• 제목/요약/키워드: water depth change

검색결과 563건 처리시간 0.025초

수공구조물이 하천환경에 미치는 영향에 관한 연구(II) : 수질 및 생태학적특성 (A Study on Effects of Hydraulic Structure on River Environment(II) : Water Quality and Ecological Characteristics)

  • 안승섭;최윤영;이수식
    • 한국환경과학회지
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    • 제11권4호
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    • pp.309-317
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    • 2002
  • In this study, water protection reservoir is selected as the target which is located at the estuary of Taehwa river to analyze and examine the effects of hydraulic structure on river environment. This study examined the water quality variation characteristics among many effects of hydraulic structure on river environment before and after removal of the sediment protection reservoir when low flow is yielded. This study aims at the definition of factors which cause the change of ecological environment of river due to the effects of the sediment protection reservoir, and the proposal of the direction of environmental friendly river space development through the comparison of stream variation conditions(depth, velocity, and etc.) and riverbed variation characteristics with ecological depth condition of Taehwa-river's channel for each representative species of fish and examination those. Firstly, from the examination result of water quality when low flow is yielded before and after removal of the sediment protection reservoir for problems about water quality of river due to flow amount decrease in river, it is found that DO decreases about 0.78~0.86ppm at the lower stream of Myeongchon-gyo, and BOD decreases about 0.06~0.24ppm from right upper stream to the direction of estuary when the sediment protection reservoir is removed. It is known from the above that there is some improvement of water quality from the lower stream of Taehwa-gyo to the estuary in case of removal the sediment protection reservoir. Nextly, it is thought that the effects on ecosystem due to water depth and draw down in channel is not serious on the basis of the examination of water quality analysis result according to removal of sediment protection reservoir and hydraulic depths for reservation of ecosystem, these are 10~40cm for breeding season, 10~50cm for fry period, and 10~100cm for adult period of the representative species of fish in Korea.

Analysis on the evolution of water resources situation in Qiandao Lake Basin from 1960 to 2020

  • DU Junkai;Qiu Yaqin
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2023년도 학술발표회
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    • pp.27-27
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    • 2023
  • To analyze the evolution of water resources in Qiandao Lake Basin under the condition of climate change, a WEP-L distributed hydrological model was established to simulate the water cycle process in the basin during 1960-2020. The Mann-Kendall non-parametric test method and Hurst index method were used to analyze the inter-annual variation and annual distribution characteristics of the total water resources in the basin. The multi-scale temporal and spatial distribution and evolution trend of water resources in Qiandao Lake Basin were evaluated. The results show that: (1) The WEP-L model has good simulation results in the Qiandao Lake basin, and the Nash coefficient rate is above 0.83 in the periodic period and above 0.85 in the verification period. (2) The water yield coefficient of the whole basin ranges from 0.436 to 0.630. The annual average total water resource is 12.25 billion m3, equivalent to 1176.4mm of water depth. The annual distribution process shows a unimodal structure, and the water depth of each sub-basin ranges from 742 mm to 1266 mm, and the spatial distribution is higher in the west and lower in the east. (3) The annual water resources series in the basin showed an insignificant upward trend, and the Hurst index was 0.86, indicating a continuous upward trend. From the perspective of monthly water resources, January and February increased significantly, the other months were not significant changes.

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The Relationship Between the Water Color and the Transparency in the Seas Around Korea

