• Title/Summary/Keyword: 투수량

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단일공에서 정압주입시험을 이용한 단열투수량계수 산출

  • Park Jun-Hyeong;Park Gyeong-U;Bae Dae-Seok;Kim Gyo-Won
    • Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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    • 2005.04a
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    • pp.288-291
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    • 2005
  • 방사성폐기물 처분연구의 일환으로 단열 암반지역의 지하수 유동에 있어서 각 단열조의 투수량계수를 알아보기 위하여 연구지역에 설치된 3기의 시추공에서 초음파 검층, 정압주입시험 및 유동차원 해석을 수행하였다. 단열은 방향성, 틈의 크기 등의 그 분포 특성으로 인해 각 시험구간내의 지하수 유동에 있어서, 유동형태 및 단열투수량계수를 좌우하므로 일반적으로 수리특성에 널리 이용되는 다공성매질의 연속체 개념을 통한 해석의 적용에 신중성을 고려할 필요가 있다.

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Numerical Experiments on the Evaluation of Effective Permeability and Tunnel Excavation in the Three Dimensional Fracture Network Model (3차원 균열연결망 모델에서의 유효투수계수 평가 및 터널굴착 지하수 유동해석에 대한 수치실험)

  • 장근무
    • Tunnel and Underground Space
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    • v.8 no.4
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    • pp.275-286
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    • 1998
  • The effective permeability and the representative element volume(REV) of fracture network model were evaluated based on the parameters such as permeability tensor, principal permeability and the direction of principal permeability. The effective permeability ranges between the harmonic mean and the arithmetic mean of the local permeabilities of subdivided blocks. From the numerical experiments, which were for investigating the influence of model volume on the variation of flux for the cubic models, it was found that the variation of flux became reduced as the model volume approached REV. The variation of groundwater flux into the tunnel in the fracture network model was mainly dependent on the ratio of the tunnel length to model size rather than REV. And it was found that groundwater flux into the tunnel was not completely consistent between the fracture network model and the equivalent porous media model, especially when the ratio of the tunnel length to model size is small.

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Runoff Reduction Effect Analysis of Porous Asphalt Using Rainfall Simulator of Movable-Assemble Type (이동형 강우모의장치를 이용한 투수성 아스팔트 유출저감 효과 분석)

  • Jang, Youngsu;Park, Jaerock;Chun, Jonghyun;Park, Jaehyun;Shin, Hyunsuk
    • Proceedings of the Korea Water Resources Association Conference
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    • 2018.05a
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    • pp.382-382
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    • 2018
  • 최근 기후변화 및 도시화로 인해 집중호우와 도시 내의 불투수층이 증가하고 있으며, 현재 도심의 강우관리시스템이 한계에 달하여 수재해 피해가 급증하고 있다. 이와 같은 문제를 해결하기 위한 방안으로 저영향개발 기법이 대두되고 있으며, 본 기법은 해당 지역의 강우를 분산식 빗물처리 하여 도시 내의 수문학적 특성을 개발이전 상태로 회복 및 유지하는 기술이다. 저영향개발 기법의 종류는 투수성 포장, 옥상녹화, 빗물정원, 식생저류지, 식생화분 등이 있다. 본 연구에서는 저영향개발 기법 중 하나인 투수성 아스팔트에 대한 우수저감 효과를 분석하기 위해 경상남도 양산시 부산대학교 양산캠퍼스 그린인프라 저영향개발 센터에서 주차장형 LID 시설의 투수성 아스팔트 포장과 대조군인 불투수 콘크리트 포장을 실험대상으로 선정하였다. 포장체는 $10.85m(L){\times}2.3m(B){\times}0.9 m(H)$의 크기로 원지반 침투가 없는 박스형 실험시설로써 이동형 강우모의장치를 이용하여 인공강우실험을 실시하였다. 강우모의 시에 발생하는 지표유출 및 침투유출은 각 유공관을 통해 모니터링 박스에 차집되어 실시간으로 웹사이트 상에 저장된다. 저장된 자료를 이용하여 투수성아스팔트의 첨두유출량 저감, 지체시간지연효과를 분석하였다. 분석된 결과를 통해 첨두유출량은 11%저감되었고 투수성 아스팔트와 불투수 콘크리트는 각각 3시간, 1시간 동안 유출되어 2시간의 차이를 보여준다.

