• Geomechanics and Engineering
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• 제10권6호
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• pp.727-736
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• 2016

Excessive rainfall can cause runoff flows over the soil surface and as a consequence some amount of water will infiltrate into the soil. From a hydrologic modeling perspective it is necessary to estimate infiltration rate in order to calculate the actual runoff discharge. There are many parameters that can affect the infiltration rate such as soil texture, moisture and compaction. However, the most common equations used in hydrological calculations for estimating the infiltration rate do not consider the soil properties directly and estimate infiltration rate without any soil properties expressions. The purpose of this research was to investigate the relations between infiltration rate and soil texture, moisture and compaction. To achieve this purpose an experimental study was performed to show the effect of soil properties and their relations on infiltration rate by using non-linear regression.

• 한국습지학회지
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• 제13권3호
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• pp.465-470
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• 2011

액비와 퇴비 형태로 발생되어지는 양돈 분뇨는 발생량의 대부분이 농지에 적용되어지고 있다. 과잉으로 적용된 양돈 퇴, 액비는 수계의 영양소 과잉의 주원인으로 알려지고 있는데 양돈 퇴, 액비의 질소, 인 물질이 농지로부터 지표수와 지하수로 전달되어지는 경로를 파악하는 것이 본 연구의 주목적이다. 인공 강우 시험을 통해 농지로부터 양돈 퇴비와 액비가 각각 적용되어진 농지에 대해 지하수와 지표수로 유출되는 양을 조사하였는데 질소의 경우 지하수로 유출되는 부분이 가장 많은 반면 인의 경우 토양에 흡착되는 부분이 가장 많은 것으로 나타났다. 토양에 대한 인의 평균 흡착 양은 21.5 mg P/kg soil 로 나타났다.

• 한국농공학회지
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• 제37권5호
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• pp.81-89
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• 1995

One of the most difficult problem to estimate the flood inflow is how to understand the effective rainfall. The effective rainfall is absolutely influenced by the condition of soil moisture in the watershed just before the storm event. DAWAST model developed to simulate the daily streamflow considering the meteologic and geographic characteristics in the Korean watersheds was applied to understand the soil moisture and estimate the effective rainfall rather accurately through the daily water balance in the watershed. From this soil moisture and effective rainfall, concentration time, dimensionless hydrograph, and addition of baseflow, the rainfall-runoff model for flood flow was developed by converting the concept of long-term runoff into short-term runoff. And, real-time flood forecasting model was also developed to forecast the flood-inflow hydrograph to the river and reservoir, and called RETFLO model. According to the model verification, RETFLO model can be practically applied to the medium and small river and reservoir to forecast the flood hydrograph with peak discharge, peak time, and volume. Consequently, flood forecasting and warning system in the river and the reservoir can be greatly improved by using personal computer.

• 환경영향평가
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• 제22권1호
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• pp.1-17
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• 2013

Carbon sequestration on soil is one of the counter measurements against climate change in agricultural sector. Increasing incorporation of organic fertilizer would increase soil organic carbon (SOC) but it could bring high potential of nutrient losses which would result in water quality degradation. In this paper, literature review on soil organic carbon behavior according to agricultural management is presented. The results of field experiment to identify the effect of organic and commercial fertilizer applications on SOC and runoff water quality were also presented. Field experiment confirmed increased SOC and nutrient concentrations in runoff water as application rate of organic fertilizer increase. The potential use of simulation model to develop best agricultural management practice considering carbon sequestration and water quality conservation at the same time is discussed and monitoring and modeling strategies are also suggested to achieve the goal.

• 한국공간정보시스템학회 논문지
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• 제11권1호
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• pp.97-104
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• 2009

현재 GIS는 유역의 지형학적 분석분야에서 뿐만아니라 유역의 수문학적 분석분야에서도 유용한 도구로 활발하게 활용되고 있다. 본 연구에서는 SSARR모형을 기반으로한 유역유출분석 모형을 활용하여 금강유역을 대상으로 장기유출량을 산정, 검증하고 이를 토대로 강우-유출 관리 모듈과 연계하여 신뢰도 있는 수문정보를 산정하여 사용자에게 제공코자 하였다. 모의와 검증을 거친 적정한 토양습윤지표, 용수이용량, 직접 및 기저유출량 등의 다양한 수문성분들이 GIS Tool의 활용을 통하여 소유역 단위의 유용한 수문학적 공간정보로서 생산되었다. 또한 사용자의 편의를 위하여 Graphic User Interface를 설계하여 다양한 수문정보를 도시함으로써 향후 효율적 유역수문관리를 지원하는 Toolkit으로 활용될 수 있을 것으로 판단된다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.48-58
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• 2004

Objectives of this research were to reclaim the coal mine overburdens using the lime waste cake from the soda ash production by stabilizing the overburden slopes, introducing neutralizing the AMD from runoff and leachate in an attempt find the sink to dispose the lime wastes and alleviate the environmental problems caused by the closed coal mines. The pH changes of the runoff and leachate collected in the tanks at the end of the experimental plots, averaged over measurements from April to August, indicated that the runoff pH of the coal overburden was 4.3 but increased significantly to the ranges of 6.7 to 7.1 with treatments of tile calcites and lime wastes. This might be related with the decreases in Fe concentrations in the runoff and leachate from the coal overburdens. The Fe concentrations in tile runoff seemed to increase with the amounts of precipitation. Results demonstrated that the amounts of lime wastes at 25% of the lime requirement were sufficient for neutralizing the acidic coal overburden. Either layering between the coal waste and topsoil or mixing with coal overburdens could be adopted as the lime waste treatment method. The lime wastes from the soda ash production might have a potential to be recycled for the reclamation of the abandoned coal mines to alleviate the environmental problems associated with coal mine waste.

