• 한국습지학회지
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• 제7권2호
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• pp.121-132
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• 2005

천수만 황도 갯벌의 IKONOS 영상을 이용한 표층 퇴적상 분류를 위하여 광학 반사도를 입도, 조류로의 형태, 지잔존수 (surface remnant water)의 면적비와 같은 다양한 퇴적환경 요소들과 비교하였다. IKONOS 영상과 갯벌 내의 소지형별 퇴적환경 사이의 관계를 분석하기 위하여 Echo-sounder를 이용하여 갯벌 Digital Elevation Model (DEM)을 만들었다. 펄-혼합 퇴적상과 모래 퇴적상의 경계에서 광학 반사도의 차이가 뚜렷하게 나타났으며 사주의 구분도 가능하였다. 펄-혼합 퇴적상 지역은 조류로가 매우 복잡하게 발달하고 있으며 지형이 상대적으로 높은 곳에 위치하고 있었다. 펄과 혼합 퇴적의 경계에서 지표수의 존재 유무가 다르게 나타났으나 광학 반사도의 차이가 뚜렷하지 않았다. 모래 퇴적상의 경우 조류로가 단순하게 직선형으로 발달했으며 지형도 상대적으로 낮은 지역에 분포하였으며 지표잔존수가 거의 전 지역을 덮고 있어 광학 반사도가 낮게 나타났다. 최대우도 분류법을 이용한 표층 퇴적상 분류정밀도는 86.2 %로 나타났다. 이 결과로부터 IKONOS와 같은 고해상도 영상에 대해 지표잔존수, 조류로 분포와 지형 등의 갯벌 퇴적학적 특성을 고려한다면 펄, 혼합 그리고 모래 퇴적상 구분은 가능하다는 것을 알 수 있다.

• 보존과학연구
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• 통권24호
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• pp.81-98
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• 2003

The biodeterioration on Iksan Mireuksaji pagoda has been studied with fucus on application of K201 as a chemical treatment. Total of 39species, including 10 algae, 16 lichens, 6 mosses and 7 unidentified bacteria and fungi, were collected and identified on the surface of the pagoda. Most of them caused serious discoloration on the surface. The effectiveness and stability of K201 was examined by applying it on some part of the pagoda. A mild spraying of solution diluted to half of original reagent was good enough to eliminate all the deteriorating species on the surface. Most of discoloration disappeared after the treatment except the red color caused by iron substance. The effectiveness of the regent was compared with water wash. The stone was first washed with water and the dirt on the surface was scrubbed off from the surface. The initial surface of the stone was clearer in water wash. However, many of the deteriorating species reappear in 4 weeks after water wash. Although spraying of the reagent K201 could noteliminate all the remnant of dead organisms as good as scrubbing the surface, no deteriorating algae or lichen was observed until two month after treatment. Therefore, spraying method with chemicals seems more stable and reliable way to remove the biodeterioration than physical scrubbing of the surface.

• 방사성폐기물학회지
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• 제19권4호
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• pp.517-532
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• 2021

Safe geological disposal of spent nuclear fuel (SNF) requires knowledge of the deep hydrochemical characteristics of the repository site. Here, we conducted a set of deep hydrochemical investigations using a 750-m borehole drilled in a model granite system in Wonju, South Korea. A closed investigation system consisting of a double-packer, Waterra pump, flow cell, and water-quality measurement unit was used for in situ water quality measurements and subsequent groundwater sampling. We managed the drilling water labeled with a fluorescein dye using a recycling system that reuses the water discharged from the borehole. We selected the test depths based on the dye concentrations, outflow water quality parameters, borehole logging, and visual inspection of the rock cores. The groundwater pumped up to the surface flowed into the flow cell, where the in situ water quality parameters were measured, and it was then collected for further laboratory measurements. Atmospheric contact was minimized during the entire process. Before hydrochemical measurements and sample collection, pumping was performed to purge the remnant drilling water. This study on a model borehole can serve as a reference for the future development of deep hydrochemical investigation procedures and techniques for siting processes of SNF repositories.

