• Journal of the Korean Vacuum Society
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• v.4 no.2
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• pp.183-188
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• 1995

고에너지(50-200KeV)로 가속된 이온을 모재표면에 물리적으로 투입하므로써 표면의 조성 및 조직을 변화시키는 공정인 이온주입기술을 이용하여 경량고강도소재로 각광받고 있는 AI2218 합금의 재식성 향상을 연구하였다. 질소이온주입은 DuoPIGatron 이온원을 사용하여 가속전압 100KeV, 조사량 $1{\times}10^{17}ions/\textrm{cm}^2$~$5{\times}10^{17}ions/\textrm{cm}^2$의 조건으로 행하였으며 AI합금의 열화를 방지하기 위하여 시편온도를 $60^{\circ}C$이하로 유지하였다. 질소이온 주입재의 재식성 평가를 위하여 3.5% NaCI 용액에서 양극분극시험 및 5% NaCI 용액에서 염수분무시험을 행하였다. Auger Electron Spectroscopy와 Transmission Electron Microscopy을 이용하여 표면의 질화물형성 여부를 조사하였으며, Scanning Electron Microscopy을 이용하여 부식된 표면을 관찰하였다. AI2218합금에 질소이온을 주입한 결과 표면에 미세한 AIN 석출물을 형성하였으며 이러한 질화물형성에 의해 공식(pitting)발생을 억제하고 부식전류밀도를 감소시켜 내식성이 향상되었다.

• Economic and Environmental Geology
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• v.44 no.2
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• pp.123-133
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• 2011

The lab scale experiments to investigate the geochemical reaction among supercritical $CO_2$-mineral-brine which occurs at $CO_2$ sequestration sites were performed. High pressurized cell system (l00 bar and $50^{\circ}C$) was designed to create supercritical $CO_2$ in the cell, simulating the sub-surface $CO_2$ storage site. From the high pressurized cell experiment, the surface changes of Ca-feldspar, amphibole (tremolite) and olivine, resulted from the supercritical $CO_2$-mineral-brine reaction, were observed and the dissolution of minerals into the brine was also investigated. The mineral slabs were polished and three locations on the surface were randomly selected for the image analysis of SPM and the surface roughness value (SRV) of those locations were calculated to quantify the change of mineral surface for 30 days. At a certain time interval, SPM images and SRVs of the same mineral surface were acquired. The secondary minerals precipitated on the mineral surfaces were also analyzed on SEM/EDS after the experiment. From the experiments, the average SRV of Ca-feldspar increased from 2.77 nm to 20.87 nm for 30 days, suggesting that the dissolution of Ca-feldspar occurs in active when the feldspars contact with supercritical $CO_2$ and brine. For the amphibole, the average SRV increased from 2.54 nm to 8.31 nm and for the olivine from 0.77 nm to 11.03 run. For the Ca-feldspar, $Ca^{2+}$, $Na^+$, $Fe^{2+}$, $Si^{4+}$, $K^+$ and $Mg^{2+}$ were dissolved in the highest order and $Si^{4+}$, $Ca^{2+}$, $Fe^{2+}$ and $Mg^{2+}$ for the amphibole. Fe (or Mg) - oxides were precipitated as the secondary minerals on the surfaces of amphibole and olivine after 30 days reaction. Results suggested that $Ca^{2+}$, $Fe^{2+}$ and $Mg^{2+}$ rich minerals would be significantly weathered when it contacts with the supercritical $CO_2$ and brine at $CO_2$ sequestration sites.

• The Journal of Engineering Geology
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• v.15 no.1
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• pp.1-8
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• 2005

As a trial to find an efficient technique for determining hydraulic conductivity, a test application of electrical conductivity measurement technique was made using a signal conditioning data acquisition system in borehole. The experiment was made in two test boreholes BM-2 and BM-3 which are located in the Experiment forests of Kangwon National University in Bongmyongri, Chunchon. We obtained series of electric conductivity variation curves after the beginning and completion of saline water injection using these two bore-holes as the pumping well and the observing well alternatively, The analysis of time series electrical conductivity data suggests kinds of valuable information about aquifer properties by holes and depths, and we could confirm the potential of this method as an efficient tool for in situ aquifer test.

