• 박물관보존과학
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• 제9권
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• pp.17-29
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• 2008

국립중앙박물관 소장 고려시대 동전 25점을 보존처리 하였다. 대상동전은 '동국중보', '동국통보', '해동통보', '해동중보', '삼한중보' 등 5종이다. 유물에 나쁜 영향을 줄 수 있는 염화물을 모두 제거하면 동전의 글자 및 형태가 훼손될 우려가 있어 부분적으로만 제거하였다. 현재까지 동국통보의 명문서체는 6종류 이상으로 알려져 있는데, X-Ray사진을 이용해서 판독한 결과 본 연구에서는 3종류의 명문을 확인하였다. 동전의 녹제거 과정에서 입수한 청동녹은 납동위원소비분석을 통해 동전의 원료 산지를 추정하였다. 최근에는 청동녹에 의한 여러 가지 과학분석이 이루어지고 있는 추세이다.

• 박물관보존과학
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• 제5권
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• pp.49-57
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• 2004

성덕대왕신종은 서기 771년에 완성되었으며 규모에 있어서나 예술적인 수준에 있어서 탁월한 걸작품으로서 우리 청동문화의 정수이다. 그러나 성덕대왕신종을 주조하기 위해 어디에서 원료를 입수하여 어떻게 배합하고 주조했는지에 대한 사료가 남아있지 않아 성덕대왕신종을 깊이 있게 이해하는 데 한계가 있다. 본 연구는 국립경주박물관에서 성덕대왕신종에 대한 안전진단의 일환으로 점검 과정 중 신종 내부에 돌출된 부분에서 채취한 시료 3점의 분석결과를 정리한 것이다. 성덕대왕신종을 제작하기 위한 원료의 배합비, 주조 당시의 금속조직, 원료의 산지 등에 중점을 두고 조사하였다.

• 자원환경지질
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• 제28권3호
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• pp.243-249
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• 1995

In order to investigate the origin of sulfate in rain waters and to evaluate the feasibility of using sulfur isotope method as a tracer of atmospheric pollutants, the sulfur isotopic ratio of sulfate in rain waters collected in Chonju city from October 1994 to March 1995 was monitored and was compared with those of possible sources proposed by previous works. The pH of rain waters shows an intermediate acidic range from 4.45 to 6.88 and their daily variation appears to be well correlated with to the amount of precipitation. The sulfur isotopic ratios of sulfate in rain waters show a highly restricted range from 0.0 to + 1.8‰. The ${\delta}^{34}S$ values are similar to those of soil and pine tree surrounding Chonju city, but largely deviate from those of China. D-parameter($d={\delta}D-8{\delta}^{18}O$) of rain waters varies from 9.4 to 28.8. The values indicate that the rain waters in Chonju city are originated from the rainy front of China continent. All data obtained from this study suggested that sulfate in the rain waters collected in Chonju city was mainly derived from the sulfur dioxide gas emitted by the petroleum combustion. Therefore, sulfur isotopic study for the precipitation provided an excellent tool for environmental assessment in this region and for tracing the source of atmospheric pollutants.

• 분석과학
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• 제15권1호
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• pp.7-14
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• 2002

본 연구에서는 레이저 애블레이션 이온 트랩 질량분석법을 이용하여 금속 및 세라믹 시료들에 대한 원소분석을 수행하였고, 이때 이온화 장치로는 XeCI 엑시머 레이저를 사용하였고 검출장치로서 이온트랩 질량 분석기를 사용하였다. 시료는 트랩의 바깥에 장착하여 시료의 교환이 매우 쉽도록 하였고 고체시료의 분석에 있어서 매우 효과적임을 밝혔다. 헬륨기체의 압력이나 이온저장시간, 초기질량제한 RF 전압 등에 대한 기초 실험을 통하여 실험의 최적 조건을 구하였고 (헬륨 기체압력 $1{\times}10^{-4}$ Torr 이온 저장시간 100 ms 초기 질량 제한전압 $1150V_{p-p}$), 이 결과를 토대로 금속시료(구리, 몰리브데늄)와 세라믹 시료(알루미나 세라믹, 지르코니아 세라믹) 들에 대한 원소분석을 수행하였다.

