• 한국문화재보존과학회:학술대회논문집
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• 한국문화재보존과학회 2004년도 제20회 발표논문집
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• pp.15-24
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• 2004

The Seokgatap pagoda composed of mainly alkali granite and other minor pink-feldspar granite, fine-grained granite, granodiorite, diorite, gabbro, and tuff. Despite the small loss and damage derived from joints, its peel-off and exfoliation are serious enough to cause the heavy deterioration on the stone surface. The chemical and petrological weathering has partly replaced the original rock-forming minerals with clay minerals and iron oxyhydroxides. Based on the petrogenesis, rock materials of the pagoda is very similar to rocks of Dabotap pagoda and the Namsan granite in the Gyeongju. The central fart of the pagoda has sunken highly, which caused all the corners to split and the structural transformation to become worse. The reverse V-shaped gaps between the materials have broken stones filled in a coarse way. The iron plates inserted between the upper flat stone laid on other stones and tile pagoda body in the north and east side has been exposed in the air and corroded, discoloring of the adjacent stones. The overall diagnosis of the Seokgatap pagoda is the deteriorated functions of the stone materials, which calls for a long-term monitoring and plans to reinforce the stone surfaces. But the main body including the pagoda roof stone needs washing on a regular basis, and the many different cracks should be fixed with glue by using the fillers or hardeners designed for stone cultural properties after removing the cement mortar. In case of the replacement of the stone materials with new stones, it's necessary to examine the pagoda for the center of gravity and support intensity of the materials. The structural stability of the pagoda can be attained by taking a reinforce measure in geotechnical engineering and making a drainage. The ground humidity, which has aggravated weathering and structural instability, should be resolved by setting up a humidity reduction facility. The contamination of lichens and bryophyte around the pagoda and on the surface is serious. Thus biochemical treatments should be given too in order to prevent further biological damages and remove the vegetation growing on the discontinuous planes.

• Korean Chemical Engineering Research
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• 제45권3호
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• pp.304-309
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• 2007

본 연구에서는 감압법 및 열자극법에 의한 메탄하이드레이트 생산실험을 수행하기 위해 고압의 다중공 평판형 셀기기를 설계 제작하였다. 이 실험장비를 이용하여 고투과성 미고결 시료 공극시스템에서 감압법과 열자극법에 의한 생산실험을 수행하여 생산메카니즘을 분석하였다. 감압법에 의한 생산실험 결과, 일반 가스전과는 달리 하이드레이트 해리에 의한 공극내에서의 소스효과로 인해 일시적으로 압력이 상승하고 또한 흡열반응으로 인해 온도가 하강함을 확인 하였으며, 열자극 생산실험을 수행한 결과에서는 감압법의 경우 열자극법에 비해 해리속도가 느리게 진행되어 가스생산이 낮은 상태로 지속되는 것으로 나타났다. 한편, 열자극법 중 열을 가한 후 곧바로 생산하는 경우, 주입지점 주변에서만 해리되고 또한 그 지역에서만 투과도가 커지는 것으로 나타났으며, 생산초반 이후 해리속도는 soaking까지 시행한 경우에 비해 해리가 느리게 진행됨을 알 수 있다. 한편, 본 연구의 낮은 하이드레이트 포화도를 갖는 미고 결시료 공극시스템에서 열자극법의 적정 soaking 시간 규명실험을 통해 압력과 생산거동을 고찰하였다. 그 결과, 6분간 soaking 한 경우, 온도 하강에 의한 하이드레이트의 재형성으로 2분 및 4분간 soaking한 경우보다 낮은 회수율을 보였다. 본 연구의 실험결과는 향후 높은 하이드레이트 포화도를 갖는 고결 시료 공극시스템에서의 실험을 통해 더욱 확연히 드러날 것으로 예상된다.

• Geomechanics and Engineering
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• 제7권3호
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• pp.263-277
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• 2014

In the conventional design of retaining structures in a seismic zone, seismic inertia forces are commonly assumed to act upwards and towards the wall facing to cause a maximum active thrust or act upwards and towards the backfill to cause a minimum passive resistance. However, under certain circumstances this design approach might underestimate the dynamic active thrust or overestimate the dynamic passive resistance acting on a rigid retaining structure. In this study, a new analytical method for dynamic active and passive forces in c-${\phi}$ soils with an infinite slope was proposed based on the Rankine earth pressure theory and the Mohr-Coulomb yield criterion, to investigate the influence of seismic inertia force directions on the total active and passive forces. Four combinations of seismic acceleration with both vertical (upwards or downwards) and horizontal (towards the wall or backfill) directions, were considered. A series of dimensionless dynamic active and passive force charts were developed to evaluate the key influence factors, such as backfill inclination ${\beta}$, dimensionless cohesion $c/{\gamma}H$, friction angle ${\phi}$, horizontal and vertical seismic coefficients, $k _h$ and $k_v$. A comparative study shows that a combination of downward and towards-the-wall seismic inertia forces causes a maximum active thrust while a combination of upward and towards-the-wall seismic inertia forces causes a minimum passive resistance. This finding is recommended for use in the design of retaining structures in a seismic zone.

