• Title/Summary/Keyword: 미고결층

Search Result 64, Processing Time 0.03 seconds

Hydrogeological Properties of Uunconsolidated Formations and Bedrocks in the Central Area of Busan Metropolitan City (부산 도심지역 미고결층과 기반암의 수리지질 특성)

  • Hamm Se-Yeong;Cha Yong-Hoon;Cheong Jae-Yeol
    • The Journal of Engineering Geology
    • /
    • v.15 no.4 s.42
    • /
    • pp.407-421
    • /
    • 2005
  • This study aims to investigate hydrogeological properties of the central area from Yangjeong-Dong to Sujeong-Dong in Busan Metropolitan City. For this study, pumping tests were carried out in the bedrock aquifer of Yangjeong-Dong and the unconsolidated aquifer near Busanjin railway station. The pumping test in the bedrock aquifer containing the Dongrae fault revealed specific hydraulic characteristics with respect to the fault. The pumping test in the unconsolidated aquifer revealed the hydrogeologic properties of both coastal landfill and fine sediments. It was found that the Moench's sphere-shaped dual-porosity model fits the bedrock aquifer, whereas the Neuman's uncofined aquifer model accords with the unconsolidated aquifer. The average transmissivity and storage coefficient of the bedrock aquifer are $2.75{\times}10^{-5}m^2/s\;and\;6.41{\times}10^{-5}$ and those of the unconsolidated aquifer are $8.24{\times}10^{-4}m^2/s\;and\;3.70{\times}10^{-3}$, respectively. On the other hand, slug tests gave average transmissivity and storage coefficient values of $9.84{\times}10^{-4}m^2/s\;and\;1.21{\times}10^{-2}$, respectively.

In situ iron/manganese removal and permeability improvement at the river bank filtration site (강변여과수내 철망간 저감 및 투수성 개선)

  • Kim, Byung-Woo;Kim, Byung-Goon;Hur, Young-Teck;Kim, Dong-Sup;Kim, Hong-Suck
    • Proceedings of the Korea Water Resources Association Conference
    • /
    • 2018.05a
    • /
    • pp.228-228
    • /
    • 2018
  • 강변여과는 지하수 인공함양 방식 중 유도함양(induced recharge) 또는 간접함양 방식에 속한다. 이는 하천 및 강변 부근에 집수시설을 설치한 후, 미고결층 대수층(unconsolidated aquifer)의 자연 오염 저감능을 이용하여 지표수를 간접 취수하는 방식으로 수질이 불량한 지표수가 대수층을 관류하면서 희석, 화학적 이온 교환 및 반응, 흡착, 생물막(biofilm; 미생물에 의한 자연저감), 여과 등을 통하여 수질이 개선된다. 강변여과수내의 용존 농도가 높은 철과 망간은 수처리 비용증가, 용수관정 및 시설물의 수명단축을 초래한다. 따라서 강변여과 지역의 미고결 대수층에서 효과적인 철과 망간 동시 제거(vyredox)를 위해 에어서징(air surging)과 블록 서징(block surging)을 실시하기 위해서 실내 물탱크 모델(water tank model)에서 에어서징에 따른 공기 순환 우물시스템을 관찰하였으며, 이를 바탕으로 현장시험(Test bed)에 적용하였다. 미고결 대층수층에서의 철 망간은 음용수 기준치(각각 0.3 mg/L)를 초과하고 있으며, 강변여과 취수 개발 및 이용을 제한하는 요인이 되고 있다. 본 연구에서 사용된 에어서징과 블록서지 기술은 자갈층 및 미고결 대수층에 충진된 슬라임 및 폐색(clogging)을 제거함과 동시에 관정 주변의 대수층의 투수성 개선과 산화환경으로 치환되며, 대수층에 잔존하는 철/망간의 산화물들을 관정내로 빼낼 수 있는 방법이다. 따라서 서징에 따른 폐색 제거효율을 검토한 결과에서 철 망간 이온농도 저감효과와 관정 주변의 수리전도도(hydraulic conductivity) 및 저류계수(coefficient of storage)가 증가한 것으로 나타났다. 이와 같이 강변여과에 의한 폐색은 미고결층내 공기주입 및 블록서지를 통하여 철/망간 이온농도 저감 및 수리특성 개선 효과에 유용한 것으로 평가된다.

  • PDF

Case Study on Design and Construction of Rock Structures in Cenezoic Zone (신생대 지층에서의 암반구조물 설계 및 시공 사례)

  • Park, Do-Hyun;Kim, Je-Kyung;Park, Chi-Myeon;Kim, Young-Geun
    • Proceedings of the Korean Geotechical Society Conference
    • /
    • 2005.10a
    • /
    • pp.247-267
    • /
    • 2005
  • 이암층 역암층 그리고 화산암층과 같은 특수지질 불량구간에서 터널과 암반사면의 합리적인 시공을 달성하기 위해서는 먼저 대상지질에 대한 지질조건과 암반특성을 정확히 이해하는 것이 필요하며, 이를 바탕으로 지반특성에 적합한 보강대책을 수립하도록 하여야 한다. 본 고에서는 포항지역과 경주지역에서의 미고결 이암 및 역암층 그리고 제주도 화산암층에서의 암반 구조물에 대한 설계 및 시공사례를 검토하고 전형적인 미고결 지층으로 알려진 신생대 지층에서의 터널과 암반과 같은 암반구조물에 대한 설계 및 시공상의 제반 문제점을 고찰하므로서 이에 대한 합리적인 대책을 수립하고자 하였다.

