• 제목/요약/키워드: Tidal estuary

검색결과 273건 처리시간 0.025초

친환경간척농지개발과 우리농업 (Phil-Environmental Tide Land Reclamation and Korean Agriculture)

  • 허유만
    • 한국작물학회:학술대회논문집
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    • 한국작물학회 2001년도 추계 학술대회지
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    • pp.59-71
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    • 2001
  • In Korea, It was natural and inevitable to reclaim tidal land for farming due to over-population in small territory. Looking back upon the history of tidal land reclamation in Korea, We can find the first case of it in 13th century KangHwaDo(Island), and also find several records of small scale reclamations of western sea-coast from Korea dynasty to Chosun dynasty. A lot of wide fertile agricultural areas on western sea-coast have been developed through tidal land reclamation for about 1000-year after Korea dynasty. and on these areas, we have produced rice which we live on. An average areas of farming land per capital in korea is only 0.04ha, which is one sixth of global average. For water resources, similarly, capacity of water resources alloted to one person is $11{\%}$ of global average. So, without supplementary water development, we will have suffered from a severe deficiency of water Therefore we must prepare for these predictable short water and food problems. and tidal land reclamation may be suitable alternative to settle these problems. However, tidal land reclamation is a work of closing estuary, intercepting sea water inflow, developing a freshened estuary lake and farming lands etc. therefore it apparently causes a change of ecosystem, water quality and littoral environment. Nowadays, widely recognized the importance of environmental preservation, it is desirable or requested to make phil-environmental and sustainable development minimizing the environmental influence due to tidal land reclamation project. In this paper, the role of tidal land reclamation project in the development process of Korean agriculture was reviewed and the direction of afterwards tidal land reclamation project was suggested.

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낙동강하구 을숙도 갯벌에서 새섬매자기의 생육 특성 (Growth Characteristics of Bolboschoenus planiculmis on the Eulsuk Tidal Flat of the Nakdong River Estuary, Korea)

  • 김구연
    • 생태와환경
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    • 제53권4호
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    • pp.453-460
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    • 2020
  • Bolboschoenus planiculmis is an important prey species for winter migratory birds in the Nakdong River Estuary region, but its population has declined in the last decade due to a physio-chemical shift. To identify the growth and development characteristics of B. planiculmis, we carried out an experimental survey on the aboveground and belowground sections of B. planiculmis specimens in the Eulsuk tidal flat from April to September 2019. We divided the belowground area into two groups: a vegetation group in which B. planiculmis exists and a non-vegetation group in which B. planiculmis does not exist and measured the rate of tubers. We observed a 45% appearance frequency in the vegetation group and only a 5% frequency in the non-vegetation group, indicating that there were no supplies for plant growth. The mean density, length, and biomass of B. planiculmis aboveground were 166.90±149.62 n m-2, 44.39±5.45 cm, and 67.63±54.46 g DW m-2, respectively, which was approximately half of those obtained from the study in the Eulsuk tidal flat in 2002. Tuber number was the highest in the 15~25 cm deep layer(41.50%). The mean number of total tubers belowground was related to different sediment conditions(FS: flat surface, DS: disturbed surface) 251.75±16.86 n pot-1 for FS and 171.00±25.18 n pot-1 for DS, which was significantly different(total tubers: p<0.005). The mean biomass of B. planiculmis above-ground was 21.11±1.60 g DW pot-1 for FS and 15.41±1.38 g DW pot-1 for DS, which was significantly different(p<0.05). This research provides primary materials for the restoration of the Nakdong River Estuary, wintering sites for migratory birds, and protection of B. planiculmis.

새만금 갯벌의 패류 생물량 (Biomass of Shellfish in the Saemangeum Tidal Flat on the West Coast of Korea)

  • 김종식;황선도
    • 한국수산과학회지
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    • 제36권6호
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    • pp.757-761
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    • 2003
  • Spatial distribution and biomass of commercial shellfish were investigated in the Saemangeum tidal flat on the west coast of Korea during August 1999. Thirteen species of shellifsh were collected. Major dominant species of the study area were Umbonium thomasi with a density of $6.7\;ind.{\cdot}m^{-2}\;(38.2\%)$, Mactra veneriformis with $6.6\;ind.{\cdot}m^{-2}\;(37.4\%)$ and Reticunassa festiva with $1.3\;ind.{\cdot}m^{-2}\;(7.2\%)$. Commercially important species such as M. veneriformis ($90.7\;ind.{\cdot}m^{-2}\;69.3\%$), M. lusoria ($15.6\;ind.{\cdot}m^{-2}\;11.9\%)$), C. sinensis ($8.7\;ind.{\cdot}m^{-2}\;6.7\%)$) were dominant in total weight. Most of the shellfish were distributed between the mid-littoral and sub-littoral zones, but C. sinensis and L. flexuosa were distributed mainly in the polluted areas of the supra-littoral zone. The spatial distribution pattern of each shellifsh species generally resembles the Mangyeong and Dongjin estuary. Biomass of commercially important species, M. veneriformis, M. lusoria, C. sinensis and Ruditapes philippinarum in the tidal flat (ca. 850 ha) was estimated to be 774, 135, 67 and 10 tons, respectively.