• Journal of the Korean Recycled Construction Resources Institute
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• v.9 no.2
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• pp.191-199
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• 2021

In this study, the correlation between the influencing factors on corrosion and Half Cell Potential(HCP) measurement was analyzed considering the three levels of W/C ratio, cover depth, and chloride concentration. The HCP increased with enlarged cover depth, so it was confirmed that the increment of cover depth was effective for control of corrosion. Based on the criteria, the case of 60mm cover depth showed excellent corrosion control with under -200mV, indicating increase of cover depth is an effective method for reducing intrusion of external deterioration factors. When fresh water was injected to the upper part of specimens, very low level of HCP was monitored, but in the case that concentrations of chloride were 3.5% and 7.0%, HCP dropped under -200mV. In addition, the case with high volume of unit binder showed lower HCP measurement like increasing cover depth. Multiple regression analysis was performed to evaluate the correlation between the corrosive influence factors and HCP results, showing high coefficient of determination of 0.97. However, there were limitations such as limited number of samples and measuring period. Through the additional corrosion monitoring and chloride content evaluation after dismantling the specimen, more reasonable prediction can be achieved for correlation analysis with relevant data.

• Proceedings of the Korean Vacuum Society Conference
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• 2013.02a
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• pp.335-335
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• 2013

최근 다기능 소재의 개발이 필요함에 따라 서로 상반되는 2가지 이상의 물성을 동시에 구현할 수 있는 소재의 개발이 요구되고 있다. 4 성분계 물질을 단일 타겟으로 제조함으로써 다수의 타겟을 이용하는 기존 PVD 방법의 복잡성과 재형성 등의 문제점을 해결하고 다기능성을 구현할 수 있는 코팅막을 제조할 수 있게 된다. 본 연구에서는 제조된 4 성분계 모물질을 UBM 최근 다기능 소재의 개발이 필요함에 따라 서로 상반되는 2가지 이상의 물성을 동시에 구현할 수 있는 소재의 개발이 요구되고 있다. 4 성분계 물질을 단일 타겟으로 제조함으로써 다수의 타겟을 이용하는 기존 PVD 방법의 복잡성과 재형성 등의 문제점을 해결하고 다기능성을 구현 할 수 있는 코팅막을 제조할 수 있게 된다. 본 연구에서는 제조된 4 성분계 모물질을 UBM 스퍼터링법을 이용하여 질화 공정을 도출하였고 질소 함량에 따른 물리적 특성 및 박막의 특성에 대해 연구하였다. BMG (Bulk Metallic Glass) 타겟을 이용하여 마그네트론 스퍼터링법으로 박막을 코팅하였다. 시편은 Si wafer, SUS 그리고 부식 특성 평가를 실시하기 위하여 냉연강판을 사용하였다. 시편은 아세톤, 알코올로 각각 10분간 초음파 세척한 후 진공장비에 장착하여 Ar 분위기에서 글로우 방전으로 청정을 30분간 실시하였다. 시편청정이 끝나면 ~$10^{-6}$ Torr까지 진공 배기를 실시하고 Ar 가스를 주입하여 2.5 mTorr로 진공도를 유지하여 스퍼터링으로 박막 코팅을 실시하였다. 스퍼터링 파워는 약 0.6 kW (2.0 A)으로 고정하였고 질소 유량은 0~10 SCCM으로 변화시켜 BMG 박막을 코팅하였다. 질소가 첨가된 BMG 박막에서는 시편의 색상이 노란빛으로 나타났으며 이것은 타겟의 조성 중 가장 많이 함유되어있는 Zr이 질화되어 색상의 변화가 일어난 것으로 판단된다. BMG 코팅을 위해서 진공용기로 주입한 질소의 유량이 소량인 경우에도 BMG 코팅층에 비교적 많은 양의 질소가 존재하였고 일정량 이상에서는 BMG 코팅층에 존재하는 질소의 양이 포화되는 현상을 보였다. 질소 유량 3, 4 SCCM의 BMG 코팅층에서 ZrN (111), ZrN (200) Peak이 관찰되었다. BMG 코팅층의 경도 측정결과 Bias 50 V 인가 시 ~22 Gpa로 경도가 가장 높았다. BMG 코팅층의 내부식 특성을 평가하기 위해 염수분무 시험을 실시하였고 ~$10{\mu}m$의 두께를 갖는 BMG 코팅층에서 염수분무 시작 후 48시간 만에 적청이 발생하였다.

