall, and infiltration. Sediment size distribution during erosion processes appear to depend on many factors such as rainfall characteristics, vegetation cover, hydraulic flow, soil properties and slope. This study involved laboratory flume experiments carried out under simulated rainfall in a 3.0 m long ${\times}$ 0.8 m wide ${\times}$ 0.7 m deep flume, set at $17^{\circ}$ slope. Five experimental cases, consisting of twelve experiments using three different sediments with two different rainfall conditions, are reported. The experiments consisted of detailed observations of particle size distribution of the out-flow sediment. Sediment water mixture out-flow hydrograph and sediment mass out-flow rate over time, moisture profiles at different points within the soil domain, and seepage outflow were also reported. Moisture profiles, seepage outflow, and movement of overland flow were clearly found to be controlled by water retention function and hydraulic function of the soil. The difference of grain size distribution of original soil bed and the out-flow sediment was found to be insignificant in the cases of uniform sediment used experiments. However, in the cases of non-uniform sediment used experiments the outflow sediment was found to be coarser than the original soil domain. The results indicated that the sediment transport mechanism is the combination of particle segregation, suspension/saltation and rolling along the travel distance.

포획된 부유물질의 입도분포를 고려한 탁도계 검교정 (Turbidity Meter Calibrations Based on Grain Size Distribution of Trapped Suspended Material)

  • 조홍연;김백운
    • 한국해안해양공학회지
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    • 제15권1호
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    • pp.33-38
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    • 2003
  • 가덕도 인근 연안해역에서 채취된 해저 퇴적물과 연직방향으로 배열된 표사포획장치로부터 획득된 부유물질을 이용하여 탁도계 검교정을 수행하였다. 포획된 부유물질은 모래 함량이 약 6%인 해저 퇴적물에 비하여 주로 실트 및 점토로 조성되었으며, 해저면으로부터의 놀이가 증가함에 따라 세립화하는 경향을 보였다. 해저 퇴적물에 대한 탁도계 검교정 선형 회귀식의 기울기는 최소값으로 나타났으며, 수심별로 포획된 부유물질에 의한 선형 회귀식의 기울기는 포획 고도가 증가함(즉, 입도가 감소함)에 따라서 점진적으로 증가하였다. 이러한 결과는 해저 퇴적물에 대한 탁도계 검교정 결과로부터 부유물질 농도를 환산할 경우 과대추정의 오차가 발생되며, 본 연구해역의 경우에는 그 오차가 최대 25%까지 증가할 수 있다는 것을 보여준다. 따라서 해저 퇴적물보다는 수층에서 포획된 부유물질의 입도분포를 고려하여 보정된 검교정식을 적용하는 것이 부유물질 농도의 측정오차를 최소화하는 방법으로 사료된다.

Monsoonal sediment transport along the subaqueous Mekong Delta: An analysis of surface sediment grain-size changes

  • Thanh C., Nguyen;An T., Dang;Khuong N.T., Tran
    • Ocean Systems Engineering
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    • 제12권4호
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    • pp.403-411
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    • 2022
  • Annually, about 48-60% of sediment discharge of the Mekong River is delivered near the mouths of the Mekong River branches which is mostly coinciding with the southwest (SW) monsoon. This sediment budget in turn will be southwestwardly transported along the coast of the Mekong Delta (MD) during the northeast (NE) monsoon. Analysis of monsoonal changes in grain-size distribution (GSD) of surface sediment contributes to a better understanding of erosion and deposition processes along the MD. This study aims to figure out changes in GSD and sediment textures along the MD between SW and NE monsoons based on 183 surficial sediment samples collected along the MD during two field surveys carried-out in October 2016 and February-March 2017. Compared to the GSD during the SW and NE monsoon, the GSD along the MD changed significantly, especially in the estuary areas and along the coast of Bac Lieu and Ganh Hao. Whereas, in the west coast of the MD, GSD seem no changes between the two seasons. These changes in seabed sediment suggest that sediment with grain-sizes ranging from silt to fine sand can be transported during only a NE season.