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Analysis of Relationships Between Topography/Geology and Groundwater Yield Properties at Pohang using GIS (GIS를 이용한 포항시 지형 및 지질과 지하수 산출능력 간의 상관관계 분석)

  • Lee, Sa-Ro;Kim, Yong-Sung;Kim, Nam-Jin;Ahn, Kyoung-Hwan
    • Economic and Environmental Geology
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    • v.41 no.1
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    • pp.115-131
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    • 2008
  • The aim of this study is to analyze relationships between topography/geology which affects physically groundwater regime and groundwater yield properties in Pohang City using Geographic Information System (GIS). For the purpose, topographic factors such as ground elevation, ground elevation difference, ground slope, and ground regional slope, and hydrogeologic unit, and groundwater yield properties factors such as transmissivity, specific capacity, and well yield, were constructed to spatial data base. Then the relationships between topography, geology and groundwater yield properties were analyzed quantitatively using GIS overlay technique. As the results, ground-water yield of unconsolidated sediments and porous volcanic rocks is the highest among the hydrogeologic units of study area, and clastic sedimentary rock is the lowest. There are positive relationship between the elevation and elevation difference and the groundwater yield properties and negative relationship between the topographic slope and the groundwater yield properties.

Hydraulic Properties of Duksan Hot-spring Area (덕산온천 지역의 수리적 성질)

  • 함세영;조병욱;성익환
    • The Journal of Engineering Geology
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    • v.9 no.2
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    • pp.101-118
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    • 1999
  • The pumping test analysis on 28 pumping test data in Duksan hot-spring area was performed using the fractal model, the leaky fractal model, and the steady-state dual-porosity fractal model. The fractional flow dimension 1.9 or 2.0 was determined in the central put of the hot spring and the fractional flow dimension 1.5-1.7 in the marginal area. For the flow dimension 2.0, the correlation between the transmissivity and the productivity index by the aquifer loss was much better than that between the transmissivity and the specific yield by the total drawdown. On the other hand, for the flow dimension 1.9, the correlation between the generalized transmissivity and the productivity index was very similar to that between the generalized transmissivity and the specific yield.

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Aquifer Transmissivity Estimation with Kriging Techniques and Numerical Model in the LAN (Kriging기법과 수치모형에 의한 이안지구 대수층의 투수량계수 추정)

  • 조웅현;박영기;김환홍
    • Journal of the Korean Society of Groundwater Environment
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    • v.1 no.2
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    • pp.113-120
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    • 1994
  • One of the delicate problems in aquifer management is the identification of the spatial distribution of tile hydrological parameters. The observed data are insufficient to identify the distribution of transmissivities in LAN aquifer. To determine the distribution of the transmissivity in LAN aquifer, it would be required to transform the observed heads at the pilot points into transmissivities. Therefore, three procedures wire tackled for the identification of the spatial distribution of the hydrological parameters; geostatistical estimate of the parameter field on the basis of known well point, heads reconstructed by a numerical model, and modification of the values at pilot points by a minimization algorithm. The variogram of Kriging has been applied to a total of 258 transmissivity value in attempt to quantify their distribution of LAN aquifer. Variogram of the observed and optimized transmissivities at pilot points are adapted to the exponential form. So, it is fitted by theoretical one with coefficients of w=0.623, a=2.743. Values of head obtained through numerical analysis are adjusted to the observed values so that heads have been transformed completely into the transmissivities at the observation wells. The procedure represented contour map of the estimated transmissivities and the calculated head.

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균열 대수층의 정호 함양 시험

  • 석희준;김형수;백건하;정수은;김진삼
    • Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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    • 2004.04a
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    • pp.443-446
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    • 2004
  • 이동장수 먹는샘물 공장부지내에 파쇄대에 위치한 관정에서 인공수압파쇄 및 인공함양 시험을 실시하여 대수성 산출 증대효과와 저장 증대효과를 살펴보았다. 인공수압파쇄 시험은 두개의 관정(MW-2, O-7)에 실시하였고, 마찬가지로 인공함양 시험도 다른 두개의 관정(O-7a, MW-7)에 대해서 실시하였다. 또한 대수성 산출능의 효과를 살펴보기 위하여 인공수압파쇄 및 인공함양시험 전후에 각각 양수 시험을 실시하여 비양수량, 투수계수, 및 수위강하를 구하였다. 따라서 사전 사후 대수성 시험 비교 결과 인공수압파쇄 시험에서는 평균적으로 약 367 %의 투수계수의 증가율과 271 %의 비양수량의 증가를 나타내었다. 마찬가지로 인공함양 시험 결과 O-7a는 약 110%의 투수계수의 증가와 약 75%의 비양수량의 증가를 보였다. 반면에 MW-7는 거의 변화가 없었다. 인공함양시험은 인공수압파쇄시험보다 낮은 투수계수 증가율을 보이거나 거의 변화를 일으키지 못했지만 주변에 있는 관정에 주입압과 비슷한 양상를 갖는 수위변화를 일으키는 것으로 보아서 함양된 주입수가 주변의 대수층에 널리 퍼져 있을 것으로 추측된다.