• 한국토양비료학회지
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• 제34권3호
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• pp.158-164
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• 2001

밭토양에 돈분이 시용되었을 때 토양에서 유실되는 유거수에 의한 질산태질소의 유거손실을 구명하기 위하여 본 연구를 실시하였다. 경사가 4% 정도 되는 밭토양에 나지와 옥수수 재배조건 하에서 돈분을 무처리, 50, $100ton\;ha^{-1}$ 수준으로 처리하고 유거수 중에 질산태질소 유거량을 조사한 결과는 다음과 같다. 유거수량은 강우량이 많을수록 증가하였으나 돈분시용량이 증가할수록 유거수량은 감소하였다. 유거수 중에 질산태질소의 농도는 옥수수 재배조건에서 높았는데 같은 처리 조건에서 나지에서의 유거수 중에 질산태질소 농도에 비하여 86.9, 42.9,33.6% 가 높았다. 질산태질소의 총유거 손실량은 나지구에서 높았으며 처리 수준별 유거량은 $1.34{\sim}3.15kg\;NO_3-N\;ha^{-1}$ 였다. 유거수 중에 양이온들의 농도는 K> Mg> Na> Ca 순이었다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2006년도 학술발표회 논문집
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• pp.2-11
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• 2006

In the processes of hydrological cycle, when precipitation reaches the ground surface, water may become surface runoff or infiltrate into soil and then possibly further percolate into groundwater aquifer. A part of the water is returned to the atmosphere through evaporation and transpiration. Soil moisture dynamics driven climate fluctuations plays a key role in the simulation of water transfer among ground surface, unsaturated zone and aquifer. In this study, a one-layer canopy and a four-layer soil representation is used for a coupled soil-vegetation modeling scheme. A non-zero hydraulic diffusivity between the deepest soil layer modeled and groundwater table is used to couple the numerical equations of soil moisture and groundwater dynamics. Simulation of runoff generation is based on the mechanism of both infiltration excess overland flow and saturation overland flow nested in a numerical model of soil moisture dynamics. Thus, a comprehensive hydrological model integrating canopy, soil zone and aquifer has been developed to evaluate water resources in the plain region of Huaihe River basin in East China and simulate water transfer among precipitation, surface water, soil moisture and groundwater. The newly developed model is capable of calculating hydrological components of surface runoff, evapotranpiration from soil and aquifer, and groundwater recharge from precipitation and discharge into rivers. Regional parameterization is made by using two approaches. One is to determine most parameters representing specific physical values on the basis of characterization of soil properties in unsaturated zone and aquifer, and vegetations. The other is to calibrate the remaining few parameters on the basis of comparison between measured and simulated streamflow and groundwater tables. The integrated modeling system was successfully used in the Linhuanji catchment of Huaihe plain region. Study results demonstrate that (1) on the average 14.2% of precipitation becomes surface runoff and baseflow during a ten-year period from 1986 to 1995 and this figure fluctuates between only 3.0% in drought years of 1986, 1988, 1993 and 1994 to 24.0% in wet year of 1991; (2) groundwater directly deriving from precipitation recharge is about 15.0% t of the precipitation amount, and (3) about half of the groundwater recharge flows into rivers and loses through evaporation.

• 한국토양비료학회지
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• 제40권6호
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• pp.488-494
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• 2007

고랭지 농업은 표고가 높은 산지의 경사지에서 이루어지고 있고, 비료 및 퇴비 등의 고투입농법에 의존하고 있기 때문에 토양유실 가능성이 상당히 높고 따라서 환경에 악영향을 미칠 가능성이 크다. 이 연구는 식생을 이용한 토양 유실저감효과를 규명하기 위하여 경제성이 있는 산채작물을 재배함으로서 이들의 토양 유실 저감 정도를 평가하였다. 2005년 실험에 따르면 배추포장에 비하여 눈개승마와 참취 포장의 토양 유실량은 1/2로 저감되었으며, 유출량 또한 상대적으로 눈개승마 재배 포장과 침취 재배 포장에서 낮은 것으로 나타났다. 경사도(15%, 30%, 45%)에 따른 토양유실량은 경사도가 증가할수록 증가하였으며, 15% 포장에서 눈개승마의 경우 52.50 kg, 30% 포장에서 눈개승마의 경우 108.33 kg, 45% 포장에서 눈개승마의 경우 171.50 kg로 나타났으며, 배추포장의 경우는 눈개승마 포장에 비해 2~3배 많은 토양 유실량을 보였다.

• 한국농공학회:학술대회논문집
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• 한국농공학회 1998년도 학술발표회 발표논문집
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• pp.22-27
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• 1998

A grid-based soil moisture routing model(GRISMORM) was developed to assess the information of groundwater recharge using spatial data such as Landsat TM and digital elevation model etc.. The model predicts the hydrologic components, that is, surface runoff, subsurface runoff, baseflow and evapotranspiration at each grid elements by grid-based water balance computation.