• Title/Summary/Keyword: Sediment Yield

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A Correlation of reservoir Sedimentation and Watershed factors (저수지 퇴사량과 유역인자와의 상관)

  • 안상진;이종형
    • Water for future
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    • v.17 no.2
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    • pp.107-112
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    • 1984
  • It si presented here that in order to estimate reservoir sedimentation rate through the use of reservoir survey data of 66 irrigation reservoir in 3 major watersheds in this country, the correlation between reservoir sedimentation rate and the following factors; watershed area, trap-efficiency, watershed slope, shape factor of water shed, and reservoir deposition age in two models simple regression model and multiple regression model. Appropriatness of the proposed models have been calibrated from the survey data and as a result, it has been determined that the multiple regression model is much more accurate than the simple regression model. The annual sediment yield is correlated with watershed area and reservoir trap efficiency. It has been found that variation of the annual average sedimentation rate and the annual reservoir capacity loss rate are influenced by the trap efficiency of reservoir.

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Estimation of Sediment Yield in the Naesung-cheon with SWAT Model (SWAT 모형에 의한 내성천의 비유사량 추정)

  • Kim, Dae-Gon;Yang, Moon-Yong;Ha, Sung-Won;Yu, Kwon-Kyu
    • Proceedings of the Korea Water Resources Association Conference
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    • 2010.05a
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    • pp.1734-1738
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    • 2010
  • 최근 이상 기후에 따른 유역 환경의 변화가 크게 눈에 띄고 있다. 또한, 댐건설이나 하도 준설 등 인위적인 요인에 의해 유역 및 하천의 유사 거동이 크게 변화하고 있다. 그러나, 하도 관리의 기본 자료인 하천 유역의 유사 발생량에 대해서는 체계적인 연구가 부족한 실정이다. 본 연구는 분포형 수문 모형을 이용하여 체계적이고 합리적으로 비유사량을 산정하기 위한 연구이다. 대상 유역으로는 낙동강 주요 지류 중 하나이며, 영주댐이 건설될 계획인 내성천으로 선정하였으며, 이용하는 모형은 대상유역의 토양 특성, 토지이용과 관리 상태를 고려하는 SWAT(Soil and Water Assessment Tool) 모형을 선정하였다. 먼저, GIS와 연계된 SWAT 모형을 적용하기 위하여 수치 고도자료, 토양도와 토지이용도를 구축하고, 내성천 유역의 기상 및 우량 관측소를 고려하여 일강수자료, 일 최대/최소 기온을 포함한 기후자료를 입력하였다. 그리고, 대상 유역에 위치한 수문관측소와 수질 관측소를 고려하여 소유역으로 세분화한 후 토양특성과 토지이용에 따른 모의를 실시하였다. SWAT 모형을 이용한 비유사량 산정에서 문제가 되는 것은 식생 피복 상태와 토양 침식성 인자인 것으로 나타났다. 또한, 산정된 비유사량은 내성천의 하천 유사량 측정 자료에서 산정한 비유사량과 비교하였다. 그 결과 SWAT 모형은 유사량 실측 자료에서 산정된 비유사량보다 상당히 큰 값을 산정하였다. 그러나, 보다 체계적인 입력 자료가 축적된다면, SWAT 모형을 이용하여 합리적인 비유사량 산정이 가능할 것으로 보인다.

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Estimation of Sediment Yield to Sangju-Dam of Nakdong-River Using the RUSLE Model (RUSLE모형을 이용한 낙동강 상주보까지의 토사유출량 산정)