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Estimation of WEPP's Parameters in Burnt Mountains (산불지역의 WEPP 매개변수 추정)

  • Park, Sang-Deog
    • Journal of Korea Water Resources Association
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    • v.41 no.6
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    • pp.565-574
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    • 2008
  • Fire-enhanced soil hydrophobicity often increases runoff and erosion in the mountain hillslope following severe wildfires. Estimation techniques for WEPP's parameters were studied in burnt mountain slopes. In burnt mountain slopes, the model over-predicted runoff in the small runoff and under-predicted runoff in the great runoff, and in the lower sediment runoff it had a tendency to over-predict soil loss. The effective hydraulic conductivity was most sensitive in the WEPP's runoff and its sediment runoff was mainly effected by the effective hydraulic conductivity, initial saturation, rill erodibility, and interrill erodibility. To improve the applicability of the WEPP, the adjustment coefficient of effective hydraulic conductivity was defined for runoff and the adjustment coefficient of rill erodibility and interrill erodibility was presented for sediment runoff. The adjustment coefficient of effective hydraulic conductivity in wildfire mountain slopes increased with maximum rainfall intensity of single storm and the vegetation height index. The adjustment coefficients of rill erodibility depended on soil components of size distribution curve and total rainfall depths in single storm. The adjustment coefficients of interrill erodibility decreased with increases of maximum rainfall intensity and vegetation height index. These results may be used in the application of WEPP model for wildfire mountain slopes.

Characteristics of Aquifer System and Change of Groundwater Level due to Earthquake in the Western Half of Jeju Island (제주도 서반부의 대수층 체계와 지진에 의한 지하수위 변동 특성)

  • Ok, Soon-Il;Hamm, Se-Yeong;Kim, Bong-Sang;Cheong, Jae-Yeol;Woo, Nam-Chil;Lee, Soo-Hyoung;Koh, Gi-Won;Park, Yun-Seok
    • Economic and Environmental Geology
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    • v.43 no.4
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    • pp.359-369
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    • 2010
  • This study characterizes aquifer system and hydrogeologic property in the western half of Jeju Island where wells were drilled for regional water supply in three sub-areas (northwestern, western, and southwestern sub-areas). The aquifer system of the northwestern sub-area is largely composed of upper high-permeability layer, upper low-permeability layer, lower high-permeability layer, and lower low-permeability layer. On the other hand, the aquifer systems of the western and southwestern sub-areas are mostly composed of upper low-permeability layer, high-permeability layer, and lower low-permeability layer. Transmissivity and specific capacity decrease in the order of the northwestern, western, and southwestern sub-areas. The relationship between specific capacity and the top surface of tuff is negative with a high correlation coefficient of -0.848, indicating that the tuff acts as the bottom of the aquifer. Groundwater level change due to the 2004 Sumatra earthquake is an average of 23.74 cm in the northwestern sub-area, an average of 9.48 cm in the western sub-area, and none in the southwestern sub-area. Further, it is found that groundwater change due to the earthquake has a positive relationship with transmissivity and specific capacity.

A modification of SWMM to simulate permeable pavement, and the effect analysis on a release of treated wastewater and the permeable pavement (투수성 포장을 고려한 SWMM의 수정 및 하수처리 재이용수와 투수성 포장의 효과분석)

  • Lee, Jung-Min;Lee, Sang-Ho;Lee, Kil-Seong
    • Journal of Korea Water Resources Association
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    • v.39 no.2 s.163
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    • pp.109-120
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    • 2006
  • Permeable pavement and release of treated wastewater into streams can increase streamflow of urban streams for a dry weather period. A SWMM code was modified to have a permeable pavement option. The modified SWMM was applied to continuous simulations of urban runoff from Hakuicheon watershed and it was used to analyse the effect of a permeable pavement installation and the reuse of treated wastewater. A critical error in the pan coefficient multiplication was also corrected in the modification. The analysis results of the reuse of treated wastewater is as follows: The low flow ($Q_{275}$) increases by 1.63 times as much as the current one and the drought flow ($Q_{355}$) increases by 3.57 times as much as the current one. If the impervious area in the Hakuicheon watershed is replaced with the permeable pavement area by 10 percent, the low flow and the drought flow increases by 3 percent and 17 percent, respectively. The results shows the effectiveness of the release of treated wastewater into stream to increase urban streamflow. The permeable pavement installation also play a minor role in the drought flow increase.