• The Journal of Engineering Geology
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• v.23 no.4
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• pp.375-380
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• 2013

The concept of safe yield places an emphasis on balancing groundwater withdrawal with groundwater recharge but ignores naturally occurring groundwater discharge. Because streams and their alluvial aquifers are closely linked in terms of water supply and water quality, to be properly understood and managed they must be considered together. Therefore, some districts in Kansas have reevaluated their safe-yield policies to account for natural groundwater discharge and stream-aquifer interactions by amending their safe-yield regulations to include a portion of baseflow as the minimum desirable streamflow (MDS). This study proposes a modified safe-yield policy in which the drought flow is chosen as the MDS. Baseflow separation was conducted from streamflow hydrograph and the results are presented as a flow-duration curve. The exploitable groundwater can be determined by subtracting MDS from the cumulative baseflow. This method was tested in the Musimcheon watershed, which was validated for streamflow using the SWAT-K model. The annually averaged exploitable groundwater in the whole watershed was estimated to be 86 mm. The exploitable groundwater amounts were also estimated for each subwatershed in the Musimcheon watershed.

• Water for future
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• v.16 no.3
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• pp.171-179
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• 1983

In the Jeon Cheon Basin, unconsolidated alluvium and marine clay beds overlying Tertiary conglomerate and impermeable mudstone, and Cambro-Ordovician sedimentary rocks composed of mainly cavernous limestones, and age-unknowned crystalline rocks are occured. Most productive rock is Cambro-Ordovician limestones containing a lot of solution openings and secondary porosities and shows its transmissivity of 1836$m^2$/day and storativity of 1.47 $\times$ $10^{-3}$. The storage of deep seated groundwater in linestone aquifer is estimated about 1059 $\times$ $10^6$ metric tons, being equivalent to 6 years total precipitation of the basin. The safe yield of the groundwater to be abstracted from the aquifer is about 126,000 tons/day. To pump at least 100,000 tons/day of groundwater from the said aquifer, a well field comprising 34 deep wells ranging in depth from 80 to 100 meter and penetrating the cavernous limestone aquifer shall be established at middle and down stream area.

• Proceedings of the Korea Water Resources Association Conference
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• 2018.05a
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• pp.21-21
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• 2018

수자원 시스템의 용수공급의 안정도를 평가하는 지표로 국내에서는 이수안전도 혹은 안전채수량(safety degree for water shortage or safe yield)의 개념이 이용된다. 아울러 공급 측면에서는 기준갈수량, 공급신뢰도, 저수용량 등이 분석되고 있으며, 수요 측면에서는 용수공급 보장일수, 최소 부족량, 갈수 조정기간 및 용수부족에 따른 피해정도 등을 고려하고 있다. 전통적으로 수자원 시스템의 평가는 용수공급 실패기간의 통계적 특성을 분석하여 이루어진다. 용수공급 실패기간으로부터 분석되는 통계적 특성은 용수부족 발생빈도, 용수부족 지곡기간 및 용수부족 총 양 등 세 가지로 정량화되는 것이 일반적이다. 수자원 시스템이 수요를 만족시키는 정도인 신뢰도(reliability), 용수부족 발생 후 얼마나 빨리 회복하는지를 나타내는 회복도(resilience) 및 용수부족의 양적 크기를 나타내는 취약도(vulnerability)의 지표는 앞서 언급된 세 가지 통계 특성으로부터 계산된다. 본 연구에서는 Copula 기반 이변량 빈도해석 개념을 적용하여 댐 용수공급 취약성 평가 방법을 개선한 후, 국내 남강 댐 유역의 용수공급 취약성을 평가해보고자 한다. 이를 위해, 국내외에서 이용되고 있는 용수공급 평가지표들의 특성들을 정리하였다. 다음으로는, 취약성 평가 방법에 Copula 기반 이변량 빈도해석 방법을 적용하는 방법을 제안하였다. 본 연구의 분석은 용수공급 실패 사상을 기준으로 수행되었으며, 용수공급 실패 사상의 발생확률은 포아송 분포, 총 부족량은 대수정규분포로 모의되었다. 최종적으로는 남강 댐의 재현기간별 취약성 평가 결과를 도출하여 본 연구에서 제안한 취약성 평가방법의 적용성을 검증하였다.

