• 제목/요약/키워드: Ground water level

검색결과 602건 처리시간 0.032초

Assessment of health risk associated with arsenic exposure from soil, groundwater, polished rice for setting target cleanup level nearby abandoned mines

  • Lee, Ji-Ho;Kim, Won-Il;Jeong, Eun-Jung;Yoo, Ji-Hyock;Kim, Ji-Young;Lee, Je-Bong;Im, Geon-Jae;Hong, Moo-Ki
    • 한국토양비료학회지
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    • 제44권1호
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    • pp.38-47
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    • 2011
  • This study focused on health risk assessment via multi-routes of As exposure to establish a target cleanup level (TCL) in abandoned mines. Soil, ground water, and rice samples were collected near ten abandoned mines in November 2009. The As contaminations measured in all samples were used for determining the probabilistic health risk by Monte-Carlo simulation techniques. The human exposure to As compound was attributed to ground water ingestion. Cancer risk probability (R) via ground water and rice intake exceeded the acceptable risk range of $10^{-6}{\sim}10^{-4}$ in all selected mines. In particular, the MB mine showed the higher R value than other mines. The non-carcinogenic effects, estimated by comparing the average As exposure with corresponding reference dose were determined by hazard quotient (HQ) values, which were less than 1.0 via ground water and rice intake in SD, NS, and MB mines. This implied that the non-carcinogenic toxic effects, due to this exposure pathway had a greater possibility to occur than those in other mines. Besides, hazard index (HI) values, representing overall toxic effects by summed the HQ values were also greater than 1.0 in SD, NS, JA, and IA mines. This revealed that non-carcinogenic toxic effects were generally occurred. The As contaminants in all selected mines exceeded the TCL values for target cancer risk ($10^{-6}$) through ground water ingestion and rice intake. However, the As level in soil was greater than TCL value for target cancer risk via inadvertent soil ingestion pathway, except for KK mine. In TCL values for target hazard quotient (THQ), the As contaminants in soil did not exceed such TCL value. On the contrary, the As levels in ground water and polished rice in SD, NS, IA, and MB mines were also beyond the TCL values via ground water and rice intake. This study concluded that the health risks through ground water and rice intake were greater than those though soil inadvertent ingestion and dermal contact. In addition, it suggests that the abandoned mines to exceed the risk-based TCL values are carefully necessary to monitor for soil remediation.

현장계측에 의한 지반거동 분석 (Ground Movement Analysis by Field Measurements)

  • 전용백;조상완
    • 한국산업융합학회 논문집
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    • 제8권3호
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    • pp.161-168
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    • 2005
  • This study is analysis for adjacent structures and ground movement by deep excavation work. Underground Inclinometer has shown that deformation of increment is minor within to allowable limit. According to the measurements result of slope and crack for adjacent structures, a detached house showed bigger than hospital structure to deformation of increment. Variation of underground water level didn't effect so much to ground and adjacent structures movement because underground water flows in rock and didn't give the water press to propped walls. Measurement data of strut variation is within tolerance limit. Because excavation site's wall was strengthened suitably. This study will contribute in establishment of measurement standard and information-oriented construction during deep excavation in multi-layered ground including rock masses.

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TDR센서를 이용한 제방의 포화도 및 지하수위 해석 (Analysis of Saturation and Ground Water level in The Embankment Using TDR Sensor)

  • 박민철;김기영;이재호;한희수
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2010년도 추계 학술발표회
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    • pp.404-415
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    • 2010
  • In this paper, using the TDR sensors, variation of soil water content changes were measured as TDR data. Then filtering technique was determined using Fourier transform. Determine the moisture content of soil and ground water level and tried to determine unsaturated zone. First, variation of water content changes were measured TDR data by indoor experiment. Then as a function of TDR data made for water content of soil. Next, through Acrylic indoor laboratory model experiments, changes in ground water levels and lateral penetration of the field conditions were reproduced in an indoor. Field applicability of the TDR sensor was demonstrated by analysis of this. TDR sensor was installed in the embankment, TDR data were measured by TDR sensor.

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온도계측을 통한 교량 세굴 및 수위 측정방법 (New measuring method for the scour and the water level by temperature measurement)

  • 주봉철;박기태;황윤국
    • 한국콘크리트학회:학술대회논문집
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    • 한국콘크리트학회 2009년도 춘계 학술대회 제21권1호
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    • pp.553-554
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    • 2009
  • 광섬유센서 등과 같은 정밀온도센서를 이용하여 기온, 수온 및 수중 지표면 온도를 측정하고, 각각의 온도 변화에 대응하여 교량 세굴 및 수위를 파악할 수 있는 계측시스템을 개발하고 이를 소개한다. 온도계측을 통한 교량 세굴 및 수위 측정 방법은, 온도를 측정할 수 있는 센서를 수중 지표면을 기준으로 일정깊이와 높이로 설치하여 각각의 위치에 따른 온도 변화량을 분석하여 세굴량을 추정하는 시스템이며, 센서를 교각 상부까지 연장할 경우 수심 측정까지도 가능한 방법이다.

