• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2007년 가을학술발표회
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• pp.481-501
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• 2007

Excessive rainfalls due to climatic changes can trigger an increase in rainfall-induced slope failures that pose real threats to both lives and properties. Many high slopes in residual soils could stand at a steep angle, but failed during or after rainfall. Commonly, these slopes have a deep groundwater table and negative pore-water pressures in the unsaturated zone above the groundwater table contribute to the shear strength of soil and consequently to factor of safety of the slope. Stability assessment of slope under rainfall requires information on rate of rainwater infiltration in the unsaturated zone and the resulting changes in pore-water pressure and shear strength of soil. This paper describes the application of unsaturated soil mechanics principles and theories in the assessment of rainfall effect on stability of slope through proper characterization of soil properties, measurement of negative pore-water pressures, seepage and slope stability analyses involving unsaturated and saturated soils. Factors controlling the rate of changes in factor of safety during rainfall and a preventive method to minimize infiltration are highlighted in this paper.

• 한국토양비료학회지
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• 제18권2호
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• pp.121-127
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• 1985

토양수분(土壤水分)을 효율적(效率的)으로 관리(管理)할 수 있는 토양개량방법(土壤改良方法)을 구명(究明)하고 토양입단(土壤粒團)의 특성(特性)이 수분변화(水分變化)에 미치는 영향(影響)을 파악(把握)하여 토양구조개선(土壤構造改善)에 적정기준(適正基準)을 제시(提示)하기 위(爲)하여 사양토(砂壤土)와 식양토(埴壤土)에 친수성(親水性)인 Uresol과 소수성(疎水性)인 Bitumen을 처리(處理)하여 시험(試驗)을 실시(實施)하였다. Perspex관(管)을 세토(細土)로 채우고 개량제(改良劑)를 처리(處理)한 토양입단(土壤粒團)과 처리(處理)하지 않은 토양(土壤)을 2cm 두께로 복토(覆土)한 후(後), 인공강우하(人工降雨下)에서 수분(水分)의 침투량(浸透量)을 측정(測定)하고 인공기상조건(人工氣象條件)에서 r-선(線) 수분측정기(水分測定機)를 이용(利用)하여 수분(水分)의 증발량(蒸發量)을 조사(調査)하였다. 토양(土壤)의 수분침투량(水分浸透量)은 친수성(親水性) 토양개량제(土壤改良劑) Uresol 처리(處理)에 의하여 18.7~50.8% 증대(增大)되었으며 소수성(疎水性) Bitumen 처리(處理)는 25% 이하(以下)로 감소(減少)되었다. 증발량(蒸發量)은 Bitumen 처리(處理)로 22.0~68.1%로 억제(抑制)되었으며 Uresol 처리(處理)도 38.7~68.4%로 감소(減少)되었다. 수분침투(水分浸透)와 증발(蒸發)을 합(合)한 총수분이용율(總水分利用率)은 Uresol 처리(處理)에 의하여 2배(倍) 이상(以上) 높일 수 있었다. 토양입단(土壤粒團)의 안정성(安定性), 습윤각(濕潤角)등은 수분(水分)의 침투(浸透)와 증발(蒸發)에 영향(影響)을 끼쳤으며 특(特)히 수분침투(水分浸透)와 습윤각(濕潤角)-안정지수(安定指數), 수분증발(水分蒸發)과 습윤각(濕潤角)-불안정지수(不安定指數)와는 고도(高度)의 유의성(有意性)있는 대수함수적(對數函數的)인 정(正)의 상관(相關)이 있었다. 토양입단(土壤粒團)의 안정성(安定性)은 수분(水分)의 침투(浸透) 및 증발억제(蒸發抑制)와 정상관(正相關)이 있으나 습윤각(濕潤角)의 개선(改善)은 수분침투(水分浸透)와 증발(蒸發)을 모두 증대(增大)시키는 요인(要因)이 되므로 전체적(全體的)인 수분관리면(水分管理面)에서는 토양입단(土壤粒團)의 안정성(安定性)을 증대(增大) 시키는 것이 효율적(效率的)인 것으로 판단(判斷)되었다.

• 상하수도학회지
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• 제10권1호
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• pp.69-77
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• 1996

To evaluate the change of the groundwater flow and the water table response resulting from urbanization, two cases of the transient three-dimensional numerical simulations were performed. Variations of the groundwater flow system caused by withdrawals were analyzed. Two cases of infiltration rates were applied in this study to verify the water table changes. One is the rate under the circumstance during 1994 and the other is the revised rate. The numerical results from this study indicated that groundwater flow was influenced by human impacts. Groundwater flow has been concentrated to Taegu Textile Complex area where had large amount of pumping. Water table so far decreased -2.76m a year due to withdrawals. Water tables of many points were increased more than 30cm when the surface was reformed by infiltrating the rainfall. It was appeared that the improvement of surface to recharge the precipitation was very important to preserve and manage for the groundwater.

