• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.265-265
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• 2022

유량조사는 측선수, 측정시간, 측정위치, 측정방법 등 많은 기준이 있으며 이를 잘 준수하는 것이 높은 품질의 유량측정 성과를 확보하는 방법이다. 그러나 이러한 기본적인 기준을 잘 준수하더라도 현장 상황에 따라 유량측정 성과에 오차가 포함 될 수 있다. 본 연구에서는 상류 소수력발전소의 방류량에 따라 유량이 변화하고 수위관측소 부근에 큰 저류공간이 있는 현장 여건이 유량측정성과에 어떠한 영향을 끼치는지 검토하였다. 홍천군(주음치교) 관측소는 홍천강 상류에 위치하며 소수력발전소의 운영에 따라 관측소를 흘러가며 그 유량이 소수력발전소의 영향으로 점변한다. 일반적으로 이러한 경우 측정시간을 최대한 짧게 가져가 유량자료의 정확도를 확보한다. 하지만 홍천군(주음치교)의 경우 수위관측소 주변에 큰 저류공간이 있어 이를 동시에 고려해야 하며 단순하게 측정시간을 짧게 하는 것만으로는 측정성과의 품질을 확보 할 수 없다. 왜냐하면 이 저류 공간으로 물이 유입되는 시간동안은 수위관측소의 수위 상승은 미미하지만 하천 유량은 증가하는 부등류가 발생한다. 유량측정은 등류가정에 의한 것으로 수위관측소 주변이 부등류가 발생하면 유량측정 성과에 큰 오류가 나타나기도 한다. 홍천군(주음치교)에서 현장 상황이 등류일 때와 부등류일 때 모두 측정을 실시하였으며 그 차이를 확인하였다. 저류공간의 물 유입이나 유출이 없는, 즉 등류 상태의 유량측정 성과는 수위-유량관계식과 2.86%차이를 보였으며 부등류 상태의 유량측정 성과는 19.85%차이를 보여 큰 차이를 보였다(기준수위 0.49m). 또한 소수력발전소 운영에 따라 유량 상승 시에는 수위-유량관계곡선식 대비하야 양(+)의 편차율이 발생하고, 유량이 하강 시에는 수위-유량관곡선식 대비 음(-)의 편차율 발생하는 것으로 나타났다. 소수력 발전소는 동절기를 제외한 상시 운영으로 홍천군(주음치교) 관측소의 정확한 수위-유량관계식을 확인하기 위하여 소수력 발전소 운영을 중단하고 측정을 실시하였으며 유량변동을 멈추고, 즉 등류 흐름에서 측정한 성과는 수위-유량관계식과 차이가 1.06% 불과한 것으로 나타났다. 수문조사는 측선수, 측정시간, 측점수 등 많은 기준이 있다. 그러나 이러한 측정기준과는 별개로 현장은 다양한 조건이 발생하며 측정성과의 정확도에 영향을 끼치는 경우가 발생하기도 한다. 따라서 유량측정 기준을 잘 준수하는 것도 중요하지만 현장상황을 파악하고 이에 적절한 유량측정을 실시해야 그 오차를 최소화 할 수 있다.

• Journal of Soil and Groundwater Environment
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• v.10 no.1
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• pp.65-74
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• 2005

National groundwater monitoring stations have been managed throughout the country by Korea Water Resources Corporation (KOWACO) in order to monitor variations in quantity and quality of groundwater resources. A multi-sensor installed in each monitoring station well measures groundwater level, water temperature and electrical conductivity every six hours and the logged data are automatically transmitted to a host computer in KOWACO. Meanwhile despite regular station inspection and replacement of deteriorate or broken devices, abnormal values or outliers often occur due to intrinsic limitations of automatic monitoring and transmission. Thus prompt recognition and measures to these values are essentially required to reduce disturbance and missing period of the data. In this study, time and frequency of outlier occurrence were analyzed for the water level data obtained from national groundwater monitoring stations within the Han river basin in 2000. The analysis results indicated that the most prominent patterns of the outliers were rapid decline for water level, no variation for temperature and steep decline for electrical conductivity. This study provided a sample criterion for determining the outlier for each parameter.

