• Ocean and Polar Research
• /
• 제36권2호
• /
• pp.87-101
• /
• 2014

Recently, more attention has been paid to the geomorphological changes in the Nakdong River Estuary, because those changes are caused by artificial activities including weirs, reclamation and construction. In order to analyze quantitatively the recent geomorphological variability in the Nakdong River Estuary, we surveyed the depth and elevation of submarine topography near Jinwoodo and Sinjado from March 2007 to February 2012. A statistical method (based on Digital Shoreline Analysis System) and an Empirical Orthogonal Functions method were used to evaluate the morphological changes. According to the statistical variables (DCE, NDC, EPR, LRR), the highest amount and rate of accumulation were recorded around the Gadeokdo whereas the greatest amount of erosion appeared around the coast off the eastern part of Sinjado. In particular, a dynamic variation of morphology was clearly observed in the vicinity of the sub-tidal channel located between Jinwoodo and Sinjado, which seems to be attributable to channel migration. As a result of the EOF method, the first mode (48.7%) is most closely related to the pattern of morphological variability that might be associated with the westerly movement of sediment by longshore current. The spatial variability of the second mode (16.6%) was high in the shoreface of Sinjado, showing a 4-year periodicity of temporal variability. The strong correlation (coefficient 0.73) between the time coefficient and suspended sediment discharge from Nakdong River emphasizes the role of sediment discharge to deposition in this area. The spatial variability of the third mode (11.3%) was distributed mainly around the coast off the eastern part of Sinjado, which is related to the movement of the coastline of Sinjado. Based on the last 5 year's data, our results suggest that the study area is characterized on the whole by a depositional pattern, but the extent of sedimentation is different locally.

• 한국조경학회지
• /
• 제23권3호
• /
• pp.132-143
• /
• 1995

Comprehensive development projects were carried out on the Han River from 1982 to 1986 for the purpose of creating a more serviceable places such as a riverside parks and autoroads and so on. However because of the river development, river ecosystem and function were destroyed. And many local autonomous entity follows comprehensive development projects as if it is a model case. To investigate the impact that the river development effects the river ecosystem, two sites which are Anyangcheon and Sooipcheon were surveyed in the right of around plants ecosystem and structure. Two sites are creek of the Hna River. Sooipcheon maintains the sound ecosystem. It has sufficient carrying capacity for the river recreation activity. The reason is that a hydrophyte absorbs nutrients from the stream and the river ecosystem meets the around terrestrial one neturally. Number of hydrophyte increase from upstream going forward to downstream. Number of hydrophyte increase from upstream going forward to downstream. Anyangchoen is seriously polluted stream out of many branch stream of the Han river. In the upstream various woody plants and hydrophyte appeared. But from the river developed area at midstream, naturalized plants dominated such as Bidens tripartita, panicum dichotomiflorum etc. To manage the creek ecologically, hydrophyts were introduced in partly for natural purification after rehavilitate the riverside, and steadily monitoring is demanded.

• 생태와환경
• /
• 제44권4호
• /
• pp.358-363
• /
• 2011

본 연구는 영산강수계 광주지역에 대하여 XAD와 FTIR를 이용하여 자연유기물질에 대한 분포특성을 연구하였다. XAD 8/4 resin을 이용한 NOM fractionation 분석은 친수성 및 소수성을 변별하는데 사용되어졌다. FT-IR은 자연유기물의 구조에서 기능족을 분석하는데 사용되어졌다. XAD 조사에서 영산강본류의 광주상류지점(GJ-1), 광주하류지점(GJ-2), 광주천(GJC), 광주하수처리장(GJS) 등 4개 지점에서 대부분 친수성으로 조사되었다. 다만, 3월에 GJ-1 지점에서는 소수성이 주를 이루었다. 5월에는 수온의 상승과 함께 미생물의 활성의 증가로 4개 지점 공통적으로 친수성으로 조사되었고, 10월에는 3월과 매우 유사한 결과가 되었다. FT-IR 조사에서는 넓거나 높아 뚜렷한 피크들이 주로 지방족 화합물, 특히 OH 그룹, CH, $C-H_2$, $C-H_3$ 및 C-O 알코올 그룹들로 나타났고, 이들은 친수성 물질들이다. FT-IR 조사에서 그 외의 피크들은 약간의 방향족 화합물, 특히 C=O (Ketone) 그룹이 나타났다. 결과적으로 본 연구에서 영산강수계 광주지역은 주로 친수성 물질들이며, 지방족 화합물(OH, C-H etc.)인 것으로 조사되었다.

• 안보군사학연구
• /
• 통권1호
• /
• pp.423-446
• /
• 2003

While the demand for energy has shown a sharp increase recently, the supply seems to be limited by the fact that the conventional fossil fuel energy or nuclear energy has its own environmental problems such as, for example, global warming or nuclear waste disposal. To overcome such limited supply of energy, the utilization of natural thermal energy such as river water and seawater as well as treated sewage can be a substantial supplement. The potential use of the unused energy has become more and more feasible these days as the heat pump technology has been advanced. In the present study, the unused energy resources are estimated on regional and monthly basis for each resource by the method proposed here in order to establish the fundamental data for its utilization. The potential use of the unused energy is a1so discussed.

