• 한국습지학회지
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• 제11권3호
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• pp.71-80
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• 2009

도시하천은 하천특성이 다양하므로 각 하천별 자연형 하천정비계획을 위한 대안 수립 및 선정방법이 필요하다. 그런데 국내의 자연형 하천복원관련 지침이나 기준에서는 구체적인 방법을 제시하지 않고 있다. 일반적으로 하천복원의 궁극적인 목적은 자연성의 회복에 있으며, 최근에는 친수성 증진을 포함하는 추세이다. 본 연구에서는 자연형 하천정비계획 및 사업의 대안선정에 하천자연도를 사용하였다. 국내실정에 맞도록 개발된 AHP를 이용한 하천자연도법을 사용하고, 유럽의 도시하천복원지침(URBEM, Urban River Basin Enhancement Methods)을 참고하여 자연형 하천정비계획의 대안을 간편하게 비교 선정하는 방법을 제시하였다. 대상하천의 하천자연도 평가항목은 하천의 특성을 고려하여 선택한 후, 복수의 대안을 구성하고 대안별 하천자연도를 산정하여 비교함으로서, 각 대안별 자연성 회복효과 및 하천정비계획 성과를 측정하는 것이 용이하였다. 따라서 하천자연도 평가항목을 평가자가 대상하천의 특성에 맞게 선택하여 대안을 선정하면 자연형하천계획 수립에 효과적인 것으로 판단된다.

• 한국환경과학회지
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• 제27권2호
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• pp.63-74
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• 2018

As part of the Four Major Rivers Restoration Project, multifunctional weirs have been constructed in the rivers and operated for river-level management. As the weirs play a role in draining water from tributaries, the aim of this study was to determine the influence of the weirs on the water level of the Nam River, which is one of the Nakdong River's tributaries. Self-organizing maps (SOMs) and a locally weighted scatterplot smoothing (LOWESS) technique were applied to analyze the patterns and trends of water level and quality of the Nakdong River, considering the operation of the Changnyeong-Haman weir, which is located where the Nam River flows into the Nakdong River. The software program HEC-RAS was used to find the boundary points where the water is well drained. Per the study results at the monitoring points ranging between the junction of the two rivers and 17.5 km upstream toward the Nam River, the multifunctional weir influenced the water level at the Geoyrong and Daesan observation stations on the Nam River and the water quality based on automatic monitoring at the Chilseo station on the Nakdong River was affected strongly by the Nakdong River and partly by the Nam River.

• 한국환경과학회지
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• 제22권2호
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• pp.195-203
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• 2013

I investigated the river morphology and river naturality according to the environment of the Hwang River. The numbers of flexions at the upstream regions were more than those of downstream regions. The Hwang River showed very low overall diversity of the flow. Materials of river shore at low channel width were mainly boulders or gravel at the upstream regions, and the middle and downstream were silts and clay. Artificial masonry and natural materials were mixed from materials of river levees. The Hwang River was some of the natural herbaceous vegetation to riparian zones. Land utilities for floodplain were extremely overall farmland were predominant, and partly used by natural vegetation in the forest, a soccer field, some park facilities, residential, and commercial facilities. The water was width sleep / rivers beam ratio of 10 to 20%. Currently estimation for river naturality widely used in rivers were consisted of a narrow wide a variety of items and did not reflect the actual.

• 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.

• 한국환경복원기술학회지
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• 제10권1호
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• pp.1-8
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• 2007

The Anyang River which located in an urban area near Seoul had been managed focusing on supplying home and industrial water and preventing floods, coping with rapid industrialization and urbanization. Consequently, it was changed into a deadly river during 25 years. Its channel was straightened by concrete and water quality deteriorated to BOD 190mg/l. In addition, water quantity has been rapidly decreased and has been drying up. Also, as the river ecosystem, landscape, water-friendly function, and so forth were seriously deteriorated, people turn away from the urban river. From 2001, the master plan under the 10-year has been actively carried out centering on the preceding items, which are healthy river in which fishes inhabit, safe river free from floods and droughts, and pleasant river where citizens visit. As a result, its water quality was remarkably improved by BOD 5mg/l in 2005 and some upper zones were improved enough to allow people to swim. Moreover, various animals including fish and birds gather around the river. Now, the 'Anyang River Restoration Project' is recognized as the first comprehensive and systematic nature-friendly urban river improvement in Korea.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 추계학술발표회
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• pp.435-437
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• 2003

In order to investigate processes and factors controlling the chemical and isotopic compositions of the Han River, seasonal studies were carried out. The North Han River was much lower in the concentrations of total dissolved solids (TDS), dissolved inorganic carbon (DIC) and major ions than the South Han River, but higher in $SiO_2$ concentration, $\delta$$^{34}$ $S_{so4}$ value and $^{87}$ Sr/$^{86}$ Sr ratio. This indicates that the chemical and isotopic compositions of the Han River were strongly controlled by the geology of their drainage basins: silicate rocks in the North Han River and carbonate rocks in the South Han River. The $\delta$$^{34}$ $S_{so4}$ values were relatively higher in the North Han River (5.90$\pm$1.46$\textperthousand$)) than in the South Han River (3.48$\pm$0.73$\textperthousand$). This implies that dissolved S $O_{4}$$^{2-}$ in the North Han River might be mostly derived from deposition of atmospheric sulfates, whereas in the South Han River from oxidation of sulfide minerals in the abandoned poly-metallic deposits and the coal-bearing sedimentary rocks distributed over the upstream as well as deposition of atmospheric sulfates. The $^{87}$ S $r^{86}$ Sr ratios in the North Han River were distinctly higher than those in the South Han River, reflecting water-rock interaction with different rock types.pes.

