• 한국공작기계학회논문집
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• 제11권5호
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• pp.88-92
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• 2002

This research is about slurry wear of SM45C and SUS304, which using standard sand and KUM river sand. The results are as follows ; 1. Mass loss rates of both standard sand and KUM river sand were linearly increased as increasement of time and velocity. 2. The average diameter of sand from relatively, less wear rate and portion of larger particles. 3. Wear resistance was linear with time and velocity of liquid jet regardless of type of sand. Also, it was able to evaluate with the formula, $HV^2$/E calibrated with n, the velocity index. 4. The wear surface in liquid jet experiment was smooth. The maximum wear depth was observed at the location 2~4mm apart from the center in the condition of $90^{\circ}$ of collision angle 6mm of nozzle diameter, and 20mm of collision distance. The sectional shape in radial appeared as 'W'shape.

• 한국시스템다이내믹스연구
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• 제12권1호
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• pp.59-74
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• 2011

This article deals with an economic evalutation of the 'Pasture Project of Kum River', which is the farming plan of mitten crabs in a stream of it. An augmented model of social capital is based on the past ecological-economic system dynamics model and elaborated further with suggestions of social capital literature. During the modeling process a chain diagram of causal relations and its relevant mathematical equations are presented for simulating the project performance, and the simulation results are provided to contrast the dynamic behaviors of the former ecological-economic model with ones of the new model incorporating social capital. The results indicate that an increase in the economic benefit of the project could happen in case of considering the process of social capital accumulation around the case area, which can be regarded as a remarkable trial to approve the common confidence in the role of social capital to enhance an economic achievement.

• 한국환경보건학회지
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• 제18권1호
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• pp.69-75
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• 1992

Authors investigated the heavy metals in water, soil, rice and Urine of residents along the KUM river. Sample were analyzed by Varian Atomic absorption Spectrophotometer. The results obtained were as follows. 1. The Contents of cadmium and Lead in water were in the range of 0~2.15$\mu$g/l, 0~4.29$\mu$g/l, respectively. 2. The Contents of heavy metals in soil were in the range of 0.32~0.91mg/kg, 5.59~21.55mg/kg for Cd, Pb respectively. 3. Those in rice were in the range of 0.025~0.062mg/kg for Cd, Pb respectively. 4. The mean of Lead and Cadmium Concentration in Urine of residents of Munju Ri were 28.63$\mu$g/l and 1.66$\mu$g/l respectively, Those was also the highest level among the investigated group.

• 한국동물학회지
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• 제30권4호
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• pp.379-386
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• 1987

Karyotype of the ricessh Orygias latipes (Temminck et Schlegel) was investigated using 151 specimens of eleven populations in the southern Korea. Based on the karyotype analysis, two distinct chromosomal groups were found. One group, occurring in the Kum River, the Mankyong River, the Dongjin River, the Ysngsan River and the SEmjin River had a diploid chromosome number of 46 and arm number of 70, which contained one pair of "large" metacentric chromosomes. The other group, occurring in the Tamjin River, the Hyongsan River andthe all four island populations observed had a diploid chromosome number of 48 and arm number of 68. These results showed that 0. latipes of 6 inland populations was identical with the Chinese population in diploid number, arm number and presence of "large" metacentric chromosome, while the present species of island populations ana populations of the Tamjn R. and Hyongsan R. was similar to the Japanese population in chromosome number and arm number. The karyotype variation in populations indicated that karyotypes will probably provide useful information in studying zoogeography of this species.phy of this species.

• 생태와환경
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• 제33권1호통권89호
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• pp.51-60
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• 2000

금강 중${\cdot}$하류의 본류와 지류에서 수질오염의 특성과 변동양상을 파악하기 위하여 1998년 3월부터 1999년 6월까지 총 8회 조사하였다. 환경요인 중 질소, 인 및 chl-a의 변동이 다른 요인에 비해 증감양상이 뚜렷하였고 특히 무기 N${\cdot}$P의 영향은 지류 중 갑천, 미호천 및 석성천이 가장 큰 것으로 관찰되었다. 수질은 수문요인과도 관련성이 높아 평수량이하의 유량이 장기화되거나 비교적 유량이 적은 저수기${\sim}$갈수기에 급격하게 악화되었고 계절적으로 12월${\sim}$3월에 현저하였다. 중${\cdot}$하류에서 $NH_{4}$와 SRP는 하류로 유하하면서 급격하게 감소(1,476${\to}$577 ${\mu}g$ N/l, 117${\to}$11 ${\mu}g$ P/l)하였고 chl-a는 지수적으로 증가(9.0${\to}$64.4 ${\mu}g/l$하는 경향이 뚜렷하였다. 반면에 $NO_{3}$와 $BOD_{5}$는 정점간에 큰 차이가 없었고 일정하였다. 식물플랑크톤의 생장에 대한 제한영양염은 N${\cdot}$P 농도의 변화 뿐만 아니라 TN/TP 또는 DIN/SRP비가 본류에서 각각 42와 544로서 비교적 높아 N보다는 P가 제한인자로 볼 수 있었다. 유기물의 간접적인 지표인 $BOD_{5}$ 평가에서 본류 및 지류가 III급수로 판정되었으나 특히 갑천의 경우는 V급수 이상이었다. 그 외 chl-a, 투명도, TN 및 TP로서 수질을 평가한 결과 전반적으로 부영양 수준을 초과한 것으로 나타났다. 금강 중 중${\cdot}$하류에서 수질오염의 전개양상은 갑천과 미호천을 포함한 지류로부터 높은 N${\cdot}$P 영양염의 유입 영향이 주된 요인으로 볼 수 있었고 반면에 하류에는 만성적인 식물플랑크톤의 번무가 관찰되어 이에 대한 주요 오염원의 수질관리가 시급하였다.