• The Journal of Engineering Geology
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• v.14 no.4 s.41
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• pp.417-427
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• 2004

The horizontal collector well is used to treat some weak points of the vertical well in the bank filtration site. In this study two empirical formulas(Milojevic and Petrovic) are selected to examine the applicability for calculating the yield of the horizontal collector. And they are compared with the compute simulation results for multiple wells. Milojevic empirical formula which considers the conditions such as aquifer, well location, the diameter of screen etc. is more applicable than Petrovic formula. Draw-down characteristics of horizontal collector was well simulated by using the computer simulation for multiple wells. The results are well agreement with Milojevic formula, and the draw-down and the retention time of the horizontal collector can be controlled by adjusting the angle of lateral screens.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.12 no.3
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• pp.115-125
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• 1992

The variation of flow pattern caused by the topographical change of Kwangyang bay, is analyzed using the numerical tidal model for the depth-integrated two- dimensional long wave equation. The results of study are as follows. Due to pier construction, the area of water surface is deceased and the water inflow into the Kwangyang bay is reduced. For this result, at the outer bay of Myo island, the tidal range is slightly increased. And at the inner bay, water level is dropped generally, and especially at the time of low water tide, the phenomena of water level drop obviously appears. According to the variation pattern, flow velocities is lower than those of non-construction condition over the Kwangyang bay. But at the channel(from Kwangyang east stream) flowing into the east Kwangyang bay, for the contraction of channel profile, flow velocity is increased. The study based on the 100 year frequency design flood discharge from Sueocheon(river) and Dongcheon(river) which are flowing into the bay and Seomjin River flowing along the boundary of the bay is also performed. During the spring tide condition, the results showed the rise of water level about 1.2 m at Seomjin River Estuary and 0.3 m at inner bay is occurred.

• Journal of Korea Water Resources Association
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• v.40 no.3
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• pp.277-286
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• 2007

In this study, we analyzed the flow characteristics in the wide-crested side weir of trapezoidal section by using a three dimensional numerical stimulation. From this study, as the Froude number increases in the main channel, the overflow discharge ratio and the discharge coefficient of lateral overflow tend to decrease. And it was also found that the increase of the lateral overflow reduces the channel discharge area in the downstream, and the size of recirculating zone is increasing in the opposite side of side weir. The stream-wise water surface on the side where the side weir is installed falls down rapidly in the weir starting point, gradually ascending, and rapidly rising at the end point. The reason why the water surface rapidly rises at the weir end point is because the weir end point hinders the flow.

• Economic and Environmental Geology
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• v.51 no.6
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• pp.567-577
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• 2018

One of problems related with water curtain cultivation (WCC) in Korea includes severe declination of groundwater levels during the peak season, and it is likely that the problem can be resolved efficiently when the connection characteristics between groundwater and stream are well understood. This study examined temperature, and oxygen/hydrogen stable isotopic compositions of the flowing groundwater to understand the connection between stream and ground water, and the influence of stream water on the nearby aquifer. This study was performed in Wangjeon-ri (Kwangseok-myon, Nonsan City), the well-known strawberry town using WCC technique. The sampling was done during February 2010 through June 2011 for both groundwaters and nearby streams. Temperature distribution pattern indicates that stream widely affected groundwater in the right part of WCC ara. In the left part, the influence of stream seems to occur narrowly near the stream. The similar phenomenon is reflected in the oxygen and hydrogen isotopic data.