금강하구역의 수동력학적 변화 (1) -관측자료를 중심으로- (Hydrodynamic Changes in the Keum River Estuary (1) - By Field Observed Data Analysis -)

  • 서승원
    • 한국해안해양공학회지
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    • 제10권1호
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    • pp.10-17
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    • 1998
  • 다양한 공사가 진행되는 금강하구의 수동역학 변화를 조석 및 조류 그리고 수심변화등의 관측자료를 중심으로 해석하였다. 2년여에 걸쳐 수집된 수심측정 자료를 분석한 결과, 군산외항부근의 도류제 축조구간에서는 뚜렷한 조류속도의 증가와 연평균 50 cm에 다다르는 세굴이 진행되는 것이 확인되었다. 그러나 군장산업단지조성호안공사 및 새만금4호 방조제 축조 내면 간사지에서는 가을철 2개월에 30cm의 퇴적이 관측되는 등 유속의 둔화와 함께 퇴적이 급속히 진전되는 현상으로 수동역학의 전이 현상이 나타나 공사로 인한 금강하구의 수동역학체계는 매우 급격하게 변화됨을 보인다

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섬진강 하구역 잘피(Z. marina)서식지의 해양환경 특성 (Marine Environmental Characteristics of Seagrass Habitat in Seomjin River Estuary)

  • 지형석;서희정;김명원;이문옥;김종규
    • 한국해양공학회지
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    • 제28권3호
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    • pp.236-244
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    • 2014
  • This study considered a seagrass habitat in order to analyze the characteristics of a marine environment of seagrass located in the Seomjin river estuary, through an analysis of the distribution of the water depth, field observation, and three-dimensional numerical experiments using an EFDC model. The seagrass habitat was usually distributed at D.L(-) 0.5~0.0 m, and was hardly seen in the intertidal zone higher than that range. The distribution of the water temperature was within the range of $7.0{\sim}23.2^{\circ}C$, and the seagrass was demonstrated to have a strong tolerance to changes in the water temperature. In addition, the salinity distribution was found to be 27.2~31.0 psu, with suspended solids of 32.1 mg/L, which were higher than the previous research results (Huh et al., 1998), implying that there may be a reduction in the amount of deposits caused by the suspended solids. As for the sedimentary facies, they were comprised of 62.7% sand, 19.1% silt, and 18.2% clay, indicating that the arenaceous was superior and the sedimentary facies were similar to that of Dadae Bay. According to a numerical experiment, the maximum tidal current was 75 cm/s, while the tidal residual current was 10 cm/s, confirming that it sufficiently adapted to strong tidal currents. The erosion and deposition are predicted to be less than 1.0 cm/year. Thus, it is judged that the resuspension of sediments due to tidal currents and the changes in sedimentary facies are insignificant.

Numerical Simulation of the Tidal Bores on the Qiantang River

  • Hui W.H.;Pan Cun-Hong
    • 한국전산유체공학회:학술대회논문집
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    • 한국전산유체공학회 2003년도 The Fifth Asian Computational Fluid Dynamics Conference
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    • pp.221-223
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    • 2003
  • The tidal bores of the Qiantang River on the East coast of China are simulated numerically based on the shallow water theory. The governing equations, which were traditionally formulated using water depth, are formulated in terms of water surface level, and the fractional-step method is applied in conjunction with a Godunov-type scheme. In addition, the source terms due to bottom gradient are discretized centrally to exactly balance the flux terms. Our numerical simulation produces tidal bores in excellent agreement with field measurements.

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조석과 하천수 유입을 고려한 낙동강 하구역의 퇴적특성 (The Characteristic of Deposition in Nakdong estuary considering Tide and River discharge)

  • 전용호;류청로;이인철;김헌태
    • 한국해양공학회:학술대회논문집
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    • 한국해양공학회 2003년도 춘계학술대회 논문집
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    • pp.157-162
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    • 2003
  • Nakdong estuary is located at south-eastern coast of the Korea. A lot of sediment from upper river were deposited at this area. It has cause many problem such as changes in topography and tidal current. Changes of characteristic of deposition were cause by topographic change of nakdong estuary. Analyzing and evaluating data, we could predict the direction of movement of the sand bar and the growth toward south-eastern of Nakdong estuary. It was caused by decreasing river discharge after construction of Nakdong-kang barrage.

