• 제목/요약/키워드: Nagdong River

검색결과 45건 처리시간 0.041초

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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낙동강 삼각주 말단의 지형 변화 (Landform Changes of Terminal Area of the Nagdong River Delta, Korea)

  • 오건환
    • 한국제4기학회지
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    • 제13권1호
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    • pp.67-78
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    • 1999
  • 낙동강 삼각주 말단은 하중도와 사주 그리고 간석지의 퇴적미지형으로 이루어져 있으며, 이들 미지형들은 해안선에 평행하게 바다쪽으로 향해 하중도군, 제1사주군, 제3사주군, 그리고 제4사주군의 순으로 배열되는 특징을 나타낸다. 하중도군은 을숙도-명호도-신호도로서 1916년 이전에 형성되었고, 제1사주군인 맹금머리등-대마등-진우도는 맹금머리등을 제외하면, 하중도군과 함께 1916년 이전에 출현된 사주들이다. 제2사주군인 백합등-장자도와 제3사주군인 나무싯등-새등은 각각 1970년과 1984년 이전에 형성되었으며 제4사주군인 다대등-도요등은 최근인 1990년 이후에 등장된 사주로서 현재 합성되어 있다. 이러한 사실은 삼각주 말단이 1987년 낙동강 하구둑 건설이후 빠르게 전진 발달하고 있다는 것을 의미하며, 이는 하구둑과 신호공단 및 명지주거지의 조성을 위한 하구 부근의 준설과 인공적인 수로의 변경에 따른 토사의 일시적 재퇴적현상에서 비롯된 것으로 보이며, 그 결과 연구지역의 미지형 변화는 삼각주 말단에서 일어나고 있는 낙동강의 유수와 파랑 그리고 연란류 및 조류의 에너지가 하구둑 건설 이전에 작용했던 것처럼 균형을 이룰 때까지 계속될 것으로 생각된다.

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낙동강 하류 수계에서 저층수 및 저질퇴적층의 환경 (Environmental Conditions of Sediment and Bottom Waters near Sediment in the Downstream of the Nagdong River)

  • 정하영;조경제
    • 생태와환경
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    • 제36권3호통권104호
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    • pp.311-321
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    • 2003
  • 낙동강의 하류지역 (낙동강, 서낙동강 및 조만강)의 수질오염에 있어서 저질퇴적층의 영향을 파악하기 위하여 저질과 저층수의 환경을 조사하였다. 세 지점에서 수질을 모니터링 하였을 때, 고수온기인 5 ${\sim}$ 8월에 수표면과 저층간의 수온, 용존 산소, $PO_4\;^{3-}$, $NH_4\;^+$의 차이가 컸다. 7 ${\sim}$ 8월 중에 저층의 용존 산소는 대체로 5 mg $O_2/l$ 이하로 유지되는 빈도가 높았고, 이 기간에 저질-수층 경계면에서 $PO_4\;^{3-}$$NH_4\;^+$의 이동이 활발할 것으로 추정된다. 저질에 가까운 저층에서 무기 영양염 농도와 수층chl-a 농도는 지역적으로 낙동강<서낙동강<조만강의 순이었고 수심이 얕고 저질 퇴적층이 발달할수록 수질에 미치는 영향이 컸다. 저질의 유기물 함량은 하류 쪽으로 갈수록 증가하였고, 낙동강보다는 서낙동강 수계에서 더 높았으며 저질의 가비중과 역 상관관계로서 오염도 뿐 아니라 저질입도와 관련이 있었다. 저질 공극수내 $PO_4\;^{3-}$$NO_3\;^-$은 수층보다 그 농도가 매우 낮았으나 $NH_4\;^+$$SiO_2$농도는 수층과 유사하거나 더 높았다. 공극수 내 $NH_4\;^+$$SiO_2$농도는 저질 깊이에 따라 증가하였고, $PO_4\;^{3-}$는 감소한 반면 $NO_3\;^-$은 일정하였다. 반면 저질 내 치환성 무기영양염은 공극수 무기영양염 농도보다 최대 수백배 높았으며 $PO_4\;^{3-}$, $NH_4\;^+$, $SiO_2$는 저질 깊이에 따라 감소했으나 $NO_3\;^-$는 증가하였다.