• 자원환경지질
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• 제33권2호
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• pp.117-128
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• 2000

Regional evaluations of slope stability by the failure criterion and by environmental geological factors were conducted. The failure criterion is the general conditions for plane failure which consider the geometrical conditions between geological discontinuities and topographical slope planes. The factor focused in this condiction is dip and dip direction. Geostatics, named semivariogram was used for establishing structural domains in slope stability evaluation by the failure criterion. The influential range was calculated to 6 km in the case of dip direction of dominant joint set and 7 km in the case of dip of the same dominant joint set. Then applying this failure criterion to the study area produced a slope stability map using the established domains and slopes generated by TIN module of ARC/INFO GIS. This study considered another regional slope stability analysis. 5 failure-driven factors 9the unstable slope map, geology, engineering soil, groundwater, and lineament density) were selected and used as data coverages for regional slope stability evaluation by geoenvironmental factors. These factors were weighted and overlayed in GIS. From the graph of cumulatave area (%) and instability index, finding critical points classified the instability indices. The most unstable slopes are located in the southern area of Mt. Eorae, Dabul-ri, and the eastern area of Junkok-ri in the first area is plane failure. Also, the expected orientations of failure are 59/338 and 86/090 (dip/dip direction).

• 한국환경과학회지
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• 제24권4호
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• pp.481-494
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• 2015

Groundwater level hydrographs from observation wells in Jeju island clearly illustrate distinctive features of recharge showing the time-delaying and dispersive process, mainly affected by the thickness and hydrogeologic properties of the unsaturated zone. Most groundwater flow models have limitations on delineating temporal variation of recharge, although it is a major component of the groundwater flow system. Recently, a convolution model was suggested as a mathematical technique to generate time series of recharge that incorporated the time-delaying and dispersive process. A groundwater flow model was developed to simulate transient groundwater level fluctuations in Pyoseon area of Jeju island. The model used the convolution technique to simulate temporal variations of groundwater levels. By making a series of trial-and-error adjustments, transient model calibration was conducted for various input parameters of both the groundwater flow model and the convolution model. The calibrated model could simulate water level fluctuations closely coinciding with measurements from 8 observation wells in the model area. Consequently, it is expected that, in transient groundwater flow models, the convolution technique can be effectively used to generate a time series of recharge.

• Environmental Engineering Research
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• 제10권6호
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• pp.294-305
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• 2005

The effectiveness of fly ash-, quicklime-, and quicklime-fly ash-based stabilization/solidification(S/S) in chromium(Cr) contaminated soils was investigated using modified semi-dynamic leaching tests. Artificial soil samples composed of kaolinite or montmorillonite contaminated with chromium nitrate(4000 mg $Cr^{3+}\;kg^{-1}$ of solid) were prepared and then subjected to S/S treatment using quicklime, fly ash, or quick lime-fly ash. The effectiveness of the treatment was evaluated by assessing the cumulative fraction of leached $Cr^{3+}$ as well as, by computing the effective diffusivity ($D_e$) and the leachability index (LX) of the treated samples. The reduction in $Cr^{3+}$ release for the untreated samples was more pronounced in the presence of montmorillonite, which was attributed to sorption. Treatment with quicklime, fly ash, or quick lime-fly ash was significantly effective in reducing $Cr^{3+}$ release most probably due to the formation of pozzolanic reaction products and $Cr(OH)_3$ precipitation. The most effective treatment was observed in montmorillonite-sand soil samples treated with quicklime-fly ash (99.8% removal). The mean $D_e$ decreased significantly and the mean LX was greater than 9 for all treated samples, indicating that the treated soils were acceptable for "controlled utilization". The mechanism controlling $Cr^{3+}$ leaching from all treated samples during the first 5 days appeared to be diffusion.

• Environmental Engineering Research
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• 제10권3호
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• pp.112-121
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• 2005

The effectiveness of quicklime-based stabilization/solidification (S/S) in immobilizing lead (Pb) was assessed by performing semi-dynamic leaching tests (ANS16.1). In order to simulate landfill leaching conditions, the ANS 16.1 test was modified by using 0.014 N acetic acid (pH = 3.25) instead of distilled water. Artificial soil samples as well as field soil samples contaminated with Pb were tested. The effectiveness of quicklime treatment was evaluated by determining diffusion coefficients ($D_e$) and leachability indices (LX). A model developed by de Groot and van der Sloat was used to elucidate the controlling Pb leaching mechanisms. Overall, upon quicklime treatment Pb leachability was significantly reduced in a]l of the samples tested. The mean LX values were higher than 9 for an artificial soil sample containing 30% kaolinite treated with 10% quicklime and for a field soil sample treated with 10% quicklime, which suggests that S/S treated soils can be considered acceptable for "controlled utilization". Moreover, quicklime treatment was more effective in artificially contaminated soil with high kaolinite content (30%), indicating the amount of clay plays an important role in the success of the treatment. The controlling Pb leaching mechanism was found to be diffusion, in all quicklime treated samples.

