• Title/Summary/Keyword: Tidal river

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감조하천에서의 저수위 유량산정 다중회귀식 개발 (Development of Regression Equation for Water Quantity Estimation in a Tidal River)

  • 이상진;류경식;이배성;윤종수
    • 한국물환경학회지
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    • 제23권3호
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    • pp.385-390
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    • 2007
  • Reliable flow measurement for dry season is very important to set up the in-stream flow exactly and total maximum daily load control program in the basin. Especially, in the points which tidal current effects are dominant because reliability of the low measurement decrease. The reliable measuring methods are needed. In this study, we analysis the water surface elevation difference of water surface elevation. Quantity relationship to consider tidal currents in these regions. It is known that tidal current effects from Nakdong river barrage are dominant in Samrangjin measuring station. We developed multiple regression equation with water surface elevation, quantity, and difference of water surface elevation and compared these results water measured rating curve. All of these regression equation including linear regression equation and log regression equation fits better measured data them existing water surface elevation quantity line and Among three equations, the log regression equation is best to represent the measured the rating curve in Samrangjin point. The log regression equation is useful method to obtain the quantity in the regions which tidal currents are dominant.

태화강 갑조부의 저수위 수위-유량곡선 개선 (Improvement of Low Water Level Rating Curve in Tidal River Taehwa)

  • 조홍제;황재호;문성준
    • 한국수자원학회논문집
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    • 제33권5호
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    • pp.635-645
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    • 2000
  • 감조하천에서는 수위, 유량과 조석이 상호관련이 있다. 특히 저수위에서 조석의 영향을 감안하지 않은 수위-유량관계는 부정확하다. 본 논문에서는 수위와 조위의 수면차를 변수로 하여 감조하천에서의 유량을 계산할 수 있도록 하였다. 이를 위해 태화강 감조부에 위치한 울산수위관측소 지점의 저수위 유량을 수위 및 수위와 조위의 수면차로 나타내는 다중회귀식을 개발하였으며, 기존의 수위-유량곡선식과 비교한 결과 우수한 적용성을 확인하였다.

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Three Dimensional Study of the Tidal Flat Geomorphology in the $K\breve{u}$m River Estuary by Multidate Image Analysis

  • Yoo, Hong-Rhyong
    • 대한원격탐사학회지
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    • 제2권2호
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    • pp.95-105
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    • 1986
  • The geomorophology of the tidal near $K\breve{u}$m river estuary on the west coast of Korea was studied using satellite images. There Landsat image of different tidal moment were geometrically corrected to be overlapped one another. Then topographic contours were extracted for the analysis with concept of 3-D. According to the morphological analysis, the tidal flats around $K\breve{u}$m river estuary area can be classified in three morphologically different groups: one is developped in a belt type along the shore; another is a delta type in the estuary; the other is developped between the shore line and islands. The morphological characteristics of the tidal flats in the study area seems to be mainly influenced by the tidal dynamics which are very storg on the weatern coastal zone of Korea. However the waves and human activities seem also to be important in some part of the area.

감조하천에서 실측유속과 계산유속과의 관계식 (Relation between Measured and Calculated Velocities in a Tidal River)

  • 남궁돈;이진우;조용식
    • 대한토목학회논문집
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    • 제31권6B호
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    • pp.523-529
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    • 2011
  • 감조하천은 조석의 영향을 받는 하천으로, 하루에 두 번 수위를 상승 및 하강시킨다. 감조하천에서는 홍수시 하천유속 보다 비홍수기 조석에 의한 유속이 구조물 설계에 보다 지배적인 인자가 될 수 있다. 본 연구는 한강 하류부 감조구간에서 비홍수기에 발생된 유속 및 수위 관측을 실시하고 수치해석의 검증자료로 활용하였다. 흐름해석을 위해 부정류 해석이 가능한 UNET모형을 이용하였다. 신곡수중보 아래 감조구간의 조도계수 추정을 위해 통계적인 방법이 사용되었다. 통계적 방법으로 실측수위와 계산수위 간의 불일치율을 이용하였다.

부정류에 의한 감조하천의 홍수분석 (Flood Analysis by Unsteady Flow on Tidal River Estuary)

  • 김현영
    • 한국농공학회지
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    • 제32권4호
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    • pp.81-88
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    • 1990
  • The flow in a river reach where is influenced by tidal motion is characterized by unsteady flow. The flood analysis in the river reach needs depending upon the theory based on the complete unsteady flow equations. In this study the unsteady flow model which is called CRIUM (Channel Routing by Implicit Unsteady Flow Model) was developed and was applied to the Mankyong and Dongjin river in order to analyze the flood characteristics. The results, which were calibrated and verified by the flood records to be measured in the two rivers, show that unsteady flow mode] can be used for the derivation of the flood hydrograph. The peak flood discharges were estimated as 4,960 and $2,870m^3$/sec in 100 year frequency at the estuary of the Mankyong and Dongjin river, respectively. In addition, it was analyzed that the river reaches were not influenced by tidal motion when the discharge magnitude was larger than approximately $3,000m^3$/sec.

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낙동강 하구 호석에 관한 조사연구(I)- 낙동강의 조위변동 - (A study on the tidal phenomena of Nagdong River-mouth - Tidal fluctuations of Nagdong River -)

  • 양윤모;김탁부
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 1982년도 제24회 수공학 연구발표회 논문초록집
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    • pp.3-24
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    • 1982
  • The relations between tidal fluctuation and freshwater discharge are stuied dy use of observed data in the estuarine region of the Nagdong Rivre. Damping modulus which represents the resistance to propagation of tidal wave is estimated, and it is verified that when the fresh water discharge is lower than 300 m/sec., the elevation of mean-water-level at Gupo is the same as mean sea-water-level.