낙동강하구의 습생식물 및 수중식물 구계와 분포 (Flora and Distribution of Vascular Hygro- and Hydrophytes from the Estuary of Nagdong River)

  • 정영호
    • Journal of Plant Biology
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    • 제26권4호
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    • pp.197-206
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    • 1983
  • Flora and distribution of vascular hygro- and hydrophytes were investigated from April to June, 1983 on the seven sampling sites along the estuary of Nagdong River. As the result, total 60 kinds of vascular plants are investigated, among them 13 kinds are aquatics; Rotala indica var. uliginosa, Myriophyllum spicatum, Allisma canalicultum, Vallisneria asiatica, Hydrilla verticillata, Potamogeton berchtoldii, P. crispus, Ruppia maritima, Phyllospadix iwatensis, Zostera marina, Juncus effusus, Phragmites communis, and Scirpus triqueter. Present hydrophytes are largely confined to the main-stream zone. The transition zone is poorly habitated by hydrophytes and considered for the distributconfined to the estuary and coastal zone. However, long-term conditions of salinity gradient appear to be primarily responsible for the present flora and distribution.

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부산일원(釜山一圓) 연안해빈사(沿岸海賓砂)의 퇴적학적(堆積學的) 연구(硏究) (Sedimentological Study of Littoral Beach Sand in Busan Area, South Korea)

  • 이유대;최광선
    • 자원환경지질
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    • 제16권2호
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    • pp.65-78
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    • 1983
  • This report deals with the sedimentological study of the littoral sand of beaches in the Busan area. The purpose of this report is to know the grain size, mineralogical composition, heavy mineral and clay mineral of the beach sands, and gravity measurements of the Nagdong River Deltas. 1) As a whole, the littoral sand of the beaches are composed of uniformly medium grained, moderately sorted and nearly symmetrical. The barrier sand of the Nagdong Estuary is composed of fine grained, well sorted and nearly symmetrical. 2) The littoral sand of the beaches is transported by saltation and rolling. The barrier sand of the Nagdong Estuary is transported by suspension and saltation. 3) In the littoral sand of the beaches, the ratio of feldspar to quartz is 1 :2.31 and in the barrier sand of the Nagdong Estuary 1:1.40. 4) The content of heavy mineral of samples ranges from 0.54 to 3.87 %. The principal heavy minerals are hornblende, pyroxene, epidote, garnet, leucoxene, zircon, apatite, magnetite, hematite and ilmenite with minor accessories of rutile and olivine. 5) The x-ray diffraction analysis of the clay mineral informs the existence of quartz, feldspar, kaolinite and montmorillonite. The montmorillonite is considered to have been derived from the alteration of acidic volcanic rocks. 6) To determine the depositional structure of the Nagdong Estuary, Gravity measurements were made. Free air anomaly ranges from 14.5 mgal to 33.5 mgal and Bouguer anomaly ranges from 14.3 to 23.5 mgal and both are closely related to the topography. According to the interpreted layer structure, the upper layer composing sand, silt and clay, the intermediate layer composing sand with gravel, the lower layer composing weathered and soft rock, and bed rock composing hornfels or andesite. 7) The depositional environments of the study, the littoral area is dominated by the marine environment and the Nagdong Estuary by the mixed environment.

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변형어에 관한 형태 및 중금속함량조사 -낙동강에 누식하는 Mugil Cephalus를 중심으로- (A Study on the forms and the content of heavy metals of deformational Mugil cephelus from the Nagdong River)