• Proceedings of the Korea Water Resources Association Conference
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• 2015.05a
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• pp.252-252
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• 2015

우리나라에서는 대하천정비사업을 통해 주요 국가하천마다 보와 제방을 신설 및 보축하여 홍수의 방어 및 예방에 힘을 기울이고 있으며, 근래에는 이러한 정비사업이 완료되어 가고 있는 상황이다. 제방에 대한 정비사업의 내용은 보축 및 신설이 주를 이루나, 제내지의 성토와 제외지의 보강 및 저수로의 준설 등도 함께 수행되었다. 이러한 정비사업의 영향으로 지하수 및 하천의 흐름양상은 정비사업 전과는 다르게 변화 될 것으로 추정되며, 이는 제방 안정성에 영향을 줄 수 있는 중요한 문제로 판단된다. 따라서, 이와 같은 지하수 및 하천흐름의 변화양상이 제방의 안정성에 얼마나 영향을 미칠 수 있는지 정량적으로 분석할 필요가 있을 것으로 보인다. 특히, 대하천정비사업으로 지반누수를 방지하기 위한 제내지 성토나 퇴사제거를 위한 하천준설 등이 수행되면서 제방의 외적인 환경들이 많이 변하게 되었으나 이에 대한 정량적인 연구들이 거의 수행되지 않은 것으로 판단된다. 따라서, 본 연구에서는 낙동강과 회천 합류부에 위치한 율지제를 대상으로 이곳에 설치된 간극수압계의 데이터와 2차원 침투해석 프로그램인 SEEP/W를 이용하여 제내지와 제외지 표고변화에 따른 파이핑 안정성을 분석하였다. 그 결과 제내지 표고가 상승하면 파이핑 안전율이 증가하고 표고가 하강하면 안전율은 감소하는 것으로 나타났다. 한편, 제외지의 표고변화는 제방안정성에 거의 영향을 주지 않으며 오히려 하천수위의 영향을 지배적으로 받는 것으로 판단된다. 따라서, 제방안정성을 확보하기 위해서는 기초지반의 경우, 제내지측을 상승시키고 하천수위를 하강하는 것이 효과적일 것으로 판단된다.

• Journal of Korea Water Resources Association
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• v.40 no.10
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• pp.793-800
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• 2007

This research applied to Wavelet transform that have soft resolution time and frequency area for stage of Hadong2 station in order to extract to discharge component by rainfall and tidal level component by tide. Approximation component(A6) of last level for wavelet decomposition displayed the biggest energy value 87.77%, and detail component(D3) energy value was 10.70% with periodicity of semidiurnal tide type(about 12 hours). Also skewness, kurtosis values of D3 have similar to tidal level of Yeosu. Approximation component(A6), Detail component(D6, D5) for Hadong2 stage was runoff component, and detail component(D4, D3, D2) was tide component according to effect of tide.

• The Journal of the Convergence on Culture Technology
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• v.6 no.3
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• pp.393-399
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• 2020

In this study, the subsidence behavior caused by groundwater ex-flow in a limestone cavity encountered during tunnel excavation was quantified based on numerical analysis and the effect was analyzed. Based on the groundwater level and surface subsidence surveyed at the site, a numerical analysis technique was applied to analyze the characteristics of the subsidence behavior according to the tunnel passage of the geological vulnerabilities. The results of groundwater seepage-coupled analysis were analyzed to reflect the actual ground subsidence behavior. As a result of the study, it was analyzed that the ground subsidence due to the tunnel excavation in the limestone common section(the geological vulnerable zone) was analyzed that the dramatical decrease in groundwater level was the main cause. As a result of numerical analysis, it was analyzed that the long-term cumulative settlement of the asphalt surface after the groundwater ex-flow was 76~118mm due to the reduction of the volume of the soil layer due to the decrease in the groundwater level, and the settlement amount increased as the depth of the soil layer increased.

• Tunnel and Underground Space
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• v.27 no.4
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• pp.205-216
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• 2017

Fluctuations in groundwater level are the major cause of ground subsidence in the abandoned limestone mine. In this study, evaluation of groundwater flow under three different cases of natural condition, aggregate-filling, temporary drainage in groundwater-saturated limestone mine cavities was executed by 3-dimensional analysis. In the case of aggregate-filling, although the water level both in the upper ground of mine cavities and an agricultural watershed was elevated, it was lower than the water level fluctuation of an agricultural water use and rainfall and the flow rate was similar to the flow rate of natural condition. In the case of temporary drainage, as the water level in the upper ground of mine cavities and an agricultural watershed decrease rapidly and the flow rate has increased by 25times, so the risk of ground subsidence increased.