  • Kim, Jong-Hee
    • Proceedings of the Korea Water Resources Association Conference
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    • 2012.05a
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    • pp.495-499
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    • 2012
  • 토사유출량이란 강우가 발생한 지점에서 토양침식에 의해 생산된 토사가 퇴적 및 이송 등의 과정을 거쳐 유역의 특정 지점까지 도달한 토사량을 의미한다. 토사유출량을 정확하게 산정하는 방법은 현재까지 없다. 그러나 유역단위의 대략적인 토사유출량 산정을 위해서는 경험적 모형인 USLE 모형과 수정된 형태의 RUSLE 모형 또는 MUSLE 모형이 보편적으로 사용되고 있다. 최근에는 지형정보시스템(GIS)의 발달로 RUSLE 모형과 MUSLE 모형이 주로 사용되는데 연평균 토사량 산정에는 RUSLE 모형이 사용되며 단일호우에 대한 토사량은 MUSLE 모형이 사용된다. 그러나 이 모형들은 구곡 및 하천에서의 수리학적 특성 반영하기 힘든 단점이 있어서 유출지점에 따라 유사전달률(SDR)의 개념이 요구된다. RUSLE 모형과 MUSLE 모형에 사용되는 유사전달률은 외국에서의 경험적 공식으로서 우리나라 유역 실정을 제대로 반영하지 못하는 단점이 있다. 그러므로 추후 연구에는 8~10년 이상의 토사유출량 자료를 바탕으로 그 유역의 유사전달률을 결정하고, 그 결과 값을 이용하여 단일호우 사상의 유출량과 모의유출량을 비교하여 MUSLE 모형의 강우인자인 R값을 산정해야 할 것으로 판단된다. 그 선행 작업으로, 본 연구에서는 RUSLE 모형과 기존의 유사전달률을 사용하여 낙동강 상주보까지의 토사유출량을 산정하였다. 상주보유역은 안동댐유역, 임하댐유역, 안동댐하류유역, 내성천유역, 영강유역으로 구성되며 안동댐유역과 임하댐유역은 댐의 차단으로 본 연구의 토사유출량 산정에서 제외하였다.

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Flow Properties of Gelatinized Cowpea Flour Dispersion (동부 앙금 호화액의 흐름 성질)

  • 이애랑;김성곤;이신영
    • Journal of the Korean Society of Food Science and Nutrition
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    • v.22 no.2
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    • pp.181-185
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    • 1993
  • The effects of concentrations (6~9%), heating temperatures (80, 85, 90 and 95$^{\circ}C$) and heating methods (continuous, method A and instantaneous, method B) on the flow properties of cowpea flour (air-dried sediment) at 6$0^{\circ}C$ were studied. The gelatinized cowpea flour dispersions by method B had higher values of yield stress and consistency index but lower value of flow behavior index compared to those values of method A. The log values of consistency index were positively correlated with the concentration and heating temperature for both methods. The rate of increase in the consistency index value by method B at the same concentration was greater in all heating temperatures than that by method A.

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Groundwater of bed rocks in South Korean Penninsula (한반도의 암반 지하수에 관한 연구)

  • 한정상
    • Water for future
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    • v.14 no.4
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    • pp.73-81
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    • 1981
  • More than 650 numbers of water well ranging in depth from 100M to 200M were installed in South Korean Penninsula during the last decade for the purpose of industrial use and municipal water supply. Those data were compiled and synthesized by writer to determine their hydrogeologic occurences in accordance with their geologic and areal characteristics. Rocks yielding the deep seated ground water beared in the geologic primary and secondary porosities are classified into 6 groups according to their geologic, hydrogeologic, and topographic characteristics, that are: volcanic, sedimentary, meta-sediment and/or schist, andesitic, gneissic, and granitic rocks. The order of ground water productivity of the groups is as written above. Even granitic rocks including porphyries, granite, and intermediate and basic plutonic rocks is considered to be the most poorest ground water yielding group among 6, it's average yield form a single well with average drilling depth of 116M is about 225 cubic meters per day if it's drilling site is properly located. Generally speaking, seizable geologic structures such as fractured, sheared, and faulted zone at the flat surface and valley center yield almost 310% more of deep seated bet rock ground water in comparision with minor structures of joints, bedding planes, and so on that are occured at high land. 50 numbers of water well drilled at crystalline rocks were specially checked and measured it's ground water yie 1ds at each drilled depth to determine each interval's productivity while hammer drilling was going on. The results indicate that the specific capacity and yield of each water well at a depth below 70M to 80M was almost neglegible. It means that optimum well depth of crystalline rocks, except the area having seizable geologic structures, shall be not deeper than 80M.