• 한국콘텐츠학회논문지
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• 제11권6호
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• pp.486-494
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• 2011

유역이나 하천의 변화에 따른 하상의 상승이나 하강은 하천 관리에 있어 핵심적인 요소이다. 하천의 하상 변동을 분석할 때, 기준이 되는 것은 최심 하상고나 평균하상고의 변화이다. 이 때 평균하상고는 계획 홍수위에 대한 하상의 평균이다. 본 연구는 하상 변동 분석에서 기존의 최심 하상고나 평균하상고를 이용할 때 발생하는 제반 문제를 지적하고, 연평균 홍수위에 대해 하상을 평균하는 새로운 평균하상고 개념을 제시하였다. 제안된 방법을 검토하기 위해 낙동강의 1983년, 1993년, 2005년의 3개년의 하상 자료를 이용하여 하상 변동 경향성을 분석하였다. 그 결과 낙동강에서는 1983~1993년 사이에는 대규모 하상 저하는 없었으나, 1993~2005년 사이에는 상당한 규모의 하상 저하가 발생하였다. 1993~2005년 사이에 중류부인 120~200 km 구간에서는 평균적으로 2~3 m, 최대 5 m 정도의 하상 저하가 발생하였고, 그 상류부인 200~240 km 구간에서는 1~2 m 정도의 비교적 작은 규모의 하상 저하가 발생하였다. 그러나 내성천 합류점보다 상류 구간 (240 km 이상의 구간)에서는 하상 상승과 하강은 거의 대부분 국부적인 현상에 머물고 있으며, 대규모 하상 변동이 없다. 이러한 낙동강 하상 저하의 주 원인은 대규모 골재 채취임을 밝혀내었다.

• 한국해안해양공학회지
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• 제19권3호
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• pp.274-294
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• 2007

우리나라 하구의 개수를 파악하기 위해서는 하천의 개수를 파악하는 방법으로 접근할 필요가 있다. 하천의 개수를 파악하는 방법은 하천법에서 규정되어 있는 하천분류기준(국가하천, 지방1급하천, 지방2급하천)을 따르는 것이 바람직할 것으로 사료된다. 우리나라의 국가하천 규모의 하구는 한강(+임진강+례성강), 안성천, 삽교천, 금강, 만경강, 동진강, 영산강, 탐진강, 섬진강, 가화천, 낙동강(+서낙동강), 태화강, 형산강 하구로 총13개(서낙동강, 임진강 분리하는 경우 총15개)이며, 지방1급하천 규모의 하구는 영덕오십천, 삼척오십천, 강릉남대천, 양양남대천 하구로 총4개이다. 반면, 우리나라 연안의 지방2급하천 규모의 하구는 모두 444개(제주도 포함)로 파악되었다. 행정구역별로는 전라남도 108개, 경상남도 94개, 충청남도 52개, 제주도 35개 순으로 파악되었으며, 서해안을 포함한 인위적인 구조물 및 연안개발사업으로 인하여 하구의 기능을 상실한 것으로 판단되는 하구(과거의 하구)가 포함되어 있으며, 하천의 종점이 조정(변경)되는 경우도 발생하기 때문에 분류하는 사람에 따라 다소 차이가 발생 할 수 도 있을 것으로 판단된다.

• 한국물환경학회지
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• 제23권3호
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• pp.332-338
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• 2007

In this study the flow duration curves for Nakdong river basin are analyzed. The TANK model is used as a hydrologic simulation model whose parameters are estimated from 8-day intervals flow data measured by NIER Nakdong River Water Environment Laboratory. As a comparison result between generated natural and present river flow, the present river flow is higher than the natural river flow in the up- and mid-stream of Nakdong river, while the present river flow is lower than the natural river flow in the down stream of Nakdong river.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2015년도 학술발표회
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• pp.242-242
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• 2015

Monitoring the land cover changes in Nakdong River Basins using the multi-temporal remote sensing datasets is necessary for preserving properties in the river basins and monitoring the environmental changes in the river basins after the 4 major river restoration project. This research aims to monitor the land cover changes using the multi-temporal Landsat imageries and the airborne topographic LiDAR data. Firstly, the river basin boundaries are determined by using the LiDAR data, and the multiple river basin imageries are generated from the multi-temporal Landsat imageries by using the river basin boundaries. Next the classification method is employed to identify the multiple land covers in the generated river basin imageries. Finally, monitoring the land cover changes is implemented by comparing the differences of the same clusters in the multi-temporal river basin imageries.