• Korean Chemical Engineering Research
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• 제45권5호
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• pp.515-522
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• 2007

본 연구에서는 가상의 "흑곰-HY" 가스전을 대상으로 상용저류전산시뮬레이터인 "ECLIPSE 300"을 사용하여 가스저장전으로 전환에 대비한 기술적 타당성을 평가하고자 하였다. 이 저류층의 매장량은 143 BCF로서 소규모 가스전이며, 공극률과 투과도는 각각 19.5%와 50 md로 가스의 순환이 원활이 이루어질 수 있는 비교적 양호한 저류층이다. 이 저류층에 대하여 가스저장전으로의 전환시 핵심적 검토항목인 쿠션가스 양, 저장전으로의 전환시점, 운영사이클 변경, 가스정의 수 및 수평정 적용 가능성 등에 대한 분석을 수행하였다. 분석결과, "흑곰-HY" 가스저장전에서 안정적인 가스저장을 위해서는 쿠션가스가 최소한 50% 이상이 되어야 함을 알 수 있었다. 또한 가스를 더 오랜기간동안 생산하기 위해 잔류가스를 적정 쿠션가스 양보다 적게 남겨두어도 추가로 쿠션가스만 주입하면 기술적으로는 아무 문제가 없는 것으로 나타났다. 한편, 가스를 5개월 대신 동절기 3개월간만 재생산하는 운영사이클의 경우에는 쿠션가스를 60% 이상으로 높여주거나 가스정의 수를 늘려야만 재생산이 가능한 것으로 나타났다. 가스정의 수에 대한 분석결과에서는 6개와 8개인 경우에는 저류층내 잔류가스가 증가하여 정상적인 재생산이 불가능하므로 "흑곰-HY" 가스전에서는 최소 10개의 수직가스정이 운영되어야 함을 알 수 있었다. 이에 반해 2개의 기존 수직정에 3개의 수평정을 추가로 시추하게 되면 비교적 안정적인 주입과 재생산이 가능한 것으로 산출되었다.

• Korean Chemical Engineering Research
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• 제45권6호
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• pp.638-647
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• 2007

본 연구에서는 회수증진기법 중 하나인 $CO_2$ 공법을 생산유전에 적용할 경우, 적용성 여부를 간단하고 정량적으로 평가할 수 있도록 하기 위한 평가차트를 개발하였다. 이 평가차트는 소스의 이용성, $CO_2$-오일의 혼합도, 저류층 및 오일 특성의 적정성, 주입기법의 평가항목으로 구성되어 있다. 저류층 및 오일의 특성에서 오일 비중, 오일 점성도, 오일 포화도, 저류층 온도 및 투과도의 기본평가항목에 대해서는 점수로 평가되며, $CO_2$ 순도, 저류층 두께 및 경사도 등의 추가평가항목에 대해서는 상 중 하로 구분하여 정량적으로 평가된다. 또한 미서블공법의 주입기법 평가에서는 지층경사, 수직투과성 및 저류층 두께 등에 따라 연속주입공법과 WAG($CO_2$) 공법의 여부가 정성적으로 평가된다. 이와 같이 구성된 평가차트에 대해 $CO_2$ 공법이 성공적으로 수행된 51개 유전의 적용사례를 분석하여 이를 토대로 $CO_2$ 공법이 가능한 추천점수를 설정하였다. 본 연구에서 개발한 평가차트를 국내 기업이 참여중인 스코틀랜드의 캡틴 생산유전과 베네수엘라의 오나도 생산유전에 적용하여 $CO_2$ 공법의 적용 가능성 여부를 평가하였다. 여기서 캡틴 유전은 저류층의 공극률과 투과도가 매우 양호하나, $C_{21+}$ 이상의 무거운 탄화수소 함유량이 54%를 넘는 중질유이다. 따라서 이러한 중질오일은 $CO_2$와 비미서블공법으로 진행되므로 비미서블공법 기준하의 기본평가항목에 대해서만 평가한 결과 비미서블 $CO_2$ 공법이 적정한 것으로 평가되었다. 한편, 베네수엘라의 오나도 유전에 대해서는 최소 미서블압력이 저류층 압력보다 낮게 산출되어 미서블 $CO_2$ 공법이 적용 가능할 것으로 평가되었다.

• 한국광물학회지
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• 제23권3호
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• pp.211-217
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• 2010

스카른 Zn-Pb-Cu 복합광석을 구성하는 주요 구성 광물의 정량분석을 목적으로, 마이크로 포커스 X-ray 단층촬영 장비를 이용한 스카른 복합광석의 3차원 비파괴검사를 수행하였다. X-ray 단층화상의 화상결함을 감소시키고자 제안된 화상보정법을 이용하여 화상들을 보정한 후에 3차원으로 재구성하였다. 주사전자현미경(SEM)에 의한 표면분석과 보정된 X-ray 단층화상을 비교하여 주요광물에 대한 CT 값의 범위를 결정하였다. 재구성화상 내 전체 광물의 체적비율을 분석한 결과, 황화광물 20.5%, 맥석광물 79.5%로 평가되었다. X-ray 3차원 단층화상 정량분석법은 광석 내 유용광물의 부존형상과 회수율 분석에 유용하게 적용될 것으로 기대된다.