• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.419-419
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• 2019

우리나라에서는 인공하천 중심의 개발에서 자연형 하천 복원으로 변화가 진행 중이다. 이에 따라 강우 발생에 따른 하도와 식생의 빈번한 변동이 발생하고 있다. 하천 내의 하도와 식생은 물과 유사의 상호작용을 바탕으로 형성되는 하상 형태로 하도와 식생의 변동은 건강한 하천을 나타내는 하나의 지표이다. 특히 하도와 식생은 하천의 흐름에 영향을 주고 다시 하천의 흐름은 하도와 식생에 영향을 주고받기 때문에 하천 흐름 특성에 핵심적인 요소로 볼 수 있다. 따라서 이에 대한 장기간의 모니터링이 필요하며 이에 따른 수위-유량관계를 규명할 필요가 있다. 본 연구에서는 만경강 유역에 위치한 완주군(용봉교)관측소를 대상으로 2017년부터 2018년까지 식생 및 하도 모니터링을 통한 수위-유량관계 변화를 분석하였다. 2017년에는 식생의 활착, 성장, 소멸에 따라 9개의 기간분리가 발생하였으며, 2018년에는 8개의 기간분리가 발생하였다. 2017년은 저수위1로 시작하여 성장 및 소멸을 반복하다 저수위3으로 회귀하였으며, 2018년은 2017년 저수위 3으로 시작하여 성장과 소멸을 반복하다 저수위9로 회귀하는 특성을 보여 주었다. 결과적으로 본 연구에서는 하천 내의 식생과 하도 변화에 대한 장기 모니터링과 흐름 특성이 변화하는 기간의 유량측정성과 확보를 통한 신뢰도 높은 수위-유량관계곡선식을 개발하였고 이를 통해 생산된 유량자료는 정확도가 매우 높은 것으로 분석되었다.

• Journal of IKEEE
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• v.23 no.1
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• pp.338-341
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• 2019

In this paper, we propose a novel ESD device with improved characteristics of LVTSCR, which is a representative ESD protection device, and verify the N-stack technology for design optimized for each required voltage of a specific application. The characteristics of the holding voltage and the trigger voltage, which are the main parameters, are examined and the temperature characteristic, which is an indicator of the tolerance characteristic, is also verified. well region and a parasitic NPN to form a series-connected structure. We used synopsys' T-cad simulation tool for characterization.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.376-376
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• 2020

최근의 기후변화는 이미 한반도에 평균온도의 상승과 강수량의 변화 등으로 인해 많은 수문기상학적 변화를 일으키고 있다. 낮은 빈도의 가뭄은 2~3년에 한번 꼴로 발생할 정도로 빈번하게 발생하고 있으며, 국지적인 폭우와 한반도에 영향을 미치는 태풍의 증가 등 이수와 치수측면에서의 강수의 변화는 예측하기에 어려운 정도로 그 변화의 속도가 빨라지고 있는 현실이다. 이에 수자원활용 측면에서도 기후변화를 고려하여 새롭게 평가하여야 한다. 특히나 낮은 빈도의 잦은 가뭄은 농업분야에서 용수를 공급하는 데 있어 여러 가지 문제점들을 발생시키고 농업용수 확보를 위한 대책이 필요하다. 대부분의 농업용수는 하천취수, 저수지, 지하수를 이용하고 있으며, 뚜렷한 용수원이 없는 농경지의 대부분은 지하수를 이용하는 것이 보통이다. 이러한 지하수는 물 순환 체계에서 강수에 의해 지하로 침투된 물이 토양간이나 지하대수층 등에 저류되어 지하수가 형성된다. 일반적으로 가뭄이 발생하면 우선적으로 선택되는 대책이 지하관정을 개발하여 활용하는 방안이 활용되고 있는 데 강수의 부족으로 인한 가뭄 발생시 지하수위는 어떻게 변화하는지에 대한 연구과 관측이 필요하다. 본 연구에서는 강수자료와 지하수위 그리고 강수를 활용하는 가뭄지표인 표준강수지수(SPI) 등의 자료를 활용하여 가뭄발생과 지하수위의 변동성의 상관관계를 검토하였다.