• 한국지구물리탐사학회:학술대회논문집
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• 2008.10a
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• pp.141-144
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• 2008

Geological storage of carbon dioxide has been studying in advanced countries to reduce greenhouse gases and a pilot site for geological storage is also in operation in the deep saline aquifer. Seismic wave and electrical resistivity tomography methods are applicable to monitoring techniques and they are used to evaluate the distribution range and behavior of the carbon dioxide injected in the porous sandstone formations. This paper describes the construction of an experimental apparatus which consists of a high pressure vessel and a measurement system for geological storage of carbon dioxide. The experiment apparatus will be used to measure seismic velocities and resistivities during the injection of carbon dioxide at the supercritical phase in the porous sandstones.

• Economic and Environmental Geology
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• v.43 no.4
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• pp.371-379
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• 2010

Fresh water injection test in a fractured bedrock aquifer was applied as an efficient approach to lower saline concentrations in the saltwater-freshwater transition zone formed by seawater intrusion in a coastal area. The methodology and effectiveness of fresh water injection for hydraulically controlling seawater intrusion is overwhelmingly site dependent, and there is an urgent need to characterize the permeable fractures or unconsolidated porous formations which can allow for seawater flow and transport. Considering aquifer characteristics, injection and monitoring boreholes were optimally designed and completed to inject fresh water through sand layer and fractured bedrock, respectively. We devised and used the injection system using double packer for easy field operation and maintenance. Overall fracture distribution was systematically identified from borehole image logs, and the section of fresh water injection was decided from injection test and monitoring. With fresh water injection, the fluid electrical conductivity of the monitoring well started to be lowered by the inflow of fresh water at the specific depth. And this inflow leaded to the replacement of the fluid in the upper parts of the borehole with fresh water. Furthermore, the injection effect lasted more than several months, which means that fresh water injection may contribute to the mitigation of seawater intrusion in a coastal area.

• Proceedings of the Korean Vacuum Society Conference
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• 2013.02a
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• pp.384-384
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• 2013

본 연구에서는 e-beam 증착을 이용하여 Al, Mg 단일 금속으로 다층형 Al-Mg 코팅층을 제조하여 특성 분석 및 내식성을 평가하였다. Al-Mg 코팅층은 99.99%의 Al, 99.9%의 Mg grain을 사용하여 E-Beam 가열을 통해 냉연강판 위에 코팅하였다. 증발물질과 기판과의 거리는 48 cm이며, 기판은 세척을 실시한 후 진공 챔버에 장착하고 ~10-5 Torr 까지 진공배기를 실시하였다. 진공챔버가 기본 압력까지 배기되면 아르곤 가스를 주입하고 기판홀더에 800 V의 직류 전압을 인가하여 약 30분간 글로우 방전 청정을 실시하였다. 기판의 청정이 끝나면 아르곤 가스를 차단하고 코팅층의 구성형태에 따라 Al 또는 Mg을 코팅하였다. 다층형 Al-Mg 코팅층은 2층에서 최대 6층까지 제조하였으며 $3{\mu}m$의 두께를 기준으로 Al과 Mg 코팅층의 두께비가 각각 1:1 과 2:1이 되도록 코팅하였다. 6층 이상에서는 코팅층의 두께 제어가 쉽지 않기 때문에 층수는 6층으로 제한하였다.다층형 Al-Mg 코팅층을 주사전자현미경으로 관찰한 결과, Al-Mg 코팅층간의 계면을 관찰할 수 있었다. 또한 글로우방전분광기로 Al-Mg 코팅층을 관찰한 결과, Al과 Mg 코팅층이 균일한 다층 구조를 형성하고 있는 것을 확인할 수 있었다. 다층의 Al-Mg가 코팅된 강판을 염수분무시험을 통해서 내부식 특성을 확인하였다. Al-Mg 코팅 강판의 염수분무시험 결과, Al-Mg 코팅층의 층수가 증가할 수록 내부식 특성이 향상되는 것을 확인할 수 있었으며, 이러한 현상은 Al-Mg 코팅층이 다층으로 형성되어 있어 부식 생성물을 효과적으로 차단하여 강판의 부식을 방지한 것으로 판단된다.