• 물과 미래
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• 제29권5호
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• pp.185-202
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• 1996

개발된 하천유지유량 결정 방법을 금강유역 본류 구간(대청댐 조정지에서 강경까지)에 적용하여 항목별 필요유량, 그리고 5개구간 및 대표지점에 대한 하천유지유량과 하천관리유량을 산정하였다. 갈수량은 평균갈수량을 대상으로, QUAL2E 모형을 사용하여 환경기초사설 완비여부에 따라 수질을 예측하고, 어류는 금강유역의 9개 대표어종에 대해 필요유량을 산정 하였다. 그리고 하천경관은 공주와 부여 지점에 대해, 수운은 자연 하도 방식, 물놀이는 현재와 장래에 이루어질 여가활동을 대상으로 평가하였으나, 기타 항목은 평가하지 않았다. 대체적으로 자연상태를 유지하고 있는 상류 구간은 생태계 보전 등과 같은 하천의 자연적 기능에 필요한 유량이 지배적이고, 하류는 수질 악화에 따른 수질 보전과 수상이용 등과 같은 인위적 기능에 필요한 유량이 지배적인 것으로 나타났다. 특히 목표 년도에 따라 수질보전에 대한 필요유량은 환경기초시설 완비 여부에 따라 하천유지유량과 하천관리유량이 큰 차이를 보여 하수처리에 의한 수질보전이 시급한 것으로 나타났다.

• 물과 미래
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• 제18권1호
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• pp.67-73
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• 1985

금강 감조구간의 조석전파현상을 장파, 중력파공식의 수치적분에 의한 통상적인 방법을 이용하여 조사하였다. 이용된 역학방정식은 비선형항을 포함하여 천해조를 산정할 수 있도록 하였다. 수립된 모델은 평균대, 중, 소조시의 감조구간의 조석전파를 산정하는데 이용되었으며 또한 상류홍수유출과 하구조석의 상호작용에 의한 감조구간의 수립분포를 산정하는데도 초기적용되었다. 이 연구의 목적은 하구의 체절공사가 시작되기 전의 금강감조구간의 조석역학을 조사하는데 있다.

• 기술사
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• 제10권2호
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• pp.13-26
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• 1977

The Kum-Ho river basin is one of the densely populated area having more than 35% of the total population and it was also well irrigated since ealier days in the Nackdong River Basin Most of the easily developed source of surface water are fully utilized, and at this moment the basin is at the stage that no more surface water can be made available under the present rapid development of economic condition. Since surface water supplies from the basin have become more difficult to obtain, the ground water resources must be thoroughly investigated and utilized greatly hereafter. In economic ground of the basin what part could ground water play\ulcorner In what quantities and, for what uses could it be put\ulcorner The answer to these questions can be relatively simple; the ground water resources in the basin can be put at almost any desired use and almost anywhere in the basin. The area of the basin is at about 2088km$^2$ in the middle part of Nackdong River Basin and it is located along the Seoul-Pusan Express Highway. The mean annual rainfall is about 974.7m/m, most of which falls from June to September during the monsoon. Accumulated wet period is appeared approximately after every 8 year's accumulated dry-period with the duration of 5 years. The water bearing formations in the basin include unconsolidated alluvial deposits in Age of Quatenary, saprolite derived from weathered crystalline rocks, Kyongsang sedimentary formations of the period from late Jurassic to Cretaceouse, and igneouse rocks ranging of the Age from Mesozoic to Cenozoic. The most productive ground water reservoir in the basin is calcareouse shale and sandstones of Kyongsan system, which occupies about 66% of the total area.

• 한국동물학회:학술대회논문집
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• 한국동물학회 1996년도 한국생물과학협회 국제학술대회
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• pp.124.1-124
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• 1996

No Abstract, See Full Text

• 한국해양학회지
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• 제17권1호
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• pp.1-11
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• 1982

A study on the community and distribution of phytoplankton of the Kum River Estuary has been done in fall, 1980 and spring, 1981. Ond hundred and one taxa representing 22 families, 41 genera, 107 species, 2 varieties, and 2 forms were identified. The community of the study area composed mainly of diatom species icluding the very small fraction of dinoflagellates, blue-greens and greens. The dominant species were Skeletonema costatum, Paralia sulcata, and Asterionella kariana. The total standing crop of phytoplankton of winter samples was 115,000 cells/1 in average and that of spring samples was, 1,320,333 cells/1 in average. Of the representative members, dominant species above appeared moree than 10% of the total standing crop, Skeletonema costatum being maximized up to 46%. In spring Asterionella japonica, Thalassionema nitzschioides, and Chaetoceros curvistetus appeared 3∼8%, and Thalassiosira excentricus 3% in winter. The distribuion of marine forms showed negative correlation with that of fresh water forms, although the brackish-water forms showed no relationship. This change pattern of marine, brackish and fresh-water forms are discussed with the results of time series analysis. A list of phytoplankton species observed in this study is added.