• Journal of the Korean GEO-environmental Society
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• v.16 no.4
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• pp.13-22
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• 2015

The combined impact of Dissolved Organic Matter (DOM) fouling and inorganic ($CaSO_4,Ca_3(PO_4)_2$) scaling on the retention of TNT (2, 4, 6-Trinitrotoluene), RDX (Hexahydro-1, 3, 5-trinitro-1, 3, 5-triazine) and HMX (1, 3, 5, 7-Tetranitro-1, 3, 5, 7-tetrazocane) explosive contaminants by nano-filtration membrane were studied, since organic fouling and salt scaling are the major limitations for membrane filtration. Results reported here indicate that DOM fouling layer with a humic acid does not necessarily lead to an immediate loss of permeate flux but can result in a severe impact on the flux loss when both humic acid and inorganic scaltants were presented simultaneously. The $Ca_3(PO_4)_2$ mixed with humic acid showd most sever flux loss (42%) compared to that of only humic acid presence (8%). It could be a result that the scaling formation of the NF membrane was dominated by cake layer formation of DOM and it was along with pore blocking by the formation of crystals inside the porous active matrix of the NF membrane. In addition, these results indicated that the membrane selectivity of the explosives retention trended correlated with respect to increasing explosives size (listed by MW) based on greater steric interactions and followed the order (MW, g $mol^{-1}$; removal, %): HMX (296.15; 83%) ${\gg}$ RDX (222.12; 49%) ≋ TNT (227.13; 32%). Because the scaling and fouling layer could lead to a additional cake-enhanced concentration polarisation effect, the retention of explosives with the presence of humic acid in the feed solution and inorganic scaling formation on top of an organic fouling layer do not differ substantially retention from that of pure DI feed and NaCl solution.

• Journal of the Mineralogical Society of Korea
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• v.15 no.3
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• pp.221-230
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• 2002

Weathering of biotite shows a biotite-vermiculite-kaolinite sequence at the early stage, but presents biotite-kaolinite sequence without a significant intermediate phase (vermiculite) at the late stage from the weathering profile of the granitic gneiss. Secondary 1:1 phyllosilicates are kaolinite and halloysite which show different weathering textures originated by a different formation mechanism. Kaolinitization began from the edges of biotite and propagated toward the interior of grain along a multilayered front. $10 \AA$ layers of biotite are interleaving with $7\AA$ layers of kaolinite and c-axis of two phases is consistent. Kaolinite pseudomorph of biotite is isovolumetric, compared to the biotite boundary and includes many band-like porosities parallel to the cleavage. Platy kaolinite formed by 1:1 layer fur layer replacement of biotite. Halloysitization proceeded outward from the grain edges which were foliated as fine flakes and bent at the right angle for cleavage Halloysites were extensively fanning out and greatly increased the volume of grain. This indicated that halloysite tubes were formed by epitaxial overgrowth on the surface of biotite with import of Si and Al from the external solution by dissolution of plagioclase. These halloysites have abnormally high Fe content ( ~11%).

• Journal of Life Science
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• v.29 no.6
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• pp.645-652
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• 2019

Non-small cell lung cancer (NSCLC) has the infamous distinction of being the leading cause of global cancer-related death over the past decade, and novel molecular targets are urgently required to change this status. We previously conducted a microarray analysis to investigate the association of transcription factor activating enhancer-binding protein 2C (TFAP2C) with NSCLC and revealed its oncogenic roles in NSCLC development. In this study, to identify new biomarkers for NSCLC, we focused on several oncogenes from the microarray analysis that are transcriptionally regulated by TFAP2C. Here, the cell division cycle 20 (CDC20) and tribbles pseudokinase 3 (TRIB3) were subsequently found as potential potent oncogenes as they are positively regulated by TFAP2C. The results showed that the mRNA and protein levels of CDC20 and TRIB3 were down-regulated in two NSCLC cell lines (NCI-H292 and NCI-H838), which were treated with TFAP2C siRNA, and that the overexpression of either CDC20 or TRIB3 was responsible for promoting cell viability in both NSCLC cell lines. In addition, apoptotic levels of NCI-H292 and NCI-H838 cells treated with TFAP2C siRNA were found to be suppressed by the overexpression of either CDC20 or TRIB3. Together, these results suggest that CDC20 and TRIB3 are positively related to NSCLC tumorigenesis and that they should be considered as potential prognostic markers for developing an NSCLC therapy.

• Journal of the Korean GEO-environmental Society
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• v.13 no.11
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• pp.27-35
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• 2012

The discontinuity of rock is one of important elements that have impact on the dynamic movement of rock. A slope made of gneiss has complicated geological structure because of the gneiss forming process through metamorphism covering wide range and the anisotropic structure with foliation. In this study, before cutting slope, the rock of slope had been found as a good quality by the boring test. But during construction tension cracks had occurred in the section with 170m length during large-scale excavation work with depth more than 20m. Ground surface geological investigation, boring exploration, resistivity logging and borehole image processing had been done to find the causes of the tension crack. It was possible to estimate the scale of fault existing in large area through resistivity logging and geological investigation. Large scale slickenside and fault clay had been found as the result of comprehensive analysis.