• Ocean and Polar Research
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• 제36권1호
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• pp.25-37
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• 2014

To understand the degradation processes of organic matter related to sulfate reduction by Sulfate Reduction Bacteria (SRB) in the tidal flat sediments of Hwang-do and Sogeun-ri, Tae-an Peninsula in Chungnam-do, biogeochemical characteristics were analyzed and highlighted using specific microbial biomarkers. The organic geochemical parameters (TOC, ${\delta}^{13}C_{org}$, C/N ratio, long-chain-n-alkane) indicate that most of the organic matter has been derived from marine phytoplankton and bacteria in the fine-grained sediment of Sogeun-ri, although terrestrial plant components have occasionally been incorporated to a significant degree in the coarse-grained sediment of Hwang-do. The concentration of sulfate in pore water is a constant tendency with regard to depth profile, while methane concentration appears to be slightly different with regard to depth profile at the two sites. Especially, the sum of bacteria fatty acid (a-C15:0 + i-C15:0 + C16:1w5) confirms that the these concentrations in Sogeun-ri are related to the degradation of Benzene, Toluene, Ethylbenzene and Xylene (BTEX) compounds from the crude oil retained in the sediments as a result of the Hebei Spirit oil-spill accident in 2007. The methane-related microbial communities as shown by lipid biomarkers (crocetane, PMI) are larger in some sedimentary sections of Hwang-do than in the Sogeunri tidal flat. These findings suggest that methane production by microbiological processes is clearly governed by SRB activity along the vertical succession in organic-enriched tidal flats.

• 보존과학회지
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• 제34권4호
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• pp.305-311
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• 2018

The yellow crystalline material present in yellow and green glass beads excavated from sites in the Baekje region of Korea was previously analyzed through scanning electron microscopy with energy dispersive spectroscopy and X-ray diffraction, revealing that the yellow crystalline material was $PbSnO_3$. This material is a pigment that is rarely seen in the Korean peninsula. Furthermore, some studies have been published on the provenance of lead in this material, which revealed no relationship to Korea, China, or Japan. In this study, we collected all accessible results of analyses on the lead isotope ratio of yellow and green glass beads excavated from the Korean peninsula, specifically from 7 sites in the Baekje region(located in the vicinity of Seoul, Wanju, Hwaseong, Osan, Gongju, Buyeo, and Iksan) and 2 sites in the Silla region(located in the vicinity of Gyeongju and Changnyeong). We subsequently investigated the lead provenance of the opacifying agents in the glass beads through comparison with the current extent of the galena data accumulated for the East Asian region, including Korea, China, and Japan, and for Thailand(Kanchanaburi Province), Southeast Asia. Our analysis determined that the lead provenance of the glass beads excavated from the Korean peninsula was Thailand(Kanchanaburi Province). Beyond our results, further studies should seek to determine the production sites of the glass beads. Obtaining and comparing the scientific analyses of glass beads from India and Southeast Asia would enable research on the glass beads trade through the maritime silk road.

• 보존과학회지
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• 제35권5호
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• pp.392-402
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• 2019

전북 완주 신풍유적 출토 고려시대 슬래그와 송풍관을 대상으로 신풍유적의 야동기술(冶銅技術)성격을 확인하고, 납 원료산지를 추정하기 위해 납동위원소비를 실시하여 알아보았다. 성분분석 결과, Cu-Sn-Pb 삼원계 합금하는 과정에서 비롯된 슬래그와 송풍관으로 해석되었다. 금속현미경과 주사전자현미경(scanning electron microscopy-energy dispersive spectrometer) 분석결과, 동괴와 주석괴에 방연석을 첨가하여 완제품 제작을 위한 중간소재를 생성하는 합금단계에서 발생한 부산물로 추정된다. 납동위원소비분석 결과, 한국 남부 Zone III 지역의 광산에서 채굴된 방연석을 사용하여 합금한 것으로 판단된다. 송풍관은 송풍관의 외측으로 갈수록 Mullite가 검출되어, 1,000℃ 내외에서 조업이 이뤄졌을 가능성이 있다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 추계학술대회
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• pp.232-236
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• 2000