  • Hahn, Sangbok
    • 한국해양학회지
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    • 제3권2호
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    • pp.55-62
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    • 1968
  • The distributions of average water color and the transparency in the seas around Korea show two patterns: the one is the East Sea and the South Ses, the other is the Yellow Sea. In the East Sea and the South Sea, the water colors C$\sub$E/ in Forel scales change from green to greenish blue with distance x in miles from the seashore, an average color is bluish green, 3.7 in Forel scales, and the relationship is given by C$\sub$E/ = 5e$\^$-0.056.root.x; an average transparency is 15m and the transparency T$\sub$E/ shows following formula with distance x, E$\sub$E/=0.9.root.x+10. In the Yellow Sea, the water color C$\sub$Y/ changes from green yellow to bluish green with distance, an average color is light green, 5.6 in Forel scales, and the relationship is given by C$\sub$Y/= 8.5e$\^$-0.086.root.x; an average transparency is 7m, the farther it is from the seashore, the deeper transparency T$\sub$Y/ is as following, T$\sub$Y/=1.2 .root.x+1. Along the seashore, the transparency T$\sub$Y/ is only 10% that of the East Sea and the South Sea. The distributions of the water color and the transparency by depth change in values within the continental shelf. The water color in Forel scales decreases with the distance from the seashore and depth; the transparency increases with the distance and depth. They are caused by suspended particles, especially suspended clay, and it is the major factor in the change in color and transparency, particularly in the Yellow Sea. In September, the sea water is the clearest in the seas around Korea, transparency shows the maximum and water color the minimum in forel scales. The water color shows green yellow when transparency is 1m, green at 10m, and greenish blue at 20m. the relationship between the water color and the transparency shows an exponential distribution as following, C=9e$\^$-kT/, k=0.0625m$\^$-1/. This formula agrees with calculated formulas between the water color and the transparency from the emprircal formulas C$\sub$E/ and T$\sub$E/, C$\sub$Y/ and T$\sub$Y.

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철근콘크리트 내부 온습도 경시변화 추정 모델 구축 (Prediction Model for the Change of Temperature and R.H. inside Reinforced Concrete)

  • 박동천
    • 한국건축시공학회:학술대회논문집
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    • 한국건축시공학회 2016년도 추계 학술논문 발표대회
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    • pp.83-84
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    • 2016
  • Surplus water inside a concrete other than moisture that is used for hydration of the cement affects the physical properties of the concrete (modulus of elasticity, compressive strength, drying shrinkage, and creep) by drying. Changes in temperature and humidity inside a concrete has correlation with the movement speed and reaction rate of deterioration factors such as carbon dioxide and chloride ions. In this study, comparison was performed between temperature and relative humidity inside the concrete and meteorological data for exposure environment through measurement at the site for two years. Surface temperature of the concrete (depth 1cm) was measured higher by 6℃ during the summers, while it was measured lower by 2℃ during the winters due to solar radiation, wind, and radiation cooling. As for relative humidity, change was large in the depth of 1cm, while more than 85% was maintained in the depth of 10cm.

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CSA를 혼입한 폴리머 시멘트 모르타르의 성능평가 (Evaluation of Properties of Polymer-Modified Mortar with CSA)

  • 주명기;노병철
    • 한국구조물진단유지관리공학회 논문집
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    • 제19권1호
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    • pp.35-44
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    • 2015
  • 본 연구에서는 CSA를 혼입한 폴리머 시멘트 모르타르의 강도, 흡수율, 염화 이온 침투 깊이, 중성화 깊이, 길이변화 및 내약품성에 미치는 영향에 대하여 실험적으로 구명하였다. 그 결과, CSA를 혼입한 폴리머 시멘트 모르타르의 압축, 휨, 인장 및 부착강도는 CSA 첨가량 및 폴리머-시멘트비가 증가함에 따라 증가하였다. 흡수율은 CSA 첨가량 및 폴리머-시멘트비가 증가함에 따라 감소하였다. 길이변화는 CSA 첨가량 및 폴리머-시멘트비가 증가함에 따라 감소하였다. 염화 이온 침투깊이 및 중성화 깊이는 CSA 첨가량 및 폴리머-시멘트비가 증가함에 따라 감소하였다. 또한, 내약품성은 CSA 첨가량 및 폴리머-시멘트비가 증가함에 따라 감소하였다. 이와 같은 강도 및 내구성 개선은 EVA 폴리머의 높은 인장강도에 기인하며, EVA 폴리머 및 CSA 혼입에 의하여 시멘트 수화물과 골재사이의 부착력이 개선되기 때문이라 판단된다.

