• 제목/요약/키워드: water level estimation

검색결과 406건 처리시간 0.026초

An Application of the SRTM Dataset in Inland Water Stage Measurement

  • Bhang, Kon Joon;Lee, Jin-Duk
    • 한국콘텐츠학회:학술대회논문집
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    • 한국콘텐츠학회 2014년도 춘계 종합학술대회 논문집
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    • pp.83-84
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    • 2014
  • For hydrologic applications, lake levels is very important. As a first step in developing a remote-sensing based approach, lake stage estimation using remote sensing was proposed with the SRTM data from February 2000, which was providing a one-time snapshot. After several steps using contouring, masking, and CED, it was found that iterative contour fitting to a lake outline provided the outstanding result with the operator's decision. If the lake size is large enough, a constant meter of the difference removal due to bias found by Bhang et al. (2007) might be useful for more accurate estimations for the methods. A lake-level snapshot using SRTM data could provide estimates within 0.5 m level of accuracy for large lakes (> $10km^2$) with contouring. Also, even if the processing algorithm is complex, the accuracy was reliable. Overall, we confirmed that this study would provide useful information to ameliorate the quality of the SAR-derived DEMs specifically for water areas and if more expanded, SAR images can fruit result in water monitoring.

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액체영역제어계통의 제어모델링 및 제어성 평가 (Control Modelling and Controllability Evaluation of Liquid Zone Control System)

  • 이광대;양승옥;오응세
    • 대한전기학회:학술대회논문집
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    • 대한전기학회 2004년도 학술대회 논문집 정보 및 제어부문
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    • pp.641-643
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    • 2004
  • Liquid Zone Control System controls the power of heavy water reactor. Changing the level of each zone compartment regulates one local zone power of 14 zone powers, iud the level is limited less than 90% by the control algorithm to prevent the flood. In recent years, the level and the power was controlled oscillatory in the upper zones. To find out the condition of cycling, the zone control system was modelled with the linear difference equations and identified using parameter estimation. The pole-zero plot showed that the major pole was near the stability boundary, and the system had oscillatory characteristics in nature.

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국가 지하수 관측망의 수위 및 온도 자료를 이용한 함양량 산정

  • 박창희;구민호;이대하;김형수
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2002년도 총회 및 춘계학술발표회
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    • pp.351-356
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    • 2002
  • Groundwater recharge rate was estimated by applying the groundwater level fluctuation method utilizing Theis (1937) approach with specific yield estimation technique of Shevenell (1996) and the temperature method using observed data from National Groundwater Observation Stations. Results based on analysis of water level observation data of 10 alluvium wells reveal that the recharge rates for 5 wells of Kum river area range 3.7~25.0% and those for 5 wells of Nakdong river area range 3.6~21.7%. Results obtained from the temperature method based on water temperature data indicated that the upward flow resulted from evapotranspiration is dominant for 4 wells of the Kum river area and 5 wells of the Nakdong river area. The other wells showed the downward flow which is related to groundwater recharge in these areas.

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간척지 밭작물의 관개용수량 추정을 위한 토양염분예측모형 개발 (Soil Salt Prediction Modeling for the Estimation of Irrigation Water Requirements for Dry Field Crops in Reclaimed Tidelands)

  • 손재권;구자웅;최진규
    • 한국농공학회지
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    • 제36권2호
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    • pp.96-110
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    • 1994
  • The purpose of this study is to develop soil salt prediction model for the estimation of irrigation water requirements for dry field crops in reclaimed tidelands. The simulation model based on water balance equation, salt balance equation, and salt storage equation was developed for daily prediction of sa]t concentration in root zone. The data obtained from field measurement during the growing period of tomato were used to evaluate the applicability of this model. The results of this study are summarized as follows: 1.The optimum irrigation point which maximizes the crop yield in reclaimed tidelands of silt loam soil while maintaining the salt concentration within the tolerance level, ws found to be pF 1.6, and total irrigation requirement after transplanting was 602mm(6.7 mm/day)for tomato. 2.When the irrigation point was pF 1.6, the deviation between predicted and measured salt concentration was less than 4 % at the significance level of 1 7% 3.Since the deviations between predicted and measured values data decrease as the amount of irrigation water increases, the proposed model appear to be more suitable for use in reclaimed tidelands. 4.The amount of irrigation water estimated by the simulation model was 7.2mm/day in the average for cultivating tomato at the optimum irrigation point of pF 1.6.The simulation model proposed in this study can be generalized by applying it to other crops. This, model, also, could be further improved and extended to estimate desalinization effects in reclaimed tidelands by including meteorological effect, capillary phenomenon, and infiltration.

