• 제목/요약/키워드: isotope ratio.

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국립중앙박물관소장 청동유물의 납동위원소비 데이터베이스 구축(II) (Lead Isotope Ratio Data Base for Bronze Objects at the National Museum of Korea (II))

  • 강형태;안주영;전효수
    • 박물관보존과학
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    • 제9권
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    • pp.105-116
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    • 2008
  • 국립중앙박물관 보존과학팀에서는 금속 유물의 보존처리 과정에서 얻은 청동 녹의 과학적 연구로서 납동위원소비 데이터를 구축하고 이로부터 청동기 원료의 산지와 관련된 연구를 수행하고자 한다. 청동 녹의 납동위원소비 분석을 위한 분석 장비는 한국기초과학지원연구원의 열이온화질량분석(Thermal ionization mass spectromer ; TIMS)를 활용하였다. 본 연구의 일환으로 2차 년도인 2008년에는 백제시대의 금동환형좌금 2점, 낙랑시대의 동전두 2점, 통일신라시대의 청동제화형접시 10점, 원풍통보(元豊通寶)(1078년-북송)의 청동기 4점(1점은 시대미상)등 총 18점의 납동위원소비를 분석하였다.

팔당호 내 식물플랑크톤 안정동위원소 분석을 통한 유기물 기원 평가 (Evaluation of Organic Matter Sources of Phytoplankton in Paldang Reservoir using Stable Isotope Analysis)

  • 김종민;김보경;김민섭;신기식
    • 한국물환경학회지
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    • 제31권2호
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    • pp.159-165
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    • 2015
  • The organic matter sources of phytoplankton and related environmental factors influencing algal bloom in Paldang reservoir were studied using nitrogen and carbon isotope ratio(${\delta}^{15}N$, ${\delta}^{13}C$). Phytoplankton samples for stable isotope analysis were collected from four points in reservoir using a plankton net. Physicochemical water quality, algal taxa and hydrological data were collected from published monitoring material. Phytoplankton samples were analyzed by IRMS. CN ratio of each sample was very similar to that of phytoplankton from literature cited. ${\delta}^{15}N$ of each sample was decreased during July. Mixing and dilution of nitrogen sources due to increment of influx by concentrated rainfall were considered as the main reason for the decline of ${\delta}^{15}N$. Based on analyzed ${\delta}^{15}N$ value of each sample, nitrogen source of Bughan river sample was presumed to come from soil. The nitrogen sources of Namhan river and Kyeongan stream samples seemed to be sewage or animal waste. Low ${\delta}^{15}N$ value in August (2012) seemed to be influenced by isotope fractionation due to the blooming of nitrogen-fixation blue-green algae (Anabaena spp.). Variation in ${\delta}^{15}N$ values particularly by blue-green algal bloom was considered the important factor for estimating the organic matter sources of phytoplankton.

Temporal Variations in Isotope Ratios and Concentrations of Nitrate-nitrogen in Groundwater as Affected by Chemical Fertilizer and Livestock Manure

  • Yoo, Sun-Ho;Choi, Woo-Jung;Han, Gwang Hyun;Park, Jung-Geun;Lee, Sang-Mo;Jin, Sheng-ai
    • Journal of Applied Biological Chemistry
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    • 제42권4호
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    • pp.186-190
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    • 1999
  • Isotope ratio ($^{15}N/^{14}N$) and nitrate-nitrogen concentration in groundwater were measured to investigate the effect of chemical fertilizer and livestock manure on temporal variations in nitrate-nitrogen concentration and to estimate the contribution of fertilizer and manure to groundwater contamination by nitrate. Four study wells from a rural area in Kyonggi province were selected. One well was located on an upper site from a livestock feedlot, and the others were situated at lower sites from the feedlot. The ${\delta}^{15}N$ values were analyzed by a stable isotope ratio mass spectrometer (Micromass, VG Optima IRMS). Reproducibility of the method and precision of the mass spectrometer were below 1.0 and 0.1‰, respectively Even though study wells were located at the same area, nitrate-nitrogen concentrations and ${\delta}^{15}N$ values differed and fluctuated during the sampling period. The ${\delta}^{15}N$ values of well located at upper site from the feedlot were extremely variable (-1.48~20.80‰). The ranges of ${\delta}^{15}N$ value of three wells situated at lower sites from the feedlot were 11.83~20.73 (ave. 16.11), 8.90~11.73 (ave.11.01), and 5.29~12.73‰ (ave. 8.21‰) with increasing distance from the feedlot. The average values of contribution proportion of nitrogen derived from livestock manure to nitrate-nitrogen in groundwater were 79% for the well closet to the feedlot, 44% for the well most distant from the feedlot, and 56% for the well in between the two wells.