• Water for future
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• v.27 no.1
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• pp.79-88
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• 1994

This study was conducted to analyse groundwater flow in the Bugok hot spring area using the MODFLOW model which can simulate three dimensional groundwater flow both in confined and unconfined aquifers. Based on this study the following conclusions were obtained: 1) The hydraulic conductivity and the specific storage of the aquifer were 0.0135 m/day and 0.020, respectively, and the model-predicted groundwater elevation agreed well with the observed one. 2) Simulation results showed that the groundwater level declines at the end of the one-year simulation period when the annual recharge rate is small and the annual pumping rate high, which is the worst combination. Except that combination, the groundwater level does not decline at the end of one-year simulation period indication the pumping rates used were allowable. 3) The safe yield depends upon the magnitudes of the recharge and pumping rates. The pumping rate should not produce excess decline of groundwater level around April when the water level is the lowest in a year.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.34 no.6
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• pp.1797-1806
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• 2014

By far, groundwater management has been conducted by 'safe yield' policy based on the estimation of annual average of groundwater recharge throughout the world. However, as groundwater recharge show spatiotemporal variation, dynamic analysis must be carried out to evaluate the sustainable groundwater resources. In this study, an integrated surface-groundwater model, SWAT-MODFLOW was used to compute the spatial distribution of groundwater recharge in Gyungju region. Frequency analysis is adopted to evaluate the existing values of potential amount of groundwater development which is made by the 10 year drought frequency rainfall multiplied by recharge coefficient. The conservative methods for estimating recharge rates of 10 year drought frequency in subbains are newly suggested and compared with the existing values of potential amount of groundwater development. This process will promote the limitations for existing precesses used for computing potential amount of groundwater development.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.58-58
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• 2020

최근 급속한 지하공간의 개발로 인해 도로함몰 등 지반침하가 지속적으로 발생되어 이에 대한 안전문제가 끊임없이 제기됨에 따라, 원인규명 및 대책방안을 두고 다양한 조사 및 연구가 진행되고 있다. 특히 지하개발 시 필연적으로 발생하는 유출지하수 내 지하수와 함께 토사가 유출될 경우 지반함몰이나 붕괴로 이어져 대규모 재해가 발생할 수 있기 때문에 현장에서 계측되는 데이터를 통해 사전에 지반침하를 감지할 수 있는 경보 시스템이 마련될 필요가 있으며, 이에 대한 기술개발과 관리기준의 변화가 필요하다. 본 연구에서는 현재 지하공간 개발 시 적용되는 지하수 관리 매뉴얼 중 가장 중요한 부분인 계측관리 부분에 관해 문제점을 분석하고 이를 보완하기 위한 계측 관리 및 행정 절차의 문제점을 개선하고자 한다. 지중에서 발생하는 토립자의 이동, 공동발생 및 지반함몰의 거동은 근본적으로 지하수의 이동에 의해 필연적으로 발생되며, 그 규모는 유출지하수량의 발생규모와 상관성이 높게 분석되었다. 계측 관리의 문제를 보완하기 위하여 첫 번째로 지중 굴착 시 계측되는 유출지하수와 지하수위를 연계하여 분석하여 기준을 마련하였고, 추가로 지하수 내 탁도 값을 측정하여 이를 더하여 서로간 상관성 분석을 통해 기존 지하수위 계측자료의 관리기준을 보완하였으며, 최종적으로 현장에서의 계측된 데이터를 통해 지반침하를 사전에 예측할 수 있다. 계측된 데이터의 분석결과 위험도가 감지될 경우 공동발생의 방지 및 복구에 관한 방안이 제시되며, 문제 발생 지점의 범위를 국한하여 신속하고, 경제적으로 해결해 나갈 수 있다. 이를 위해 현행 지하수법의 개선과 행정적 절차가 보완되어야 할 필요가 있다. 이러한 지하공간 개발 시 지하수 관리의 개선으로 사전에 지반침하를 예측 할 수 있고, 이를 통해 재해를 미연에 방지할 뿐만 아니라 건설산업 현장의 스마트 관리체계를 구성하여 미래 지향적인 토목현장 및 국민에 대한 신뢰도를 재고 할 수 있을 것으로 사료된다.