• Journal of the korean society of oceanography
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• 제39권1호
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• pp.1-13
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• 2004

The Yellow Sea Warm Current (YSWC) and the Yellow Sea Cold Bottom Water (YSCBW) are two protruding features, which have strong influence on the community structure and distribution of zooplankton in the Yellow Sea. Both of them are seasonal phenomena. In winter, strong north wind drives southward flow at the surface along both Chinese and Korean coasts, which is compensated by a northward flow along the Yellow Sea Trough. That is the YSWC. It advects warmer and saltier water from the East China Sea into the southern Yellow Sea and changes the zooplankton community structure greatly in winter. During a cruise after onset of the winter monsoon in November 2001 in the southern Yellow Sea, 71 zooplankton species were identified, among which 39 species were tropical, accounting for 54.9 %, much more than those found in summer. Many of them were typical for Kuroshio water, e.g. Eucalanus subtenuis, Rhincalanus cornutus, Pareuchaeta russelli, Lucicutia flavicornis, and Euphausia diomedeae etc. 26 species were warm-temperate accounting for 36.6% and 6 temperate 8.5%. The distribution pattern of the warm water species clearly showed the impact of the YSWC and demonstrated that the intrusion of warmer and saltier water happened beneath the surface northwards along the Yellow Sea Trough. The YSCBW is a bottom pool of the remnant Yellow Sea Winter Water resulting from summer stratification and occupy most of the deep area of the Yellow Sea. The temperature of YSCBW temperature remains ${\leq}{\;}10^{\circ}C$ in mid-summer. It is served as an oversummering site for many temperate species, like Calanus sinicus and Euphaisia pacifica. Calanus sinicus is a dominant copepod in the Yellow Sea and East China Sea and can be found throughout the year with the year maximum in May to June. In summer it disappears in the coastal area and in the upper layer of central area due to the high temperature and shrinks its distribution into YSCBW.

• 대한치과보존학회:학술대회논문집
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• 대한치과보존학회 2001년도 추계학술대회(제116회) 및 13회 Workshop 제3회 한ㆍ일 치과보존학회 공동학술대회 초록집
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• pp.577-577
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• 2001

The lastest concepts in bonding are "total etch", in which both enamel and dentin are etched with an acid to remove the smear layers, and "wet dentin" in which the dentin is not blown dry but left moist before application of the bonding primer. Ideally, the application of a bonding agent to tooth structure should be insensitive to minor contamination from oral fluids. Clinically contaminations such as saliva, gingival fluid, blood and handpiece lubricant are often encountered by dentists during preparation of a restoration. The aim of this study was to evaluate the effect of contamination by hem-ostatic agents on shear bond strength of compomer restorations. One hundred and ten extracted human maxillary and mandibular molar teeth were collected. The teeth were cleaned from soft tissue remnant and debris and stored in physiologic solution until they were used. Small flat area on dentin of the buccal surface were wet ground serially with 400, 800 and 1200 abrasive paper on automatic polishing machine. The teeth were randomly divided into 11 groups. Each group was conditioned as follows: Group 1 : Dentin surface was not etched and not contaminated by hemostatic agents. Group2 : Dentin surface was not etched but was contaminated by Astringedent (Ultradent product Inc., Utah, U.S.A.). Group3 : Dentin surface was not etched but was contaminated by Bosmin (Jeil Phann, Korea.). Group4 : Dentin surface was not etched but was contaminated by Epri-dent (Epr Industries, NJ, U.S.A.). Group5: Dentin surface was etched and not contaminated by hemostatic agents. Group 6 : Dentin surface was etched and contaminated by Astringedent. Group7 : Dentin surface was etched and contaminated by Bosmin. Group8 : Dentin surface was etched and contaminated by Epri-dent. Group9 : Dentin surface was contaminated by Astringedent. The contaminated surface was rinsed by water and dried by compressed air. Group10 : Dentin surface was contaminated by Bosmin. The contaminated surface was rinsed by water aud dried by compresfed air. Group 11 : Dentin surface was contaminated by Epri-dent. The contaminated surface was rinsed by water and dried by compresfed air. After surface conditioning, F2000 was applicated on the conditoned dentin surface. The teeth were thermocycled in distilled water at $5^{\circ}C\;and\;55^{\circ}C$ for 1000 cycles. The samples were placed on the binder with the bonded compomer-dentin interface parallel to the lmife-edge shearing rod of the Universal testing machine(Zwick 020, Germany) running at a cross head speed of 1.0mmimin. There were no significant differences in shear bond strength between groups 1 and group 3 and 4, but group 2 showed significant decrease in shear bond strength compared with group 1. There were no significant differences in shear bond strength between group 5 and group 7 and 8, but group 6 showed significant decrease in shear bond strength compared with group 5. There were no significant differences in shear bond strength between group 5 and group 9, 10 and 11.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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• pp.734-738
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• 2002