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3차원 지반모델링 기반의 지반함몰 위험 지반 레이어 개발 방법 (A Method of Developing a Ground Layer with Risk of Ground Subsidence based on the 3D Ground Modeling)

  • 강정구;강재모;박준환;문두환
    • 한국지반환경공학회 논문집
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    • 제22권12호
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    • pp.33-40
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    • 2021
  • 도심지에서 빈번하게 발생하는 지반함몰 사고는 지하시설물의 노후화, 지하개발 활동에 따른 지반의 교란과 지하수 변화 등 다양한 원인에 의해 발생하고 있다. 지반함몰 위험을 사전 예측하기 위해서는 지반함몰 사고에 영향을 미치는 인자들에 대한 지반 공학적 및 수리학적 검토가 필요하다. 따라서 본 연구에서는 현재 운영되고 있는 지반조사 데이터 및 지하수위 변동 정보를 이용하여 지반함몰이 발생한 연구대상 지역의 3차원 지반모델링 및 월별 지하수위에 대한 자료 분석을 수행하였으며, 이를 활용해 실제 지반함몰 발생 이력과 지반조건 및 지하수위 변화와의 관계성을 확인하였다. 또한, 기존 시추정보에서 통일 분류 체계(USCS)에 따라 제시된 흙의 공학적 특성을 지반함몰과 연관된 공학적 지표인 흙의 내부 침식 민감도로 재구성하여 지반함몰 위험도를 가시화하는데 활용하는 방법론을 제시하였다. 연구결과, 지반함몰 발생 지역의 지반은 내부 침식이 취약한 모래(SM, SC, SP, SW)가 40% 이상 구성되어 있음을 확인했으며, 지하수위 변화에 따른 지반함몰 발생빈도와의 관계성도 확인할 수 있었다.

TDR센서를 이용한 제방의 포화도 및 지하수위 해석 (Analysis of Saturation and Ground Water Level at Embankment by TDR Sensor)

  • 김기영;한희수;이재호;박민철
    • 한국지반공학회논문집
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    • 제27권2호
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    • pp.63-72
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    • 2011
  • 본 논문은 TDR센서를 이용하여, 지반 내 지하수의 거동을 계측하고 이를 이동 평균법과 푸리에 변환을 통한 필터링 기법으로 포화 및 불포화 영역의 구분 및 변화를 수치적으로 결정하고자 하였다. 먼저 실내실험을 통하여 포화도 변화에 따른 TDR데이터의 변화를 계측하고 이를 포화도에 대한 함수로 만들었다. 다음으로 아크릴 실내모형실험을 통하여 현장의 지하수위 변화 및 측방 침투조건을 재현하고 이에 대한 TDR데이터 변화를 계측한 후 해석하여, TDR센서의 현장 적용을 위한 계측자료 교정함수를 만들었다. 이 후 현장 제방에 TDR센서를 설치하고 지하수위를 변화시켜 가며 지반의 지점별 포화도를 파악함으로써 지하수위 및 건조, 불포화영역을 결정하였다.

지하수위 변화에 따른 지반함몰 영향연구 (Influence Ground Sinking with Variation of Ground Water Level)

  • 김숙자;정관수
    • 한국재난정보학회 논문집
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    • 제14권4호
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    • pp.399-408
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    • 2018
  • 연구목적: 최근 들어 도심지를 중심으로 빈번하게 발생하는 지반함몰은 인명 및 경제적 피해를 야기하여 사회적으로 큰 이슈가 되고 있다. 지반함몰 또는 도로함몰은 일반적으로 불리는 싱크홀과는 다른 원인으로 작용하고 있다. 석회암 지반이 용해되어 침식이 일어나는 싱크홀과는 달리 지반함몰 및 도로함몰은 지하수가 흙 사이로 빠져나가게 되면서 공동이 발생하게 되고 이완 및 확장이 진행되어 상부지반이 붕괴되는 현상을 말한다. 지반의 공동화는 집중호우시 침입수에 의한 공동 형성, 지하수위 상승 및 하강에 의한 토사유실 및 하수유출반복에 의한 공동 형성이 주된 원인이다. 연구방법: 본 연구에서는 지하수 모델링을 통하여 지하구조물 공사시 지하수 흐름을 검토하였다. 연구결과: 지하수 모델링결과 지하수는 하천방향으로 흐르는 것으로 분석되었으며, 이에 따른 지반함몰의 영향은 미미한 것으로 확인되었다. 결론: 지하수위 저하 및 흐름방향에 따른 지반함몰보다는 지층을 구성하는 입자의 구성에 영향을 받는 것으로 분석되었다.