• KOREAN JOURNAL OF CROP SCIENCE
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• v.14
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• pp.79-86
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• 1973

In order to investigate the heading responses of naked barleys and their grain yields under the different sowing times in spring sowing at 9 levels and to select the promising variety, present work was carried out with 11 recommended naked barley varieties and 2 newly developed lines for the period of 3 years from 1971 to 1973 at Iri, these results being summarized as follows: 1. Under spring sowing cultures, 'Wanju naked barley' being spring habit showed the highest yields among them. However, Sedohadaka and Bangju being winter habit were also considered as the promising varieties. 2. In the case of sowing the spring type naked barleys in spring the optimum sowing time of barleys at Iri was estimated in the late of February or the early of March. 3. The number of main culm leaves and tillering per hill of 'Wanju naked barley' were not influenced at sowing times. But winter type barleys being sown in spring, they were outstandingly increased in accordance with the sowing time being late, especially after the critical sowing time. 4. In comparison with average days from germinating to heading date under different seasonal sowing at the same variety, 'Wanju naked barley' took 64.4 days to get heading and Kikaihadaka and Hyangchoen gwa, the low spring growing habit varieties, 72-73 days. 5. Young spikelet differentiation stage (length of young spikelet: 0.3-0.5mm) arrived at about 30 days before heading date in comfortable sowing time without regarding spring or winter type. But number of main culms disclosed great differences among them; barleys being high spring type were 4 leaves and low about 6. 6. In the view of morphology, culm length under the different seasonal sowing could not be found out differences in the high spring type barleys, but in the low, it was grately shortened by postponing the sowing time. The barley height of rosette form had no difference at any sowing time.difference at any sowing time.

• The Journal of Engineering Geology
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• v.5 no.3
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• pp.289-300
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• 1995

At the initial stage of the underground reservoir design one should thoroughly consider surface and subsurface hydrology, hydrogeologic characteristics of aquifer system, and the function of cut - off wall because it is linked to the effective management. In this study, three dimensional finite difference model was applied to analyse the function of Ian underground reservoir at Kyungbuk Province. The steady and unsteady state conditions after construction of the underground dam were simulated through the model, and from these results the groundwater budget and the safe yield were determined. The model simulation indicates the infiltration of irrigation water to be one of the major factors of seasonal fluctuation of groundwater level. The recharge rates of irrigation water were estimated as 4.3mm/d during May and June, and 1.7mm/d during July and Agust. Groundwater recharge from the watershed area estimated to about $0.04m^3/s$, almost consistent through the year. In 1984, groundwater discharge through the transverse section of the dam was $0.002m^3/s$ and the optimum yield for two momths(July and Aguest)was $254000m^3$, however, the discharge became $0.013m^3/s$ in1993, implying the failure of cut -off function. without appropaiate of the cut - off wall, optiumum yield during the irrigaton period would be $93, 000m^3$.

• Journal of Korea Water Resources Association
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• v.53 no.12
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• pp.1193-1201
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• 2020

This study aims to develop a regression model that estimates a low-flow index that can be applied to ungauged basins. A total of 30 midsized basins in South Korea use long-term runoff data provided by the National Integrated Water Management System (NIWMS) to calculate average low-flow, average minimum streamflow, and low-flow index duration and frequency. This information is used in the correlation analysis with 18 basin factors and 3 climate change factors to identify the basin area, average basin altitude, average basin slope, water system density, runoff curve number, annual evapotranspiration, and annual precipitation in the low-flow index regression model. This study evaluates the model's accuracy by using the root-mean-square error (RMSE) and the mean absolute error (MAE) for 10 ungauged, verified basins and compares them with the previous model's low-flow calculations to determine the effectiveness of the newly developed model. Comparative analysis indicates that the new regression model produces average low-flow, attributed to the consideration of varied basin and hydrologic factors during the new model's development.