• 한국농공학회논문집
• /
• 제54권1호
• /
• pp.93-97
• /
• 2012

Agricultural water reservoirs upstream of the intake on the basis of the intaking water volume is being made. Therefore, the supply capacity of reservoirs are not considered when the water balance analysis, storm water reservoirs are based on agriculture and further secured by the reservoir water is not used to using natural river water analysis. To overcome these problems can supply reservoirs are available to permit analysis of how much the quantity of water balance analysis, it should be reflected in the line to help. In this study, the natural daily flow data and apply the dimensions of the reservoir, and for more than 30 years of the long-term water balance analysis conducted by Date Youngsan river basin can supply reservoirs are large quantity of permits available is presented.

• 산업기술연구
• /
• 제35권
• /
• pp.55-58
• /
• 2015

Natural shifting of rivers has been disturbed by anthropological activities. Urbanization in Kathmandu has been encroached the natural floodplain of Bagmati and currently channeled by training walls. The study compares the change in shape of Dhobikhola, a small tributary using 1966 and 2014 satellite images. It has been found that the original shape is heavily changed over time at the beginning and end section of river under study. The river width is now fixed by training walls and roads along the banks. Using multiple data sets like satellite images and GIS analysis, these shifts can be easily detected to plan for management and restoration of physical and ecological behaviors of rivers.

• 한국습지학회지
• /
• 제9권3호
• /
• pp.51-61
• /
• 2007

자연하천은 하천개수사업, 유역의 토지이용 변화, 댐 및 저수지 건설, 골재채취 등 여러 가지 요인에 의해 하상이 변동하게 된다. 이러한 하상변동은 하천정비 및 다양한 습지계획, 안정하도 유지관리를 위해 매우 중요한 사항이다. 본 연구에서는 골재채취로 인해 저하된 하상이 점차 안정화 되어가고 있는 금강 및 미호천 국가하천 구간을 대상으로 하천측량, 하상재료 채취 분석을 실시하고, 이를 토대로 하도 형성을 지배하는 하도특성량 분석과 수치모형에 의해 장래 하상변동을 예측하였다. 연구결과 하상경사 및 마찰속도 등 하도특성량을 통해 분석한 하상변동 잠재성 평가 결과와 수치모형을 이용한 하상변동 예측결과가 비슷한 경향을 나타냈으며, 금강 및 미호천은 장래 하도가 안정화될 것으로 분석되었다. 이와 같이 장래 하상의 세굴 또는 퇴적경향 등을 예측하고 그 특성을 반영하면, 치수적인 대책 수립과 수리적으로 안전한 구간에서의 식생호안 설치 등 치수적으로 안전하고 친환경적인 하천 및 습지계획이 가능할 것이다.

• 환경영향평가
• /
• 제12권4호
• /
• pp.259-270
• /
• 2003

To investigate the water quality and the pollution state of lower Yeongsan river system, 38 water samples were taken from the main stream of the Yeongsan river, Gomakwon and Hampyeong streams of the system in dry and flood seasons, May and August, 2001. The Yeongsan river is typically natural in accordance with pH-& diagram. But the chemistry based on Piper's diagram indicates that the river is influenced by seawater. BOD increases as the sampling sites are approaching the downstream in Gomakwon and Hampyeong streams overwhelming WQS V grade of 12.40mg/l. T-N and T-P of the river are mainly loaded not in above branch streams but in the main stream of the river, which are caused by manure for farming, domestic animal discharges and life-sewage, in possible. Meanwhile, heavy metal contents are below WQS or not detect in whole water samples. So, it shows that the above river waters be polluted by not industrial but life/agricultural foul waters.

• 한국습지학회지
• /
• 제5권1호
• /
• pp.53-66
• /
• 2003

The subject of sediment transport has been studied for centuries by engineers and river morpohologists. Many of the complex aspects of sediment transport are yet to be understood, and remain among the challenging subject for future studies. In this study, the finite element model is applied to various hypothetical channels. On the basis of the flow analysis results, sediment transport analysis is conducted using 3-different optional equations, and the results are compared with experimental results. For the purpose of predicting the sediment movements in natural river, RMA model is applied to Geum-River. It turned out to be very effective tool to predict various aspects of river evolution and the effects of hydraulic structures. The simulation results are also linked to the Geographic Information Systems (GIS).

• 환경영향평가
• /
• 제4권1호
• /
• pp.65-78
• /
• 1995

The resident attitude for preservation and development of amenity in Eulsuk island and its downstream area at estuary of Nakdong river in Korea were investigated by the questionnaires and the field surveys. Based on the results, the characteristics of this study area are the natural ecological preservation area, natural environmental preservation area and curtural assets for migratory birds. And there are a estuary bank, a Dadae beach and a Molundae park. Special amenities are (1) the light (sunrise, sunset etc), (2) the water(river, sea etc.), (3) the air(fresh wind, beautiful sound etc.), (4) the land space(beautiful view, recreation field, reed area, pine forest etc.) and (5) the stream(dancing of migratory birds, water flow, folk dance, history remains etc.). But at present, the environmental qualities as health, aesthetics safety, amenity and culture are deteriorated by development. So the number of migratory birds are decreasing. The residents desired that in future this area be use for the recreation space, the park and the natural leaning fields etc, as well as the restoration of destroyed resources.