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Identification of pollutant sources using water quality and stable isotope ratios of inflow tributaries in the lower reaches of the Han-River

  • Hong, Jung-Ki;Lee, Bo-Mi;Son, Ju Yeon;Park, Jin-Rak;Lee, Sung Hye;Kim, Kap-Soon;Yu, Soon-Ju;Noh, Hye-ran
    • 분석과학
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    • 제32권2호
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    • pp.65-76
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    • 2019
  • Despite the expansion of sewage treatment facilities to reduce pollutants in the tributaries of the Han River, water pollution accidents such as fish deaths continue to frequently occur. The purpose of this study was to identify the pollutant sources using water quality and stable isotope ratio (${\delta}^{15}N$, ${\delta}^{13}C$, ${\delta}^{15}N-NH_4$, ${\delta}^{15}N-NO_3$) analysis results in the three inflow tributaries (Gulpocheon (GP), Anyangcheon (AY) and Sincheon (SC)) of the Han River. Water quality was analyzed in June and October from 2013 to 2017, and the results showed that the concentrations of nutrients, such as T-N, $NO_3-N$, and T-P, were increased at GP4, AY3, SC3, and SC4, which lie downstream of sewage treatment facilities. The results of ${\delta}^{15}N$ for June 2017 indicated that the source of nitrogen was sewage or livestock excreta at GP4 and SC4, and organic fertilizers at AY3 and SC3. ${\delta}^{15}N-NO_3$ results suggested that the source of nitrogen was related to organic sewage, livestock or manure at GP4, AY3 and SC4. Therefore, GP4 and SC4 were more influenced by effluent from sewage treatment facilities than by their tributaries, AY3 and SC3 were considered to be influenced more by their tributary than effluent from sewage treatment facilities. With the results of this study, the source of contamination (sewage treatment facility effluent) of river inflow downstream of Han River could be confirmed using water quality and stable isotope ratio.

탄소 및 질소 안정동위원소 비를 이용한 영산강하구역 유기물 기원 추정 연구 (Determination of the Origin of Particulate Organic Matter at the Estuary of Youngsan River using Stable Isotope Ratios (${\delta}^{13}C$, ${\delta}^{15}N$))

  • 이연정;정병관;신용식;김성환;신경훈
    • 생태와환경
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    • 제46권2호
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    • pp.175-184
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    • 2013
  • 본 연구는 영산강하구역 입자물질 유입원의 시 공간적인 변화를 추정해 보고자 몽탄대교에서 영산강 하구둑에 이르는 영산강하구역 세 정점에서 연 6회에 걸쳐 수 층 부유 물질의 탄소 및 질소 안정동위원소 비를 비교하였다. 모든 정점에서 8월에 강우를 통한 외부기원 유기물의 유입이 증가하였으며, 이 때 암모니아성 질소 및 규산염의 유입 역시 함께 증가하였다. 탄소 안정동위원소 비 측정 결과 11월과 8월에 정점 별 유기물의 기원이 크게 차이 났으며, 안정동위원소 비 값을 이용하여 주요 유입원 추정이 가능하였다. 11월에 모든 정점에서 질소 안정동위원소 비가 무거운 값을 보였고, 인산염의 농도가 가장 높게 나타났는데 이는 축산폐수 및 농경지를 통한 유입이 영향을 준 것으로 판단된다. 또한 다른 정점에 비해 영산강 하구둑에서 모든 조사 기간 동안 비교적 높은 질소 안정동위원소 비를 보였으며, 이를 통해 축산폐수 및 농경지를 통한 유기물 유입이 다른 정점에 비해 높을 것으로 추정된다. 본 연구 결과를 통해 안정동위원소 비 분석은 입자성유기물의 기원을 추정하는데 유용한 방법임을 확인할 수 있었다.

농촌하천 유역의 주 오염원 추적을 위한 안정성 동위원소 질량비 분석 (Stable Isotope Ratio Analysis for Tracing thee Major Pollution Source in Agricultural Watersheds)

  • 홍영진;김철성;권순국
    • 한국농공학회:학술대회논문집
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    • 한국농공학회 1999년도 Proceedings of the 1999 Annual Conference The Korean Society of Agricutural Engineers
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    • pp.777-782
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    • 1999
  • It has been acknowledged that fertilizer and animal waste have different ratio of \ulcornerN/\ulcornerN which is presented as a symbol of $\delta$\ulcornerN, and that the values of $\delta$\ulcornerN for fertilizer and animal waste are placed less than +8 $\textperthousand$ and higher than +10$\textperthousand$, respectively. By this reason, the demarcation range for the source nitrogen mass ratio is between +8$\textperthousand$ and +10$\textperthousand$. In this study, we would suggest a possible method to trace the major pollution basis using the nitrogen isotope analysis method for management of water quality.