부산지역 해양레저관광 참여자의 만족 및 불만족에 관한 질적 연구 (Qualitative Study on the Satisfaction and Dissatisfaction of Water Leisure Tourism Participants in Busan Area)

  • 김영준;홍상민
    • 수산해양교육연구
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    • 제28권4호
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    • pp.1171-1181
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    • 2016
  • The purpose of this study was to verify the formation of satisfaction and dissatisfaction of water leisure tourism participants in Busan area using qualitative study method approach. Research participants were selected 6 water leisure tourism participants by reputational sampling method. Six participants who usually participated in water leisure tourism were selected as research participants. The data for this study included participants' observation and in-depth interview. This study categorized the coding paradigm which was presented by using the findings derived from water leisure tourism background. The results based on in-depth interview were as follows. First, water leisure tourism participants recognized environmental satisfaction of environmentally safe pleasure. Second, water leisure tourism participants recognized social satisfaction of change for leisure recognition. Third, water leisure tourism participants recognized facilities and program satisfaction of clearness and systematic programs. Fourth, water leisure tourism participants recognized instructor satisfaction of kindness and professional. Fifth, water leisure tourism participants recognized safety dissatisfaction of safety ignorance. Sixth, water leisure tourism participants recognized amenities dissatisfaction of lacking convenience. Seventh, water leisure tourism participants recognized accessibility dissatisfaction of public transportations.

지구온난화에 따른 홍수 및 가뭄 발생빈도의 변화와 관련하여 : 1. 연/월강수량의 변화에 따른 일강수량 분포의 변화분석 (On the Change of Flood and Drought Occurrence Frequency due to Global Warming : 1. Change of Daily Rainfall Depth Distribution due to Different Monthly/Yearly Rainfall Depth)

  • 윤용남;유천상;이재수;안재현
    • 한국수자원학회논문집
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    • 제32권6호
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    • pp.617-625
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    • 1999
  • 지구 온난화는 산업혁명이후 이미 시작되었으며 최근에 와서 그 정도가 심해지고 있다. CO2와 같은 온실기체의 증가를 가장 큰 원인으로 하는 지구 온난화의 영향이 아직 정량적으로 밝혀지고 있지만 대기순환모형(General Circulation Model: GCM)을 이용한 연구에서 이러한 온실기체의 증가가 지구의 평균온도를 상승시킨다고 밝히고 있다. 지구 온난화는 전지구적 물의 순환에도 영향을 미쳐 지구 곳곳의 강수패턴에 변화를 가져오는데 근래에 자주 발생하는 대규모 가뭄이나 홍수화 같은 극치기상이 이러한 지구온난화의 간접증거로 자주 언급되곤 한다. 국내의 경우도 예외는 아니어서 근래에 들어 빈번한 홍수 및 가뭄을 경험하고 있다. 본 연구에서는 지구온난화에 따른 홍수 및 가뭄의 빈도변화 분석을 목적으로 한다. 이러한 연구목적을 달성하기 위해 먼저 현재상태가 지구온난화 과정의 한 시점이라는 가정 아래 현재까지 관측된 일강수량 자료를 분석하여 과거 연강수량의 증가가 일강수량의 분포에 어떤 식으로 영향을 미치고 있는지를 분석하여 보았다. 대상자료는 금강유역의 17개 지점을 선정하여 이용하였고, 분석결과로서 연강수량과 무강수일수는 상대적으로 작은 상관을 보이고 있음을 밝힐 수 있었으며 오히려 10mm이하 또는 50mm이상의 강수일수에 0.8-0.9의 높은 상관을 보임을 파악할 수 있었다.