  • PDF

Rock Classification and Aggregate Evaluation of Tertiary Unconsolidated Deposits (미고결 퇴적층의 암반분류와 재료원 평가)

  • Kim, Sung-Wook;Lee, Kyu-Hwan
    • Journal of the Korean Geotechnical Society
    • /
    • v.26 no.7
    • /
    • pp.25-36
    • /
    • 2010
  • Tertiary unconsolidated mudstones spread throughout the eastern coast area. The demand for high quality filling materials in these areas is increasing due to harbors and large-scale residential land development. Rock produced in-situ or near site has been used as road subbase construction or reclamation materials for economical reason, but it is hard to decide appropriateness of quality specification because of its characteristics. The test results showed that unconsolidated rocks are diversely considered according to a different method of the applied geotechnical investigation. Therefore, the site of tertiary unconsolidated mudstones, the classification of rock and evaluation of rock properties that must be evaluated by objective criteria and apply a different set of criteria are needed. In addition, the environmental impact must be considered due to acid mine drainage.

Engineering Properties of Uncemented Mudrock from Yeoju Area, Gyeonggi-Do (경기도 여주지역 미고결 이암의 공학적 특성)

  • Ban, Hoki;Lee, Huiyoun;Bae, Kyujin;Cho, Wanjei
    • Journal of the Korean GEO-environmental Society
    • /
    • v.16 no.12
    • /
    • pp.53-58
    • /
    • 2015
  • Engineers should take great care of characterizing the engineering properties of mudrock, because the uncemented mudrock can be considered as a hard rock in appearance. Therefore, the mudrock samples obtained from the cut slope in Gyeongki-do were tested to evaluate the strength characteristics of uncemented mudrock in this study. The performed tests are index properties, slake durability, and swelling tests for the classification of the mudrock for engineering practice. To evaluate the effect of water on the engineering properties of the uncemented mudrock, resonant column, triaxial compression and direct shear tests with various water contents were performed. With the increasing water contents, stiffness at very small to small strain region and the cohesion value of the strength parameters decrease. Based on the test results, engineers should take great care of evaluating the engineering properties of uncemented mudrock.

Problems in Construction of Tunnel and Rock . Slope at Mudstone and Shale Resion (이암/셰일 지역에서의 터널 및 사면 시공시의 문제점)

  • 이내용;김용일;정한중;김영근
    • Proceedings of the Korean Geotechical Society Conference
    • /
    • 2002.11b
    • /
    • pp.115-140
    • /
    • 2002
  • 이암층, 함탄층, 석회암층과 같은 특수지질불량구간에서 터널과 암반사면의 합리적인 시공을 달성하기 위해서는 먼저 대상지질에 대한 지질특성, 암반특성을 정확히 이해하는 것이 필요하며, 지반특성에 적합한 지보대책을 수립하도록 하여야 한다. 본고에서는 전형적인 퇴적암지층으로 알려진 포항지역중 중생대 퇴적암류로부터 신생대 제 3기의 미고결 퇴적암류에 이르는 다양하고 복잡한 지질구조를 이루고 있는 지역에서의 터널 및 암반사면의 시공사례를 통하여 시공중의 제반문제점을 검토하여 이암층에서의 안전하고 합리적인 터널/암반사면의 시공방안에 대하여 고찰하였다.

  • PDF

Evaluation of Cementation Effect of Jeju Coastal Sediments (제주연안 퇴적층의 고결 평가)

  • Lee, Moon-Joo;Kim, Jae-Jeong;Shim, Jai-Beom;Lim, Chai-Geun;Lee, Woo-Jin
    • Journal of the Korean Geotechnical Society
    • /
    • v.25 no.11
    • /
    • pp.105-115
    • /
    • 2009
  • The Jeju sand was sampled from the beach in Jeju Island and its basic properties were analyzed. The cementation effect of Jeju coastal sediments was evaluated from in-situ tests such as SPT, CPT, and the Suspension-PS test. It was shown from test results that the Jeju sand has high extreme void ratios due to the angularity of grains and the intra-particle voids of hollow particles, similar to typical calcareous sands. From cone penetration test in the calibration chamber, it was found that the cone resistance($q_c$)-relative density($D_R$)-vertical effective stress(${\sigma}_v'$) relation of Jeju sand almost matches that of high compressible quartz sand. However, the $q_C-D_R-{\sigma}_v'$ correlation suggested for uncemented Jeju sand overestimates the relative density of coastal sediments of Jeju Island due to the cementation effect. From the analysis of the relation of cone resistance, N value, and small strain shear modulus measured in-situ, it seems reasonable to assume that the coastal sediment of Jeju Island is a naturally cemented one.

Geological Significance of Liquefaction and Soft-sediment Deformation Structures (액상화와 연질퇴적변형구조의 지질학적 의미)

  • Ghim, Yong Sik;Ko, Kyoungtae
    • Economic and Environmental Geology
    • /
    • v.52 no.5
    • /
    • pp.471-484
    • /
    • 2019
  • Liquefaction occurs by a temporal loss of sediment strength as a consequence of increased pore water pressure during the re-arrangement of unconsolidated, granular sediments. Liquefaction is dependent on the physical properties of the sediments and cause surface cracks, landslide, and the formation of soft-sediment deformation structures(SSDS). SSDS is formed by the combined action of the driving force and deformation mechanism(liquefaction, thixotropy, and fluidization) that is triggered by endogenic or exogenic triggers. So research on the SSDS can unravel syndepositional geological events. If detailed sedimentologic analysis together with surrounding geological context suggest SSDS formed by earthquakes, the SSDS provide a clue to unravel syndepositional tectonic activities and detailed paleoseismological information(> Mw 5) including earthquakes that leave no surface expression.