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송치용,남순성,천병식,Song, Chi-Yong,Nam, Soon-Sung,Chun, Byung-Sik 대한토목학회 1991 대한토목학회논문집 Vol.11 No.4
대수층에서 약액주입에 의한 차수효과를 검토하고자 동수조건을 변화시킬 수 있는 1.5 shot system의 특별주입장치에 의해 유속변화에 따른 시료토의 고결상태를 확인 조사하고, 약액의 내구성을 파악하기 위해 변수위투수시험에 의해 시간의 경과에 따른 투수계수변화를 측정하였다. 동수지반에서 차수효과(내구성)를 증대시키기 위해서는 약액의 지하수에 희석, 유실되지 않도록 유속에 반하여 gel-time을 짧게 하는 한편, 약액의 농도, 주입량(주입률) 및 주입속도를 높혀 주며, 반응율이 큰 경화제를 사용한다든지 약액 중의 수분을 작게 되도록 배합하는 등의 조치가 유효하며 직접적인 방안으로는 주입공의 간격을 좁히거나 주입열수를 늘리는 등의 대책이 필요하며 더욱 이들 제 계수는 실내주입시험 및 현장시험주입 등에 의한 자료를 바탕으로 결정함이 바람직하다. The purpose of this study is to examine the cut-off effect in aquifer by chemical grouting. Moreover, injection tests using specially prepared injection equipment of 1.5 shot system which hydrauric condition can be controlled are attempted to investigate the cut-off effect by confirming the gelling condition of samples according to the variation of flow velosity. And the permeability is measured according to changing of time by falling head test in order to consider the durability of grouts. Therefore to increase the cut-off effect in groundwater flow, shortening the gel-time according to the increasement of flow velocity, increasing the concentration and quantity of grouts(grouting ratio) according to the increasement of that, and as another direct method, contracting the distance between grouting holes or enlarging the grouting line should be done. These coefficients should be designed by data based on injection test in laboratory and field.
전기적 잡음이 심한 지역에서 지표-시추공 복합배열 탄성파탐사에 의한 암반등급 산정
김예련(Kim Ye Ryun),사상호(Sha Sang Ho),남순성(Nam Soon Sung),조철현(Jo Cheol Hyun),차영호(Cha Young Ho),박종범(Park Jong Bum),신경진(Shin Kyung Jin) 한국철도학회 2005 한국철도학회 학술발표대회논문집 Vol.- No.-
Rock mass classification by using electrical resistivity tomography(ERT) method is widely performed for the determination of rock support type in tunnel design. In the region of high electrical noise level, however, the result of the ERT will have many erroneous features. In this study, the back ground electrical noise had been measured to find out the reason why the results of ERT in this area did not agree to the expected geology confirmed by boreholes. In order to overcome this limitation of ERT, a hybrid surface-borehole array seismic refraction tomography had been followed. Using this technique, we could get P-wave velocity section including the depth level of tunnel. The comparison of the P-wave velocity and RMR shows fairly good statistical relationship to make it possible to set up the rock mass classification for the entire tunnel line.