We present spectral characteristics of tidal flat sediments and algal mat that were tested in the Gomso and Saemangum tidal flats, Korea. The objective of this study is to investigate the spectral reflectance and the radar scattering modeling in the tidal flats. Ground truth data obtained in the tidal flats include grain size, soil moisture content and its variation with time, surface roughness, chlorophyll, ground leveling, and field spectral reflectance measurement. The concept of an effective exposed area (EEA) is introduced to accommodate the effect of remnant surface water, and it seriously affects the reflection of short wavelength infrared and microwave. The nin size of 0.0625 mm has been normally used as a critical size of mud and sand discrimination. But we propose here that 0.25 mm is more practical grain size criterion to discriminate by remote sensing. Algal mat is the primary product in tidal flats, and it is found to be very important to understand spectral characteristics for tidal flat remote sensing. We have also conducted radar scattering modeling, and showed L-band HV-polarization would be the most effective combination.

• 자원환경지질
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• 제55권6호
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• pp.671-687
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• 2022

우리나라 서·남해 연안 지대는 해안으로부터 10 km 범위 내 관정의 약 47%가 해수의 영향을 받은 것으로 보고되었고, 지하수의 염분화 원인이 해수 침투 때문일 것이라 해석되어 왔다. 서천지역의 길산천은 금강하구둑이 건설·운영되어 매립 농지로 이용되기 전까지는 감조하천으로서 유역 내에는 해수에 의한 퇴적물이 생성되고 그 내부에는 염분 공극수가 존재했을 것으로 추정된다. 길산천 소유역 내 지하수는 EC 값이 111~21,000 µS/cm 범위로서 매우 높은 염분 지하수가 존재하며, 수질 유형은 Ca(or Na)-HCO₃, Ca(or Na)-HCO₃(Cl), Na-Cl(HCO₃), Na-Cl 등 다양하게 나타나고 있다. 이러한 수질의 다양성은 강수 및 지표수로부터 유입 생성되는 담수 지하수 수질과 해수 수질의 혼합 현상 때문에 기인되는 것으로 판단된다. 금번 연구에서는 이러한 수질 다양성 및 염분 지하수의 존재가 현재 진행 중인 해수 침투 때문인지 아니면 조간대 퇴적물 내 고(古)염분 공극수가 씻겨나가는 과정에서 잔존하기 때문인지를 논의하였다. 이를 위해, 연구지역 내 강수, 지표수, 해수, 지하수에 대하여 수질 특성을 비교하고, 삼중수소 함량, 산소/수소 안정동위원소 조성, ⁸⁷Sr/⁸⁶Sr 비 등을 비교·검토하였다. 산소/수소 안정동위원소 조성으로 볼 때, EC 값이 큰 염분 지하수들의 물 성분은 담수 지하수와 지표수 물이 혼합된 물로 구성되어 있으며, 삼중수소 함량에 의해 추정되는 연령이 젊은 지하수들은 NO₃ 함량이 높은 지표 영향을 많이 받은 것들로 나타나, 연구지역의 지하수 수질 진화 과정에는 담수 지하수 및 지표수가 지속적으로 영향을 미치고 있는 것으로 나타났다. 또한, 담수 지하수/지표수와 해수를 2개의 단성분으로 가정하고 Cl 함량 변화에 따른 Na/Cl ratio와 나트륨흡착도(SAR)의 변화 패턴을 고려하면, 연구지역 지하수들은 해수 침투가 아니라 고염분 지하수의 씻김 현상을 겪고 있는 것으로 해석되었다.