• Journal of Korean Society of Environmental Engineers
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• v.28 no.6
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• pp.603-612
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• 2006

The study with laboratory sandbox model has been carried out to address potential use of reclaimed water, as a way for artificially recharging the coastal aquifer, to effectively prevent from seawater intrusion. To do this, we assessed hydraulic and geochemical properties depending upon various extraction and recharging conditions. While solely being recharged, the intrusion could be significantly retarded than those of recharge and extraction implied together. At 0.5 to 2 for the ratio of the extraction over the recharge rate, the fresh water was exploited from the tank, where the void regime was simultaneously saturated with the recharged water. In the meantime, the saline water zone was diluted and back-tracked by the recharged water due to forming a hydraulic geochemical barrier around the injection well. However, if the ratio was being increased to greater than 4, saltwater more deeply intruded to the freshwater zone because the artificial recharge was not sufficiently supplied to timely back-fill the void space. When the aquifer water was intermittently extracted at the ratio of $0.5{\sim}2$ over the recharge rate, the value of S.M.I. decreased, but increasing it to more than 4 unlikely escalated the value of S.M.I as much as $3{\sim}47%$ indicating that the salt water intruded. It finally revealed that the proper ratio of extraction/recharge or intermittent extraction would efficiently retracted seawater intrusion while the freshwater sources could be conservatively utilized.

• Economic and Environmental Geology
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• v.42 no.5
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• pp.403-412
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• 2009

The objective of this study is to investigate the geochemical change of feldspar minerals by supercritical $CO_2$, which exists at $CO_2$ sequestration sites. High pressurized cell system (100 bar and $50^{\circ}C$) was designed to create supercritical $CO_2$ in the cell and the surface change and the dissolution of plagioclase and orthoclase were observed when the mineral surface reacted with supercritical $CO_2$ and water (or without water) for 30 days. The polished slab surface of feldspar was contacted with supercritical $CO_2$ and an artificial brine water (pH 8) in the experiments. The experiments for the reaction of feldspar with only supercritical $CO_2$ (without brine water) were also conducted. Results from the first experiment showed that the average roughness value of the plagioclase surface was 0.118 nm before the reaction, but it considerably increased to 2.493 nm after 30 days. For the orthoclase, the average roughness increased from 0.246 nm to 1.916 nm, suggesting that the dissolution of feldspar occurs in active when the feldspars contact with supercritical $CO_2$ and brine water at $CO_2$ sequestration site. The dissolution of $Ca^{2+}$ and $Na^+$ from the plagioclase occurred and a certain part of them precipitated inside of the high pressurized cell as the form of amorphous silicate mineral. For the orthoclase, $Al^{3+}$, $K^+$, and $Si^{+4}$ were dissolved in order and the kaolinite was precipitated. In the experiments without water, the change of the average roughness value and the dissolution of feldspar scarcely occurred, suggesting that the geochemical reaction of feldspars contacted with supercritical $CO_2$ at the environment without the brine water is not active.