에너지플러스 시뮬레이션을 통한 하천수 열원 히트펌프 시스템의 적용 가능성 분석 (An Applicability Analysis of River Water Source Heat Pump System using EnergyPlus Simulation)

  • 손병후
    • 한국지열·수열에너지학회논문집
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    • 제18권2호
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    • pp.10-21
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    • 2022
  • A water source heat pump (WSHP) system is regarded as an energy-efficiency heating and cooling supply system for buildings due to its high energy efficiency and low greenhouse gas emissions. Recently, water sources such as river water, lake water, and raw water are attracting attention as heat sources for a heat pump system in Korea. This paper analyzed the applicability of a river water source heat pump system (RSHP). The river water temperature level was compared with the outdoor air and ground temperature levels to present applicability. In addition, the cooling and heating performance were compared through a simulation approach for the RSHP and a ground source heat pump (GSHP) applied to a large-scale office building. To compare the temperature level, the actual data were applied to the river water and the outdoor air, while the simulation results were applied to the ground circulation water. The results showed that the change in river water temperature throughout the year was similar to the change in outdoor air temperature. However, unlike the outdoor air temperature, the difference between the hourly and daily average river water temperatures was not large. The temperature level of river water was lower during the heating season and somewhat higher during the cooling season than that of the ground circulation water. Finally, the performance of the RSHP system was 13.4% lower than that of the GSHP system on an annual-based.

충남지역의 지하수개발에 관한 조사 (Research on the Ground Water Developement in the Region of Choong Nam Province)

  • 민병섭
    • 한국농공학회지
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    • 제11권4호
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    • pp.1827-1831
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    • 1969
  • Resulties of research on the capacity of ground water of 994 concrete-pipe-wells and 97 infiltration-gallerys in ground-water-developement-works region executed from March to Julyin 1969, in Choong Chung Nam Do, and research on the quality of ground water for 88 wells for home-use around of River Geum Area, are as fellows: (1) Thickness of aquifer is no more than 2.85m averagely even at river-overflowed plain, alluvial plain and valley plain area that are estimated to contain ground water mostly. And so, it is guessed that ground water capacity is not much especially. (2) Soil of aquifer of the above area is sand or gravel and it is estimated to be good for ground water developement and its mean permeability coefficient is bout $2.5{\times}10^{-3}$(m/sec), and its porosity is about 33.9%. (3) The quality of ground water is good for irrigation water exception of delta plain area. Warm water plan is to need for irrigation water when water temperature is less than 19 degrees below zero. (4) Prospect of ground water developement, judging from quality and quantity, expects to lay infiltration gallery under the ground at river bed in order to utilize under-flow-water of river bed, river-overflowed plain, alluvial plain and valley plain that ground level is less than 50m. (5) Collectable water volume of under-flow-water of river bed is about 450 to $750m^3/day$ to be able to irrigate 3ha to 5ha of the cultivated land in case that infiltration gallery length is 50m and its depth is about 5m. (6) Collectable water volume at river-overflowed plain, alluvial plain and valley plain area, is estimated $150m^3/day$ to be able to irrigated 1ha of the cultivated land.

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토조실험에 의한 투수성 포장재의 수문학적 요소 분석 (Analysis of Hydrological Factor for Permeable Pavement by using Soil Tank Experiment)

  • 전상미;이정민;박재현;이상호
    • 한국물환경학회지
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    • 제25권2호
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    • pp.181-192
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    • 2009
  • In this study, the hydrological properties of permeable pavement were analyzed by the experiment and the numerical simulation. The numerical model used was a modified SWMM especially for considering the hydrological response of permeable pavement. The parameters of modified SWMM were revised by the experimental results, and then the practicability was evaluated through the comparison of the experimental and numerical simulation results. In the experiments, three different rainfall intensities such as 65 mm/hr, 90 mm/hr, 95 mm/hr were supplied for 4 hrs, and the hydraulic properties including surface outflow, subsurface outflow, ground water level, soil water contents were measured for 10 hrs. The results showed rainfall intensity effected directly on surface outflow volume and subsurface outflow volume was more effected by ground water level than rainfall intensity. The ground water level and the soil water contents were under estimated as compared with the experimental data except the portion of occurring direct runoff. The surface and subsurface outflow discharge were simulated very well in comparison with the experimental data. Consequently, the modified SWMM could be used very effectively to evaluate the hydrological property of permeable pavement.