• Restorative Dentistry and Endodontics
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• 제27권2호
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• pp.150-157
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• 2002

One of the latest concepts in bonding are "total etch", in which both enamel and dentin are etched with an acid to remove the smear layers, and "wet dentin" in which the dentin is not dry but left moist before application of the bonding primer Ideally the application of a bonding agent to tooth structure should be insensitive to minor contamination from oral fluids. Clinically, contaminations such as saliva, gingival fluid, blood and handpiece lubricant are often encountered by dentists during cavity preparation. The aim of this study was to evaluate the effect of contamination by hemostatic agents on shear bond strength of compomer restorations. One hundred and ten extracted human maxillary and mandibular molar teeth were collected. The teeth were removed soft tissue remnant and debris and stored in physiologic solution until they were used. Small flat area on dentin of the buccal surface were wet ground serially with 400, 800 and 1200 abrasive papers on automatic polishing machine. The teeth were randomly divided into 11 groups. Each group was conditioned as follows : Group 1: Dentin surface was not etched and not contaminated by hemostatic agents. Group 2: Dentin surface was not etched but was contaminated by Astringedent$^{\circledR}$(Ultradent product Inc., Utah, U.S.A.) Group 3: Dentin surface was not etched but was contaminated by Bosmin$^{\circledR}$(Jeil Pharm, Korea.). Group 4: Dentin surface was not etched but was contaminated by Epri-dent$^{\circledR}$(Epr Industries, NJ, U.S.A.). Group 5: Dentin surface was etched and not contaminated by hemostatic agents. Group 6: Dentin sorface was etched and contaminated by Astringedent$^{\circledR}$. Group 7 : Dentin surface was etched and contaminated by Bosmin$^{\circledR}$. Group 8: Dentin surface was etched and contaminated by Epri-dent$^{\circledR}$. Group 9: Dentin surface was contaminated by Astringedent$^{\circledR}$. The contaminated surface was rinsed by water and dried by compressed air. Group 10: Dentin surface was contaminated by Bosmin$^{\circledR}$. The contaminated surface was rinsed by water and dried by compressed air. Group 11 : Dentin surface was contaminated by Epri-dent$^{\circledR}$. The contaminated surface was rinsed by water and dried by compressed air. After surface conditioning, F2000$^{\circledR}$ was applicated on the conditoned dentin surface The teeth were thermocycled in distilled water at 5$^{\circ}C$ and 55$^{\circ}C$ for 1,000 cycles. The samples were placed on the binder with the bonded compomer-dentin interface parallel to the knife-edge shearing rod of the Universal Testing Machine(Zwick Z020, Zwick Co., Germany) running at a cross head speed or 1.0 mm/min. Group 2 showed significant decrease in shear bond strength compared with group 1 and group 6 showed significant decrease in shear bond strength compared with group 5. There were no significant differences in shear bond strength between group 5 and group 9, 10 and 11.