  • 어은수
    • 한국환경보건학회지
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    • 제8권1호
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    • pp.31-43
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    • 1982
  • Seventy-seven Mugil cephalus of spinal deformation, living in Hanam, Nogsan, and Myeongji area, the downstreams of the Nagdong River, were collected in order to determine their forms and the levels of heavy metal contamination between March and October, 1981. The specimens were examined by X-ray and content of cadmium, lead, copper, and zinc by atomic absorption spectrophotometer. The results were summarized as follows: 1. The rate of appearance of deformational fish to the total Mugil cephflus were 4.3% (13 fish), 5.7% (17 fish), relatively high in May and June (dry season). Meanwhile during March and October they were low by 1.0% (3 fish), 2.0% (6 fish). As far as the research areas are concerned, they appeared in larger numbers in downstreams than in upper streams Myeongji (39), Nogsan (25), and Hanam (13). 2. Concerning with fractured parts of vertebraes,86 percent (66 out of 77) had their caudal regions fractured and 72 percent (55) their first to seventh caudal regions fractured. 3. The average levels of cadmium, lead, copper, zinc detected from flesh were 0.26ppm, 2.06ppm, 6.35ppm, 0.85ppm on the other hand, they were 0.22ppm, 1.84ppm, 5.03ppm, 0.93ppm in normal fish. 4. The average levels of cadmium, lead, copper, zinc measured in the bones were 0.39ppm, 2.55ppm, 8.97ppm, 2.73ppm. Meanwhile, from normal fish they were 0.33ppm, 2.25ppm, 7.24ppm, 2.42ppm. 5. Compared with regional heavy metal contamination such as cadium, lead, zinc, Myeongji area had higher contamination content than Nogsan area Nogsan area than Hanam area. 6. Compared with heavy metal contamination level in their tissues, cadmium was highly found in bones Lead and copper were highly detected in viscera. Particularly in skeleton cadmium was 560 times, zinc 160 times in proportion to those in the downstreams of the Nagdong River.

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음료수및 공업용수로서의 낙동강 하류수질에 대하여 2. 남지이남 낙동강 하류수의 중금속 함량에 대하여 (1977년 5월~1978년 4월) (STUDIES ON THE WATER QUALITY OF NAGDONG RIVER DOWNSTREAM FOR DRINKING WATER AND INDUSTRIAL SUPPLY WATER 2. ANNUAL VARIATIONS OF HEAVY METAL CONCENTRATIONS IN THE DOWNSTREAM WATER OF NAGDONG RIVER FROM MAY 1977 TO APRIL 1978)

  • 원종훈;양한섭
    • 한국수산과학회지
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    • 제11권3호
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    • pp.139-146
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    • 1978
  • The annual variations of some heavy metal concentrations, Al, Mn, Fe, Cu, Pb, Zn, Cd, Hg were determined on tile day of spring tides in every month from May 1977 to April 1978 at eight stations in the Nagdong River downstream. Samples were taken at intervals of one or two hours from 7 a.m. to 7 p.m. at each station. Annual ranges and means of concentrations of the heavy metals are as follows : aluminium 40.7-3700 ppb, 286 ppb; manganese 10.3-261.5 ppb, 80.8 ppb; iron ND-1237 ppb, 147.7 ppb; copper ND-30.9 ppb, 2.49 ppb; lead ND-29.9 ppb, 1.10 ppb; zinc ND-156.8 ppb, 5.61 ppb; cadmium ND-1.22 ppb, 0.09 ppb; mercury ND-0.37 ppb, 0.02 ppb respectively. In general, the contents of heavy metals except managanese and mercury were higher at the stations above station one, Kupo, though the ranges of the contents showed remarkable difference according to the sampling stations. Annual means of the concentrations of iron and manganese were exceeded already the desirable standards for industrial water and closed to the criteria of raw water for public supply. The values that over the criteria of raw water were sometimes found. Mercury concentration showed comparative high level such as ND-0.37 ppb in annual range but it was not over the environment criterion, 0.5 ppb. Aluminium, iron and mercury showed generally high values in summer period and other metals in winter period, through the patterns of seasonal variations were difference depending on the sampling stations and the kind of metals.

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Heavy Metals In The Nagdong Estuary

  • Lee, Soo-Hyung;Lee, Dong-Soo;Kim, Eun-Soo;Kwak, Hi-Sang;Lee, Kwang Woo
    • 한국해양학회지
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    • 제16권1호
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    • pp.24-30
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    • 1981
  • In order to investigate water pollution of heavy metals in the Nagdong Estuary, samples were collected five times from August 1978 to April 1979 every other month, and analyzed for Cd, Cu, Pb and Zn by atomic absorption spectrophotometry. The results showed no significant heavy metal pollution in most parts of the studied areas, except near the outfalls of the Sasang Industrial Complex. In general, the heavy metal contents were higher in the dry season than in the rainy season due to the dilution effect of river water flow. Distribution of heavy metals in the dissolved and the particulate fractions were also investigated.

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