Multi-regression statistical analyses were applied for the water quality data of shallow alluvial ground water (n = 47) collected from the Youngdeok area, in order to quantitatively generalize the natural (non-anthropogenic) causes of regional water quality variation. Seven samples having the high contamination index ( $C_{a}$ > 3) reflect the striong effects by anthropogenic activity. Most of the alluvial groundwaters have acquired their quality primarily due to the dissolution of carbonate minerals. The results of multi-regression analysis show that chlorine is mainly derived from seawater effect. Sulfur isotopic compositions of dissolved sulfur and the S $O_4$/Cl ratio also enable us to discriminate the samples (n = 18) which are affected by atmospheric input of marine aerosol (sea-spray) and also by mixing between freshwater and seawater. Hydrogen and oxygen isotope data of the samples collected lie close to the local meteoric water line obtained from nearby Pohang city but has lower slope (5.45) on the $\delta$D-$^{18}$ O plot, indicating that alluvial groundwater was recharged from infiltrated meteoric water which has undergone some degree of kinetic evaporation. The estimated initial isotopic composition of the recharged water ($\delta$D = -74.8$^{0}$ /$_{00}$, $\delta$$^{18}$ O = -10.8$^{[-1000]}$ /$_{[-1000]}$ ) suggests that the alluvial ground water recharge largely occurs during summer storm events.s.s.

• 자원환경지질
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• 제29권3호
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• pp.293-304
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• 1996

The Wolchul Mt. area is composed of a biotite granite and a pink feldspar granite. These granites are distinctly different in terms of their field occurrence, mineralogy, trace element and REE composition, as well as their isotope ages. The biotite granite has higher ferromagnesian elements and lower lithophile trace element abundances than the pink feldspar granite. The biotite granite has high Sr and Ba while the pink feldspar granite has high Rb. On the Rb-Sr-Ba diagram the biotite granite plots as a granodiorite while the pink feldspar granite belongs to a strongly differentiated granite. The ${\Sigma}$ LREE/ ${\Sigma}$ REE for the biotite granite is 0.95 and for the pink feldspar granite it is 0.88. The ratio shows a steep decrese in LREE while HREE is essentially constant. Based on the Eu/Sm, $[La/Lu]_{cN}$ and low Eu(-), the biotite granite has quartz diorite to granodiorite composition while the pink feldspar granite, with a relatively high Eu(-) anomaly, falls into the monzo- to syenogranite classification. The silica vs. trace element diagrams for the two granites indicate that the biotite granite could have formed near to a continental margin or volcanic island setting environment while the pink feldspar granite formed within a continental plate or as result of plate collision. The biotite granite has a U-Pb zircon age of 175 Ma, i.e. Middle Jurassic. The pink feldspar granite is younger, it has a K-Ar orthoclase age $93.6{\pm}1.5$ Ma which is Late Cretaceous age.

• 보존과학회지
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• 제34권1호
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• pp.59-67
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• 2018

보물 제337호 청양 장곡사 금동약사여래좌상을 대상으로 불상의 제작기술체계 및 납 원료산지를 규명하고자 하였다. 성분분석결과 구리(Cu) 68.8%, 주석(Sn) 10.4%, 납(Pb) 17.1%의 삼원합금으로 납의 함량이 높은 중 대형 불상의 주성분 조성비와 유사한 경향성을 보이고 있다. 열이온화질량분석기(TIMS)를 이용한 납동위원소비 데이터를 한반도 납동위원소 분포도에 대입한 결과 전라도와 충청도 지역에 해당하는 영남육괴 및 옥천변성대 영역(Zone 3)에 도시되었으며, 불상이 봉안된 사찰의 인근 지역에 위치한 광산에서 채취한 원료를 사용하여 제작하였을 가능성이 있다. 이어 유사시기에 제작된 강진 고성사 청동보살좌상의 제작기법 연구와 비교분석한 결과 불상의 크기 및 조성 시기, 양식적 특성 등에 따른 제작기법의 차이점을 확인하였으며, 사찰과 동일한 영역에 위치한 방연석을 사용하였을 가능성을 엿볼 수 있다.