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Soil Erosion and Sediment Yield Reduction Analysis with Land Use Conversion from Illegal Agricultural Cultivation to Forest in Jawoon-ri, Gangwon using the SATEEC ArcView GIS (SATEEC ArcView GIS를 이용한 홍천군 자운리 유역 임의 경작지의 산림 환원에 따른 토양유실 및 유사저감 분석)

  • Jang, Won-Seok;Park, Youn-Shik;Kim, Jong-Gun;Kim, Ik-Jae;Mun, Yu-Ri;Jun, Man-Sig;Lim, Kyoung-Jae
    • Journal of Environmental Policy
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    • v.8 no.1
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    • pp.73-95
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    • 2009
  • The fact that soil loss causing to increase muddy water and devastate an ecosystem has been appearing upon a hot social and environmental issues which should be solved. Soil losses are occurring in most agricultural areas with rainfall-induced runoff. It makes hydraulic structure unstable, causing environmental and economical problems because muddy water destroys ecosystem and causes intake water deterioration. One of three severe muddy water source areas in Soyanggang-dam watershed is Jawoon-ri region, located in Hongcheon county. In this area, many cash-crops are planted at illegally cultivated agricultural fields, which were virgin forest areas. The purpose of this study is to estimate soil loss with current land uses(including illegal cash-crop cultivation) and soil loss reduction with land use conversion from illegal cultivation back to forest. In this study, the Sediment Assessment Tool for Effective Erosion Control(SATEEC) ArcView GIS was utilized to assess soil erosion. If the illegally cultivated agricultural areas are converted back to forest, it would be expected to 17.42% reduction in soil loss. At the Jawoon-ri region, illegally cultivated agricultural areas located at over 30% and 15% slopes take 47.48 ha(30.83%) and 103.64 ha(67.29%) of illegally cultivated agricultural fields respectively. If all illegally cultivated agricultural fields are converted back to forest, it would be expected that 17.41% of soil erosion and sediment reduction, 10.86% reduction with forest conversion from 30% sloping illegally agricultural fields, and 16.15% reduction with forest conversion from 15% sloping illegally agricultural fields. Therefore, illegally cultivated agricultural fields located at these sloping areas need to be first converted back to forest to maximize reductions in soil loss reduction and muddy water outflow from the Jawoon-ri regions.

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FARMING DENSITY OF OYSTER IN HANSAN-GEOJE BAY (한산${\cdot}$거제만 굴 양식장의 양식밀도에 관한 연구)

  • CHO Chang Hwan
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.13 no.2
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    • pp.45-56
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    • 1980
  • Farming density of oyster cultured in Hansan-Geoje Bay was studied to obtain the optimal farming density based on the biosedimentation analysis and the annual yield data from 1970 to 1979. Farming density of oyster extrapolated by means of pollution grade of sediment is significantly correlated to COD and phaeophytin content of the bottom mud of the bay. Pollution grade is linearly related to the number of oyster clusters suspended in the unit area. Optimal farming density was $0.12\;string/m^2$ in case of raft culture, and it was $0.12\;string/m^2$ in case of long-line culture. Farming density was well expressed by the number of strings per raft and the area covered by a raft. As strings per raft increased from 350 to 558, total yield from a raft increased and when occupied sea area per raft ranged from $1.000\;m^2\;to\;6,000\;m^2$, the yield per raft linearly increased as the area increased. This analysis suggests that the optimal density be 0.11 string per unit area $(m^2)$. As increasing the number of strings per $m^2$ the yield per string decreases, and this is well dipicted by a linear function. At this time the yield per unit area increases when the number of string increases up to the density of $0.13\;strings/m^2$. From the point of these three comprehensive analyses the optimal density was $0.11\~0.13\;string/m^2$ in case of raft culture and $0.25\;strings/m^2$ in case of long-line culture in Hansan-Geoje Bay. The maximum expected yield of oyster in Hansan-Geoje Bay is approximately 5,600 tons when maintained the string density at $0.11\~0.13\;string/m^2$.

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Evaluation of Watershed Stability by the Forest Environmental and Stream Morphological Factors (산림환경 및 하천형태인자에 의한 유역안정성 평가)