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기후변화에 따른 도시침수가 도시교통네트워크에 미치는 영향 예측 기술 개발 (Development of technology to predict the impact of urban inundation due to climate change on urban transportation networks)

  • 정세진;허다솜;김병식
    • 한국수자원학회논문집
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    • 제55권12호
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    • pp.1091-1104
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    • 2022
  • 기후변화는 전 세계적으로 강우의 빈도와 강도를 증가 시킬 것으로 예측되며 급격한 도시화와 산업화로 인해 도시 지역의 내수 침수 피해로 양상이 바뀌고 있다. 이에 기후변화에 따른 영향평가는 도시계획에 매우 중요한 요소로 언급되고 있으며, 세계기상기구(WMO)는 기상 현상으로부터 발생할 수 있는 사회, 경제적 영향을 고려하는 영향예보의 필요성을 강조하고 있다. 특히 교통에 있어서 도시침수로 인한 교통 시스템의 성능 저하는 사회에 가장 해로운 요소이며 영향을 받는 주요 도로마다 시간당 £ 100k 정도인 것으로 추정하고 있다. 그러나 국내의 경우 현재 기상재해의 발생에 대한 정확한 예보 및 특보를 제공해도 그 영향을 제대로 전달하지 못하고 있다. 따라서 본 연구에서는 도시홍수의 침수심을 제시하고 차량에 영향을 미칠 수 있는 피해에 대처하기 위해 각 지역의 고해상도 분석 및 수문학적 요인을 반영하고, 강우로 인한 홍수 정도와 차량 운행에 미치는 영향 정도를 조사할 필요가 있다고 판단하였다. 이에 강우-침수심-차량속도의 산정식을 간단한 선형회귀식이 아닌 다양한 머신러닝 기법을 이용하여 제시하고자 한다. 또한 또한 기후변화 시나리오를 강우-침수심-차량속도 산정식에 적용하여 집중호우 시 도시하천의 침수를 예측하고 미래 기후변화의 영향을 고려한 도로 침수로 인해 발생할 수 있는 교통 네트워크의 장애를 평가하며, 도시 교통흐름 계획에 이용하는 기술을 개발하고자 한다.

원격 로봇선에 의한 운항속도에 따른 수심측량의 정확도 분석 (Accuracy Analysis of Sounding Data Caused by Speed of Robot-ship)

  • 최병길;박홍기;조광희
    • 대한공간정보학회지
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    • 제15권4호
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    • pp.111-116
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    • 2007
  • 본 연구의 목적은 DGPS와 음향측심기를 장착한 소형의 로봇선을 이용하여 저수지의 수심정보를 획득하고 이를 이용하여 정확도를 분석하는데 있다. 즉 로봇선의 속도를 변화시키고 이에 따른 속도별 수심측정의 정확도를 분석하였다. 현장실험 결과, 로봇선의 속도가 느릴수록 수심측정의 오차가 적었으며, 로봇선의 속도가 5km/hr까지는 정규분포의 신뢰구간인 95% 이내에 포함되는 것을 알 수 있었다.

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m-Aramid Films in Diverse Coagulants

  • Kim, Ji-Young;Jung, Ji-Won;Kim, Sam-Soo;Lee, Jae-Woong
    • 한국염색가공학회지
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    • 제21권4호
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    • pp.63-67
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    • 2009
  • m-Aramid dissolved in N,N-dimethylacetamide (DMAc), were coagulated in different coagulants such as water, methanol, ethanol, propanol and butanol. Various concentrations and temperatures of the coagulants were also used to evaluate dyeing properties of coagulated m-aramid films. Field emission scanning electron microscopy (FE-SEM) was employed to investigate the surface morphology of m-aramid films. Wide angle X-ray diffraction (WAXD) was conducted in order to measure crystallinity change of mcaramid fibers and films. WAXD patterns showed that crystallinity of m-aramid fibers was reduced after film formation. In addition, color depth (K/S value) was measured and the results revealed that the film coagulated in water possessed fairly enhanced color depth.