• 한국수자원학회논문집
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• 제49권9호
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• pp.741-748
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• 2016

개착식 하상여과에 대해서 실험실 규모의 모형을 구축하고 중사, 왕사, 화산석, 자갈에 대한 단일 여재를 구성하였다. 실험을 통해 투수계수 및 하상 여과에 대한 취수량을 추정하고, 지하수 유동 모델링인 Visual MODFLOW를 통해 탁도 변화에 따라 수정된 투수계수를 적용하고 미치는 영향을 분석하였다. 각 여재마다 22개의 수정 투수계수 시나리오가 적용되었다. 전체 모델링에서 최소 오차는 화산석(2~5 mm)을 여재로 한 경우 상부에서부터 3개 지층에 대해서 20% 감소된 투수계수를 적용한 시나리오다. 이는 화산석의 특성상 탁도를 유발하는 황토가 여재에 흡착되어 상부에서 3번째 지층까지 영향을 미치는 것으로 추정되었다. 또한 입자의 크기가 작은 중사의 경우 5% 감소된 투수계수를 상부에서 두 번째 지층까지 적용한 시나리오에서도 작은 오차 값을 나타냈다.

• 한국농공학회지
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• 제31권2호
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• pp.116-124
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• 1989

Based on the theory of runoff equation proposed by SCS, the actual storage capacity(Sa) as a modified retention paramater was introduced to estimate the effective rainfall for the daily streamfiow analysis. During a storm, the actual storage capacity is limited by either soil water storage or infiltration rate as precipitation increases. Therefore, it was assumed that Sa is dependent on the baseflow before storm runoff(Qb) corresponding to soil water storage and the total amount of precipitation(P) corresponding to infiltration rate of a watershed. Effective rainfalls (Direct run-offs) estimate4 from SCS equation using Sa were compared with observed effective rainfalls at 10 watersheds in Geum river watershed boundary. 1. Regression equation for Sa was supposed Sa=Co+C$_1$XP+C$_2$X Qb Regression coefficients were highly significant at the level of 0. 01 and R$^2$ were 0.57 to 0.73. 2. The adjustment of coefficient of initial abstraction was made according to the storm size. It was adjusted to 025 for 30mm or less, 0.23 for 30 to 80mm, 0.20 for 80 to 200mm, and 0.1 for 200mm or more. 3. Regression equations between estimated and observed effective rainfall showed that slopes were 0.857 to 1.029 and R$^2$ were 0.779 to 0.989,

• Korean Journal of Hydrosciences
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• 제3권
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• pp.11-29
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• 1992

Recently, rapid industrialization, urbanization and higher living standards accelerate to increase groundwater consumption resulting in continuously dropping groundwater elevations. To maintain enough groundwater volume without dropping groundwater elevations, the proper groundwater rechatge is necessary. The groundwater rechatge can be classified into two categories which are natural rechatge and artiticial rechatge. Even though the natural rechatge through by dired infiltration from the rainfall is desirable, the artificial groundwater rechatge is necessaty when the increment of groundwater consumption exceeds natural recharge rate. Well method and scattering method are utilized as artificial rechatging method, a severe disadvantage, which is the reduction of the void of soil surface, is indicated in the well method. Recently, the underground piping method, which is a scattering method, is receiving increasing attention as a proper recharging method. The method is indirectly to supply water to the underground using an underground piping system. Therefore, the void of soil surface is not severely reduced and better infiltration rate can be achieved. In this paper, the artificial groundwater rechatge using underground piping method is investigated through experiments and numerical analysis. The influence of the groundwater by underground piping method is evaluated through comparing recharging heights. Good agreements between experiments and numerical analysis are obtained and the artificial groundwater recharge by underground piping method is well tested and verified.

• 한국조경학회지
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• 제27권3호
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• pp.109-113
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• 1999

The objective of this research was to develop growth media for artificial ground by blending calcined clay and coconut peat. To achieve this, aggregates of clay particles were mixed with disel oil and heated to high temperature(1150~120$0^{\circ}C$) to expand clays. The particle sizes of expanded clay were controlled to 2~5mm in diameter. Then expanded clayes were mixed with coconut peat and changes of soil physicochemical properties and their effect on plant growth of Hedera L. were determined. The infiltration rate of calcined clay was very high, but the water holding capacity, the cation exchange capacity(CEC), and the nutrient contents were low. The characteritics of coconut peat was vice verse to calcined clay. This indicates that the mixture of calcined clay and coconut peat have the better characteristics than each material. As compared to mineral soil, the infiltration rate, the water holding capacity, the CEC and the nutrient contents increased, but bulk density decreased to about 1/4. And, Hedera L. grown in the mixture of calcined clay and coconut peat(6:4, v/v) had higher plant height, longer leaf length, more total number of leaves per plant and fresh weight than that grown in mineral soil, but statistical differences were not observed between two treatments.