  • Jung, Won-Ok;Ma, Ho-Seop
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.4 no.4
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    • pp.1-11
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    • 2001
  • This study was carried out to analyze the characteristics of forest environmental and stream morphological factors by using the quantification theory(I) for evaluation of the watershed stability. Present annual mean sediment yield of erosion control dams were investigated in 167 sites of erosion control dam constructed during 1986 to 1999 in Gyeongbuk. The results obtained from this study were summarized as follows; According to the coefficients of partial correlation, each factor affecting to sediment was shown in order of gravel contents, number of first streams order, number of total streams, length of total streams, forest type, length of main stream, parent rock, stand age, soil texture, stream order, slope gradient, soil depth and aspect. Descriptions of class I were as follow; Igneous rock of parent rock, hardwood stands of forest type, less than 20 year of stand age, less than 30cm of soil depth, sandy clay loam of soil texture, more than 41% of gravel contents, south~east of aspect, 2,501~3,500m of length of main stream, 21~25 of number of total streams, 5,501~10,000m of length of total streams, 3 or more than 4 of stream order, more than 16 of number of first stream orders and more than $31^{\circ}$ of slope gradient. Descriptions of class II were as follow; Metamorphic rock of parent rock, coniferous stands of forest type, more than 25 year of stand age, 31~40cm of soil depth, silt loam of soil texture, 11~20% of gravel contents, north~west of aspect, 2,501~3,500m of length of main stream, 16~20 of number of total streams, 3,501~5,500m of length of total streams, 3 of stream order, 11~15 of number of first stream orders and more than $31^{\circ}$ of slope gradient. Descriptions of class III were as follow; Sedimentary rock of parent rock, mixed stands of forest type, more than 25 year of stand age, more than 51cm of soil depth, silty clay loam of soil texture, less than 10% of gravel contents, south~west of aspect, less than 500m of length of main stream, less than 5 of number of total streams, less than 1,000m of length of total streams, less than 1 of stream order, less than 2 of number of first stream orders and less than $25^{\circ}$ of slope gradient. The prediction method of suitable site for erosion control dam divided into class I, II, and III for the convenience of use. The score of class I evaluated as a very unstable area was more than 8.4494. A score of class II was 8.4493 to 6.0452, it was evaluated as a moderate stable area, and class III was less than 6.0541, it was evaluated as a very stable area.

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Suitable Site Assessment using Habitat Suitability Index for Ruditapes philippinarum in Gochang(Hajun) (서식지 적합지수를 이용한 고창 갯벌어장 바지락의 어장적지평가)

  • Jeon, Seungryul;Choi, Yoon-Seok;Cho, Yoon-Sik;Kim, Yeong-Tae;Choi, Yonghyeon
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.21 no.5
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    • pp.484-491
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    • 2015
  • The productivity of Manila clam(Ruditapes philippinarum) aquaculture farm is closely related to suitable site selection, so it is essential to assess the habitat suitable for aquaculture species in order to manage yield. This study evaluated the habitat suitable index(HSI) with 9 sites for tidal flat farm, Gochang(Hajun) on May 2014. The suitability index was selected Growth(hydrodynamics, chlorophyll a), Survival(sediment-sand, silt-clay) and Water Environment(dissolved oxygen, salinity). Both Weight and No weight were tried for objective judgment as HSI scoring method. As a result, it shows lower tidal flat(HSI; No weight: 0.60~0.76, Weight: 0.47~0.70) is higher than upper(HSI; No weight: 0.25~0.27, Weight: 0.09~0.10), hydrodynamics and sediment particle size are the most effective. This research can consider the potential suitable site for Manila clam through scientific approach, and provide the basis for optimal management practices in tidal flat farm.

Development Environment for Open-pit Mine Monitoring System using Geospatial Open Platform and Open Source Software (공간정보오픈플랫폼 및 오픈 소스 기반의 노천광산 모니터링시스템 개발을 위한 환경 조성)

  • Lee, Hyun Jik;Kim, Se Yul;You, Ji Ho
    • Journal of Korean Society for Geospatial Information Science
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    • v.22 no.4
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    • pp.165-173
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    • 2014
  • Open-pit mining method, is safe relatively work as compared with underground mining. And high yield, low production cost, has the advantage that it can provide a lot of production. But deforestation, tailings and slag deposition, mineral debris, dust, water, noise, land subsidence, sediment runoff discharge, I have internalized environmental disaster predisposing factors, such as landslides. Thus, it may be noted, also by typical environmental regulations. We try to deal with the changes in open pit terrain and environment related issues. Then, use the recovery period and the open pit mine and ecology off the gun, environment-friendly development of accurate monitoring methods, systems of this development is required. The use of open platforms and open source GIS tools have been developed during this period, it needs to develop spatial information environment monitoring system open pit mine construction.