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영산강유역의 지형과 주민생활 (Topography of the Yeongsan River Basin and its Locals' Life)

  • 범선규
    • 한국지역지리학회지
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    • 제8권4호
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    • pp.451-467
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    • 2002
  • 영산강은 남한의 주요 강에 속하며, 유역은 식량생산의 핵심지 중의 하나이다. 영산강유역에는 범람원과 구릉지가 널리 발달되어 있으며, 현재의 영산호 일대에는 간석지도 넓게 분포했었다. 범람원은 '들'로 불리우며, 골짜기가 중은 '물목'의 상류쪽에 넓게 펼쳐진다. 범람원은 조선 발까지는 거의 전부 논으로 재발되었다. 이 농경지를 배경으로 도회지들이 성장했다. 구릉지는 '등', '까끔', '야산' 등으로 불리우며, 나주시와 영암군에 넓게 분포한다. 구릉지의 농경지개발은 1960년대부터 시작되었으며 오늘날에도 진행되고 있다. 많은 개간지의 영농은 외지인들에 의한 임차농의 형태로 영위된다. 간석지 즉 '뻘밭'은 영산강 하류의 남해만에 넓게 펼쳐져 있었으며, 곳곳에 '개옹'으로 불리우던 갯골이 발달했었다. 간석지는 1981년에 영산강하구둑이 준공된 이후 대대적인 간척사업에 의해 농경지로 개발되어 '영산평야'로 바뀌었다. 새로운 평야의 등장으로 모든 취락이 순수 농촌으로 탈바꿈하였다.

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금강하구역에서 영양염 거동에 대한 조석 및 담수유출의 영향 (The Effect of Tidal Cycle and River Runoff on the Dynamic of Nutrients in Keum river estuary)

  • 김종구;강훈
    • 한국환경과학회지
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    • 제11권6호
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    • pp.519-528
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    • 2002
  • This study was to evaluate the impact of river runoff and salt intrusion by tide on nutrient balance of estuary during a complete tidal cycle. 24 hours time series survey was carried out during a spring tide July 2001 on a tidal estuary in the Keum river. Three stations(A,B,C) were set along a transect line of about 10km, which linked the lower part of estuary dyke to the subtidal zone. Surface water was sampled simultaneously at each station every hours f3r the determination of nutrients. Water temperature, pH and dissolved oxygen were measured in situ. Riverine input of silicate and nitrate during ebb tide significantly increased the concentration of all stations. Conversely, during high tide, nutrient concentration were lowered by the mixing of fresh water with sea water Ammonium nitrogen concentration were higher at intertidal zone(Stn.B) due to sewage inflow to Kyeongpo stream and ammonium release under anaerobic conditions. Also, these results was discussed as a biological component that influences the processes of nutrient regeneration within the estuary. Best correlations were found at lower part of estuary dyke(Stn.A) for salinity against DIN(Y=0.121 Sal.+4.97, r2=0.956) and silicate(Y=0.040 Sal.+2.62, r2=0.785). But no significant correlation was found between salinity and ammonium. Unbalanced elemental ratio(N/P, Si/N and Si/P) depended significantly on the import of nutrients (silicate & nitrate nitrogen) from river and stream. The effect of the tidal cycle and river runoff is important that in determining the extend of the variations in nutrient concentrations at all station.

A Study on River Space Restoration and Improvement of Water Quality in Nihonbashi River

  • Ito, Kazumasa
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2007년도 학술발표회 논문집
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    • pp.22-30
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    • 2007
  • Nihonbashi River takes more time to discharge water pollution because it runs low-lying areas and is easy to affect tidal flow from downstream. After rainfall, the water environment of the river has become worse. Even though the river is located in the important metropolitan area in Tokyo, it dose not have any connection with people's lives. We took Nihonbashi River as an example to consider methods for river restoration of improving water quality and river environment in densely inhabited urban areas. Especially, the major issue of river restoration is how smoothly and quickly discharges water pollution which flows into with river flow. The conclusion of this project is the effectiveness of improvement of water environment to construct of rock gates in Nihonbashi River and Kanda River to control inflows from upstream and tidal flows from downstream.

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섬진강 하구역의 3차원 혼합특성 연구 (Three-Dimensional Mixing Characteristics in Seomjin River Estuary)

  • 김종규;곽경일;정정호
    • 한국해양환경ㆍ에너지학회지
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    • 제11권3호
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    • pp.164-174
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    • 2008
  • 섬진강 하구역을 중심으로 광양만과 여수해만에서의 동시 관측한 염분의 현장관측자료의 분석과 기상, 조석, 하천유출수 및 온배수를 고려한 3차원 수치모델(EFDC) 결과를 이용하여 섬진강 하구역의 3차원 혼합특성을 파악하였다. 수치모델에 고려된 입력조건은 수심, 기상, 하천유출수 및 온배수 등이며, 개방경계에서는 염분 및 조석을 고려하여 수치모의하였다. 수치모델 검증은 조위 2개 정점과 조류 2개 정점의 조화분석을 통한조화상수 비교를 통하며 모델결과가 관측결과와 잘 일치하고 있음을 확인하였고, 조시별 유동장을 잘 재현하고 있음을 확인하였다. 동계 및 하계시 월평균 하천유출수를 고려하여 수치모의한 결과, 동계에는 32.0 psu의 등염분선이 섬진강 하구에 국한되어지나, 하계에는 30.0psu의 등염분선이 하천유출량의 영향으로 섬진강 하구역으로 확장되어짐을 확인할 수 있었다. 한편, 섬진강 하구역의 3차원 혼합특성은 전반적으로 섬진강 유출량의 변동, 해수유동구조 및 온배수 등에 의해 복잡한 형태를 보이는 것을 확인할 수 있었다.

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