• 대한지리학회지
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• 제41권4호
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• pp.404-417
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• 2006

한라산 만세동산의 표고 $1,595{\sim}l,645m$에 위치한 1차수 실험유역에서 관측한 수문자료와 인근 관측소의 기상자료를 토대로 물수지를 분석하여 한라산 아고산대의 수문순환 특성을 규명하였다. 실험유역은 주로 조면현무암으로 이루어진 면적 1.34ha의 소유역이며, 지표식생은 제주조릿대와 초본 군락이 우점하고 있다. 물수지 분석에는 2004년 4월 15일부터 9월 19일까지 157일에 걸쳐 20분 간격으로 관측한 강수량과 유량을 이용하였다. 실험유역은 해안 및 중산간지대의 저지보다 $1.6{\sim}3$배 많은 3,074mm의 강수량을 기록하였으며, 강수량의 27.6%에 해당하는 850mm가 유역 하류로 흘러나갔다 증발산량은 강수량의 14.2%를 차지하는 437mm에 지나지 않으며, 나머지 58.2%에 해당하는 1,790mm는 기반암을 통과하여 지하로 이동하였다. 실험유역은 지형성 강수가 자주 발생하는 아고산대에 위치하므로 강수량이 많고 강수강도가 크나 유출량은 강수량의 30%를 넘지 못한다. 반면에 침루량은 유출량의 2배에 달하는 강수량의 60% 정도를 차지하고 있다. 따라서 한반도의 화강암이나 편마암 유역과는 달리 물수지 요소 가운데 침루 비율이 높게 나타나는데, 이것은 토양 공극율이 높고 토층 하부에 투수성이 큰 현무암질 용암이 분포하는 제주도의 지질 특성과 관계가 있는 것으로 생각된다.

• 대한원격탐사학회지
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• 제26권5호
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• pp.497-510
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• 2010

이 연구에서는 토양의 유전상수 (dielectric constant) 표면의 거칠기 (surface roughness)와 지표면의 기하 (geometric) 등과 같은 다양한 물리적 요소들의 정보를 포함하고 있는 SAR (Synthetic Aperture Radar) 자료를 이용하여 강화도 갯벌의 표층 퇴적환경을 분석하였다. JERS-1, ENVISAT과 ALOS 위성의 다양한 SAR 자료로부터 레이더 후방산란계수 (backscattering coefficient)를 추출하여 각 퇴적환경 요소들과의 관계를 파악하고 시간변화에 따른 지표의 변화 정도를 알 수 있는 긴밀도 (coherence)를 추출하여 퇴적상과 비교하였다. SAR 영상으로부터 추출한 후방산란계수와 긴밀도를 이용한 강화도 갯벌 퇴적환경 특성을 분석한 결과 높은 긴밀도를 갖는 지역은 입도가 작은 펄이 많이 포함된 펄 퇴적상이며 긴밀도가 낮을수록 큰 입도가 많이 분포하는 지역임을 알 수 있었다. 강화도 갯벌은 다른 갯벌과는 달리 조류로가 많이 발달하여 썰물 시 수분함유량에 많은 영향을 주어 모래 퇴적상과 혼합 퇴적상은 갯벌의 노출시간이 증가함에 따라 토양 수분함유량이 감소하여 후방산란계수가 점차 감소한다. 그러나 펄 퇴적상에서는 지형 고도가 높아 해수의 많은 영향을 받지 않으며 조류로의 밀도가 높기 때문에 토양 수분함유량이 감소하지만 후방산란계수가 높게 나타났다. 또한 갯벌은 토양 수분함유량뿐만 아니라 표면에 남아있는 잔존수도 많아 강우량이 많은 날은 지표 잔존수가 증가하기 때문에 비교적 후방산란계수가 낮게 나타나는 경향을 보였다. 이 연구의 결과, 긴밀도, 후방산란계수와 각 퇴적환경 요소들의 상관관계를 알 수 있었으며, 향후 강화도 갯벌 퇴적환경의 공간적 분석을 위해 각각의 요소들이 미치는 영향에 대한 정량적인 연구가 필요할 것으로 판단된다.