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금강 하구 생태계에서 아미노산의 질소 안정동위원소비를 이용한 섭식생물의 영양단계 파악 (Determination of Trophic Position Using Nitrogen Isotope Ration of Individual Amino Acid in the Geum Estuary)

  • 최현태;최보형;신경훈
    • 생태와환경
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    • 제50권4호
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    • pp.432-440
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    • 2017
  • CSIA-AAs은 섭식 생물의 영양단계 산출 연구에서 SIA를 대체할 수 있는 연구 방법으로 크게 주목 받고 있지만, 최근까지 국내 연구 사례는 매우 부족하다. 본 연구에서는 금강 하구역에서 채집된 두 종의 다모류(Nephtyidae, Glyceridae)와 두 종의 어류 (Platycephalus indicus, Lophius litulon)에 대한 영양단계를 ${\delta}^{15}N_{AAs}$를 통해 산출하고 이를 ${\delta}^{15}N_{bulk}$를 이용해 산출한 영양단계와 비교하고자 하였다. 두 정점에서 채집된 다모류의 $TP_{bulk}$는 각각 2.6과 3.1로 다른 것으로 확인되었으며, 두 산출기법($TP_{base2}$, $TP_{base1}$)에 따른 차이는 작은 것으로 나타났다. 반면에, 본 연구에서 분석된 두 어종에 대한 $TP_{bulk}$는 각각 3.1과 2.3으로 어종 간 차이가 확인되었으나, $TP_{AAs}$는 3.8과 3.7로 어종 간 차이가 매우 작고 상대적으로 높은 영양단계가 확인되었다. 이는 두 어종이 어식성 어류임을 고려할 때 $TP_{AAs}$가 보다 더 신뢰할 수 있는 기법이라는 것을 확인할 수 있었으며, 본 연구는 한국 연안 생태계에서 CSIA-AAs의 활용 필요성과 그 유용성을 보여주고 있다.

다이오드 레이저 흡수분광법을 이용한 산소 동위원소의 성분비 측정 (Measurement of oxygen isotope ratio using tunable diode laser absorption spectroscopy)

  • 박상언;정도영;김재우;고광훈;임권;정의창;김철중
    • 한국광학회지
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    • 제15권1호
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    • pp.1-5
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    • 2004
  • 분리막을 이용한 산소-18 분리실험에서 분리된 시료의 동위원소 성분비 분석을 위해 다이오드 레이저 흡수분광장치를 구성하였다. 흡수신호의 신호 대 잡음비를 높이기 위해 lock-in증폭기를 사용한 파장변조 분광법을 채택하였다. 레이저의 주파수 변조폭 최적화와 FFT 저역통과 필터링을 통해 다중반사흡수셀에서 발생하는 간섭무늬 잡음을 줄였다. 산소-18에 대한 흡수분광장치의 최대편차는 $\pm$4$\textperthousand$로 측정되었다.

Determination of Copper in Uniformly-Doped Silicon Thin Films by Isotope-Dilution Inductively Coupled Plasma Mass Spectrometry

  • 박창J.;차명J.;이동S.
    • Bulletin of the Korean Chemical Society
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    • 제22권2호
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    • pp.205-209
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    • 2001
  • Uniformly-doped silicon thin films were fabricated by ion beam sputter deposition. The thin films had four levels of copper dopant concentration ranging between 1 ${\times}$1019 and 1 ${\times}$ 1021 atoms/cm3 . Concentrations of Copper dopants were determined by the isotope dilution inductively coupled plasma mass spectrometry (ICP-MS) to provide certified reference data for the quantitative surface analysis by secondary ion mass spectrometry (SIMS). The copper-doped thin films were dissolved in a mixture of 1 M HF and 3 M HNO3 spiked with appropriate amounts of 65 Cu. For an accurate isotope ratio determination, both the detector dead time and the mass discrimination were appropriately corrected and isobaric interference from SiAr molecular ions was avoided by a careful sample pretreatment. An analyte recovery efficiency was obtained for the Cu spiked samples to evaluate accuracy of the method. Uncertainty of the determined copper concentrations, estimated following the EURACHEM Guide, was less than 4%, and detection limit of this method was 5.58 ${\times}$ 1016 atoms/cm3.