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금강하구 갯벌 내 환경요인과 저서성무척추동물 군집 분포의 상관관계 (Relationship between Environmental Factors and Macrobenthos Assemblages in Geum Estuary Tidal-flat)

  • 유재원;이채린;박미라;윤지현;강성룡
    • 한국습지학회지
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    • 제21권1호
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    • pp.84-94
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    • 2019
  • 금강하구 서천 및 유부도 갯벌은 동아시아-대양주 철새의 이동경로상 에너지 보충을 위한 중요한 중간 기착지점으로, 갯벌의 저서성무척추동물은 이들의 중요한 먹이원이 된다. 즉, 갯벌의 저서성무척추동물은 에너지 흐름의 중요한 생태적 역할을 담당한다. 금강하구 서천 및 유부도 갯벌의 저서성무척추동물 군집 분포와 환경요인 관계를 파악하기 위해 본 연구가 수행되었다. 가을철 이주 기간에 실시한 저서성무척추동물의 군집 분포 조사 결과, 저서성무척추동물은 총 147종, 밀도와 생체량은 각각 $1,772{\pm}1,342$ 개체/$m^2$, $445.1{\pm}807.6g/m^2$으로 나타났다. 출현종과 서식밀도 자료를 기반으로 각 정점 간 상호 유사도 분석결과, 크게 2개의 군집으로 구분되었다. A 군집은 칠게-고리버들갯지렁이 군집(Macrophthalmus-Heteromastus community)이었고, B군집은 달걀얼굴갯지렁이류-단각류 군집(Spio-Urothoe-Mandibulophoxus community)이었다. B 군집이 A 군집에 비하여 평균 출현종수, 서식밀도, 생체량 등이 월등히 높았다. BIO-ENV 분석 결과, 저서성무척추동물 군집은 퇴적환경 변수인 모래함량과 분급도 조합에 의한 영향을 가장 크게 받는 것(${\rho}=0.500$)으로 나타났다. 종수와 가장 큰 상관성을 보이는 환경변수는 분급도(p=0.015)로 나타났고, 생체량과 가장 높은 상관관계를 보이는 환경변수는 공극수 DO(p=0.003)였다.

하구언 수문작동으로 인한 금강 하구역의 물리적 환경변화: I. 평균해수면과 조석 (Physical Environment Changes in the Keum River Estuary by the Dyke Gate Operation: I. Mean Sea Level and Tide)

  • 권효근;이상호
    • 한국해양학회지:바다
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    • 제4권2호
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    • pp.93-100
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    • 1999
  • 금강 하구역의 해수면 변화에 미치는 하구언 수문 작동의 영향을 알아보기 위하여 군산 내항과 외항의 조석자료를 분석하여 비조석 해수면, 평균해수면 및 주요분조의 조화상수를 구하였다. 비조석 및 평균해수면은 하구언 수문 작동이후 내항과 외항에서 낮아졌고 특히 내항에서 급격한 비조석 해수면의 하강을 보였다. 이러한 비조석 해수면의 감소로 내항과 외항사이의 평균해수면 구배가 변화되었으며 이는 주로 하구언으로부터 담수유출량이 감소하여 발생한 것으로 해석되었다. $M_2$$S_2$ 분조의 진폭은 내항에서 수분작용 후 급격히 증가하였고, 위상은 다소 감소하였다. $O_1$$K_1$ 분조의 위상과 진폭은 변화가 미약하였다 이러한 반일주조 진폭의 큰 변화는 입사파와 하구언에서 반사된 파의 중첩에 의한 것으로 해석된다.

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Prediction of Cohesive Sediment Transport and Flow Resistance Around Artificial Structures of the Beolgyo Stream Estuary

  • Cho, Young-Jun;Hwang, Sung-Su;Park, Il-Heum;Choi, Yo-Han;Lee, Sang-Ho;Lee, Yeon-Gyu;Kim, Jong-Gyu;Shin, Hyun-Chool
    • Fisheries and Aquatic Sciences
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    • 제13권2호
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    • pp.167-181
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    • 2010
  • To predict changes in the marine environment of the Beolgyo Stream Estuary in Jeonnam Province, South Korea, where cohesive tidal flats cover a broad area and a large bridge is under construction, this study conducted numerical simulations involving tidal flow and cohesive sediment transport. A wetting and drying (WAD) technique for tidal flats from the Princeton Ocean Model (POM) was applied to a large-scale-grid hydrodynamic module capable of evaluating the flow resistance of structures. Derivation of the eddy viscosity coefficient for wakes created by structures was accomplished through the explicit use of shear velocity and Chezy's average velocity. Furthermore, various field observations, including of tide, tidal flow, suspended sediment concentrations, bottom sediments, and water depth, were performed to verify the model and obtain input data for it. In particular, geologic parameters related to the evaluation of settling velocity and critical shear stresses for erosion and deposition were observed, and numerical tests for the representation of suspended sediment concentrations were performed to determine proper values for the empirical coefficients in the sediment transport module. According to the simulation results, the velocity variation was particularly prominent around the piers in the tidal channel. Erosion occurred mainly along the tidal channels near the piers, where bridge structures reduced the flow cross section, creating strong flow. In contrast, in the rear area of the structure, where the flow was relatively weak due to the formation of eddies, deposition and moderated erosion were predicted. In estuaries and coastal waters, changes in the flow environment caused by artificial structures can produce changes in the sedimentary environment, which in turn can affect the local marine ecosystem. The numerical model proposed in this study will enable systematic prediction of changes to flow and sedimentary environments caused by the construction of artificial structures.