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야간사용량 측정을 통한 배급수구역 배경야간최소유량 산정 (Estimation of background minimum night flows by metering water use in water distribution areas)

  • 이두진;김주환;김도환;김경필
    • 상하수도학회지
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    • 제24권5호
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    • pp.495-508
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    • 2010
  • The aim of this study is to develop a quantified water loss Index to evaluate and manage leakage scientifically for the reduction of non-revenue water in water distribution systems. For the purpose, unavoidable background leakage suggested from UK water industry and IWA, and allowable water leakage in accord with the concept of allowable water loss are proposed by analyzing the inflow into two study water districts and the short-term water use of each customer in the districts. The study distribution areas are selected among the metered districts with good maintenance of leakage after improvement activities in Nonsan, medium sized city in Korea. Estimation models of allowable leakage are developed by metering and analyzing the minimum night flow at residential and commercial areas in the city. In the results of the investigation, it is estimated that background night flow in residential area was larger than that of commercial area where the types of business shows small water use characteristics. Meanwhile, night flow and background water loss on internal plumbing systems show great differences for each district which is influenced much by the water use characteristics and facilities scale. Based on metering water use data in various districts, leakage management criteria can be established under the consideration of domestic conditions in Korea by analyzing separated real water use and background leakage and it is possible to apply into presentation of optimal leakage level and reasonable time for working activities for leakage reduction.

아산호 용수공급용량 유지를 위한 적정 준설량 산정 (Estimation of the Optimal Dredge Amount to Maintain the Water Supply Capacity on Asan-Lake)

  • 장태일;김상민;강문성;박승우
    • 한국농공학회논문집
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    • 제48권2호
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    • pp.45-55
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    • 2006
  • This study analyze the hydrologic conditions and the effects of selected runoff characteristics as an attempt to estimate the optimal dredge amount for Asan Lake in Korea. The runoff feature was calculated by utilizing the water balance simulation from DIROM (Daily Irrigation Reservoir Operation Model), which allowed changes in landuse to be quantified using remote sensing for 14 years. The distribution of prospective sediment deposits was been tallied based on the changes in landuse, and quantity of incoming sediment estimated. From these findings, we were then able to simulate the fluctuation of water level, gauging the pumping days not already in use, to determine the frequency of the distribution for around the. requirement annual water storage and the changing water level. The optimal dredge amount was calculated on the basis of the distribution of frequency, taking into account the design criteria for agricultural water with the 10-year frequency of resistant capacity.

하류 유량자료를 이용한 상류유역의 미계측 유출량 추정 (Estimation of Upstream Ungauged Watershed Streamflow using Downstream Discharge Data)

  • 정영훈;정충길;정성원;박종윤;김성준
    • 한국농공학회논문집
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    • 제54권6호
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    • pp.169-176
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    • 2012
  • This study describes the estimation of upstream ungauged watershed streamflow using downstream discharge data. For downstream Dongchon (DC) and upstream Kumho (KH) water level stations in Kumho river basin ($2,087.9km^2$), three methods of Soil and Water Assessment Tool (SWAT) modeling, drainage-area ratio method and regional regression equation were evaluated. The SWAT was calibrated at DC with the determination coefficient ($R^2$) of 0.70 and validated at KH with $R^2$ of 0.60. The drainage-area ratio method showed $R^2$ of 0.93. For the regional regression, the watershed area, average slope, and stream length were used as variables. Using the derived equation at DC, the KH could estimate the flow with maximum 41.2 % error for the observed streamflow.