• Clinical and Experimental Reproductive Medicine
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• v.16 no.2
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• pp.119-130
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• 1989

본 연구는 생식주기중 폐쇄여포액내에서 생물학적， 면역학적 특성을 나타내는 GTH 의 변화를 조사하고 steroid hormone과의 상관관계를 조사하며 국부조절인자로서 의 GTH의 역 활을 조사하고자 하였다. 가임기간중 215개의 여포와 IVF과정에서 185개의 여포를 얻어 여포액내 GTH의 생물학적 또는 면역학적 활성을 측정하였다. Bioactive LH(bLH)는 생쥐의 Leydig cell-testosterone production assay, bFSH는 흰쥐의 Sertoli cell aromatase assay로 측정 하였 다. Immunological GTH(iLH , iFSH) 는 MaiaClone RIA , Delfia kits를 사용하였다. 여포액내 iLH, iFSH , ihCG 는 hyperstimulation에 의해 형성된 여포의 크기와는 무관하였다. 또 hMG, huFSH 의 처리와도 상관성이 없었다. T의 농도가 높은 여포액내의 iFSH는 현저히 낮았으며 E, P 가 고농도인 여포의 ihCG 양은 현저히 낮았다. 과배란이 유도된 난소의 여포액내 iLH는 LH specific RIA로 측정시 3mIU/ml 이하이었다. 생식주기중 여포액내 bLH, bFSH는 배란기에 현저히 증가 하였다. 혈청내 GTH B/I ratio는 엘정한 반면 여포액내 LH，FSH의 생물학적， 면역학적 활성은 미수정란을 가지거나 폐쇄된 여포내의 활성보다 현저하게 높았다. 위의 결과로 보아 여포액내 생식소자극호르온은 면역학적활성보다 높은 생물학적 활성을 가지며， 생리적 현상의 지표가 된다고 추론된다. 또한 steroid, bGTH는 여포의 선택， 폐쇄를 구분하는 지표로 사용가능하며， 여포가 폐쇄될때 여포액내 B/I ratio가 현저히 낮아지는 것으로 보아 GTH의 활성이 감소되는 것으로 판단된다.

• Journal of the Korean Geographical Society
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• v.43 no.5
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• pp.701-714
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• 2008

This study examines the prevailing synoptic-scale mechanisms favorable for long-lived summer Persistent Positive Temperature Anomalies (PPTAs) as well as winter PPTAs in the United States. Such long-lived PPTAs usually occur in the south-central region of the United States in summer, but in the southwestern part of the United States in winter. Composite analyses of surface and pressure level data demonstrate that the formation of both winter and summer PPTAs is closely related to the movement of subtropical high pressure systems in the Pacific Ocean and Atlantic Ocean, respectively. The occurrence of long-lived summer PPTAs usually coincides with an extremely stable atmospheric condition caused by persistent blocking by mid- to upper-tropospheric anticyclones. Significant surface forcing is also easily identified through relatively high Bowen ratios at the surface. Warm air advection is, however, weak and appears to be an insignificant element in the formation of long-lived summer PPTAs. On the other hand, synergistic warming effects associated with adiabatic heating under an anticyclonic blocking system as well as significant warm air advection characterize the favorable synoptic environments for long-lived winter PPTAs. However, the impact of surface forcing mechanisms on winter PPTAs is insignificant.

• The Journal of Engineering Geology
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• v.15 no.1
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• pp.19-27
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• 2005

The Sambo mine is located in Hae-je Myeon, Moo-an Gun, Chollanamdo, which consists of host gneiss and rhyolite possessing quartzite veins with other compositions such as gold, silver, and sublimated sulfur. The ore grade estimated from the core was 0.05～10.9g/t or less in gold and 0.05～389g/t or less in silver, indicating a partial mineralization. The purpose of this paper is to understand the subsurface structures and the distribution of mineralized bodies in the Sambo mine using a combined method of Schlumberger, Wenner, and Dipole-di-pole resistivity surveys on the surface and the resistivity tomography survey in boreholes. The result of three-dimensional resistivity inversion showed that the mineralized body is extended to 240m long in the N10°～20°E direction, with 30m wide and 80 m thick from the surface. The low resistivity zones (<1,000ohm-m) determined from the resistivity image were in good agreement with the mineralized bodies and weak zones identified from the logged cores.