• 한국습지학회지
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• 제18권2호
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• pp.183-193
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• 2016

본 연구에서는 고속도로 강우유출수 처리목적의 우드칩 충진 침투도랑 모니터링 연구를 통하여 설계 적정성 및 성능을 평가하였다. 강우시 모니터링 자료를 바탕으로 침투도랑의 평균 저감효율을 산정한 결과 TSS 88%, COD 94%, BOD 85%, TN 80%, TP 75%이었으며 강우조건 및 설계가 다르므로 국내외 다른 연구결과와 직접적인 비교는 어렵지만 개략적으로 유사한 저감성능을 보였다. 침투도랑의 가장 중요한 설계인자인 침투속도를 산출한 결과 강우강도가 증가함 따라 침투속도도 증가하였으며 평균 침투속도는 40mm/hr, 도랑 내부의 유효 저류수심 0.8m를 기준으로 침투시간을 산출한 결과 약 0.83일로 비점오염저감시설 설치 및 관리 운영 매뉴얼(MOE, 2014)의 설치기준(이하 설치기준)을 만족하는 것으로 나타났다. 수문자료에 따르면 유입량 기준으로 설계 누적강우유출고로 산출된 WQv와 유사한 유입량을 기록한 관측자료에 따르면 전량 저류, 침투되어(유출량$${\frac{._-}{.}}$$0) 침투식 LID 시설로서의 고유한 기능적 목표를 달성하였으므로 설계 누적강우유출고 5mm는 타당하다고 판단된다. 침투도랑은 강우시 일시적으로 여과 및 저류과정에서 침수가 이루어지며 완전침투가 24시간 이내에 종료되므로 우드칩으로 부터 유기물질 등의 용출가능성은 희박하며 현장 모니터링 자료에서도 용출기미는 나타나지 않았다. 따라서 추후 침투도랑 설치기준의 개정시 국내외 연구자료를 바탕으로 여재로서 우드칩의 적용을 면밀히 검토할 필요가 있다.

• 한국환경복원기술학회지
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• 제4권3호
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• pp.55-65
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• 2001

The hydrological cycle system in the city is generally characterized by quick runoff, bad infiltration, low evaporation rate, and so on. It is caused by sealing greens up with pavements. Also, there are lots of contradictory environmental problems, such as inundation, the lack of underground water and dryness in the city, caused by the urban drainage system which is mostly focused on the quick draining off rainfall. In addition, the technique joining rain and sewage, which has more dangers of inundation, occupies 66% between two Korean drainage systems which consist of joining and dividing system. There has been some need to convert the present drainage system into the environmentally friendly hydrological cycle system. This is a theoretical study to examine some foreign cases and suggested applicable methods in our country, focusing on the environmentalyl friendly system of rainfall drainage. The precipitation treatment system can be made up of some possible phases choosing from premanagement, utilization, infiltration, retention, and inducement phases. Therefore, this study mostly focused on infiltration, retention, and inducement phases. It is necessary to suggest the multifunctional utilization of outdoor spaces, especially applying in new constructing and re-constructing residential estates.

• 한국물환경학회지
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• 제25권5호
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• pp.785-791
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• 2009

Using artificial rainfall simulator, the soil loss, which is deemed as the most cause of muddy water problem among Non-point source (NPS) pollutant, was studied by the analysis of direct runoff, groundwater discharge, and soil water storage properties concerned with rainfall intensity, slope of area, and land cover. The direct runoff showed increasing tendency in both straw covered and bared soil as slope increases from 5% to 20%. The direct runoff volume from straw covered surface were much lower than bared surface. The infiltration capacity of straw covered surface increased, because the surface sealing by fine material of soil surface didn't occur due to the straw covering. Under the same rainfall intensity and slope condition, 2.4~8.2 times of sediment yield were occurred from bared surface more than straw covered surface. The volume of infiltration increased due to straw cover and the direct runoff flow decreased with decrease of tractive force in surface. To understand the relationship of the rate of direct runoff, groundwater discharge, and soil water storage by the rainfall intensity, slope, and land cover, the statistical test was performed. It shows good relationship between most of factors, except between the rate of groundwater storage and rainfall intensity.