일 유출모형의 물수지 분석에 의한 지하수 함양량 추정 (Estimation of Groundwater Recharge by the Water Balance Analysis using DAWAST Model)

  • 이덕주;이호천;이순광;김태철
    • 한국농공학회:학술대회논문집
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    • 한국농공학회 2003년도 학술발표논문집
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    • pp.431-434
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    • 2003
  • This research developed a method for the estimation of groundwater recharge by yielding daily soil moisture content and watershed evapotranspiration from the water balance concept of the unsaturated and saturated layers in rainfall-runoff model called DAWAST. The goal of the research is to estimate the groundwater recharge fulfilling conditions of the safe discharge for any season. To meet this goal, the data of groundwater level and stream flow rate have been monitored in a study area and used to validate the model.

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Ecological Modeling for Estimation of Environmental Characteristics in Masan Bay

  • Kim, Dong-Myung
    • 한국환경과학회지
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    • 제12권8호
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    • pp.841-846
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    • 2003
  • The ecosystem model was applied to estimate the regional distribution of the net production(or consumption) of phytoplankton and the net uptake(or regeneration) rate of nutrients in Masan Bay for scenario analysis to find a proper management plan. At the surface level, net production of phytoplankton is 200 mgC/㎡/day at the entrance of the bay, and 400∼1000 mgC/㎡/day at the center of the bay. The inner area of the bay showed more than 2000 mgC/㎡/day. All areas of the bottom level have a net consumption, with the center of the bottom level showing more than 600 mgC/㎡/day. For dissolved inorganic nitrogen, the results showed a net uptake rate of 100∼900 mg/㎡/day at the surface level. It showed that the net regeneration is above 50 mg/㎡/day at the bottom level. For dissolved inorganic phosphorus, the net uptake rate showed 10.0∼80.0 mg/㎡/day at the surface level, and the regeneration rate showed 0∼20.5 mg/㎡/day at the bottom level. Therefore, in order to control the water quality in Masan Bay, it is important to consider the re-supplement of nutrients regenerated in the water column.

인공지능 모델에 의한 지하수위 모의결과의 적절성 판단을 위한 허용가능한 예측오차 범위의 추정 (Estimation of the allowable range of prediction errors to determine the adequacy of groundwater level simulation results by an artificial intelligence model)

  • 신문주;문수형;문덕철;류호윤;강경구
    • 한국수자원학회논문집
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    • 제54권7호
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    • pp.485-493
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    • 2021
  • 지하수는 지표수와 함께 용수로 사용가능한 중요한 수자원이며 특히 섬 지역의 경우 전체 수자원 중 지하수의 이용 비율이 상대적으로 높기 때문에 안정적인 이용을 위해 지하수위 변동성에 대한 연구는 필수적이다. 지하수위 변동성의 예측 및 분석을 위해 인공지능 모델을 활용한 연구들이 지속적으로 증가하고 있으나 지하수위 예측결과의 적절성을 판단할 수 있는 평가기준을 제시한 연구는 충분하지 않다. 본 연구에서는 허용가능한 지하수위 예측오차의 범위를 제시하기 위해 과거 20년 동안 전 세계 다양한 지역을 대상으로 인공지능 모델을 활용하여 지하수위를 예측한 연구결과들을 종합적으로 분석하였다. 그 결과 관측지하수위의 변동성이 커질수록 인공지능 모델에 의한 지하수위 예측오차는 증가하였다. 따라서 관측지하수위 최대변동폭과 예측오차 간의 상관성과 기존 연구들에서 제시한 평가지수들을 고려하여 평가기준을 산정하였으며, 인공지능 모델에 의한 지하수위 예측결과의 적절한 평가기준은 도출된 선형회귀식에 의한 평균제곱근오차 또는 최대오차 이하이거나, NSE ≥ 0.849 또는 R2 ≥ 0.880 이다. 이 허용가능한 오차범위는 인공지능 모델을 활용한 지하수위 예측결과의 적절성 판단을 위한 참고자료로 사용할 수 있다.