파랑과 흐름이 공존하는 영역에서의 평형 및 비평형 부유사이동특성 (Characteristics of Suspended Sediment Transport in Wave and Current Co-Existing System)

  • 김규한;;배기성
    • 한국해안해양공학회지
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    • 제3권4호
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    • pp.209-216
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    • 1991
  • 파랑과 흐름이 공존하는 영역에서의 부유사이동특성, 특히 농도분포형상 및 확산계수, 기준점농도에 미치는 흐름의 영향에 대하여 정량적인 평가를 시도하였다. 또한, 비정상이류확산방정식에 기반한 고정도수치계산법을 이용하여 평형상태에서의 부유사농도분포 및 지금까지 예측하기 곤란했던 비평형상태의 부유사농도분포의 재현을 시도하여 본 결과, 비교적 만족할만한 재현도를 나타내주었다.

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Meiobenthos in Nha Trang Bay of the South China Sea (Vietnam)

  • Pavlyuk, Olga N.;Trebukhova, Julia A.
    • Ocean Science Journal
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    • 제41권3호
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    • pp.139-148
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    • 2006
  • The distribution of the taxonomical composition and the density of meiobenthos depending on the sediment type has been studied in bottom sediments of Nha Trang Bay. The maximal population density and the taxonomical diversity were observed in the silted coarse and heterogeneous sand ($1031.4{\pm}419.7\;ind.\;10\;cm^{-2}$), whereas the minimal level of density and diversity ($588.1{\pm}152.5\;ind.\;10cm^{-2}$) was in the coarse and heterogeneous sand with shell debris and corals. The correlation between the median diameter of sediment particles and population density of meiobenthos has been revealed (r=0.82, p<0.05). In bottom sediments of Nha Trang Bay, twenty six taxonomic groups of meiobenthos were observed. Nematodes dominated in all sediment types. Representatives of four orders, twenty eight families and ninety seven genera of marine nematodes were identified. The vertical distribution of meiobenthos in different sediment types was considered. A sediment column (10 cm height) was sectioned by five 2 cm portions. In the last layer (8-10 cm) the most number of meiobenthic groups was found in sandy sediments. In the lower layers of silt sediments, only nematodes were found.

부유사 및 하상토 입도분포를 고려한 저수지 퇴사의 장기모의 (Long-Term Simulation of Reservoir Sedimentation Considering Particle-Size Distributions of Suspended Sediment and Bed Materials)

  • 김대근;신광균
    • 한국수자원학회논문집
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    • 제46권1호
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    • pp.87-97
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    • 2013
  • 본 연구에서는 HEC-RAS의 하상변동모형을 이용하여 고농도의 유사가 중소규모의 저수지에 유입하여 삼각주를 형성하는 과정을 유사의 입도분포를 고려하여 해석하였으며, 다음과 같은 결론을 얻을 수 있었다. 먼저, 삼각주의 시공간적인 분포와 년간 저수지에 퇴적되는 입도별 퇴사량을 합리적으로 예측할 수 있었다. 또한 저수지의 특정위치에서 특정시기에 어떤 입도의 유사가 주로 퇴적되는지를 합리적으로 예측할 수 있었다. 이러한 유사의 입도분포를 고려한 모의와 분석은 수자원관련 시설물의 계획 및 유지관리에 필요한 유용한 정보를 제공해 줄 수 있을 것으로 판단된다.

중소유역의 수문학적 특성이 하천유사량에 미치는 영향 (The Effects of Hydrologic Characteristics on Sediment Discharge in Streams with Small and Medium Size Watersheds)

  • 김활곤;서승덕
    • 한국농공학회지
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    • 제38권3호
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    • pp.127-136
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    • 1996
  • The purpose of this study is to provide with information for the water resources development and management in stream management planning, such as information on the sediment trensport, design of dam and water facilities, river improvement and flood plains management. The major results obtained from the field measurement and analysis of the watershed characteristics, hydraulic and sediment characteristics are as follows ; 1. The rating curve formulas obtained from the analysis of the hydraulic characteristics data collected are ; Q-=110.563 $(H-0.474)^2$ for 0.7m$(H-0.146)^2$ for 0.4m$Sr=aX{^2} {_1} X^{c}{_2}$, in the experimental watershed.

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