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      탄산칼슘을 이용한 이산화탄소 안정동위원소 표준시료 제작에 대한 연구 = Preparation of Pure CO<sub>2</sub> Standard Gas from Calcium Carbonate for Stable Isotope Analysis

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      https://www.riss.kr/link?id=A100826365

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      The isotope ratios of $^{13}C/^{12}C$ and $^{18}O/^{16}O$ for a sample in a mass spectrometer are measured relative to those of a pure $CO_2$ reference gas (i.e., laboratory working standard). Thus, the calibration of a laboratory working standard gas to the international isotope scales (Pee Dee Belemnite (PDB) for ${\delta}^{13}C$ and Vienna Standard Mean Ocean Water (V-SMOW) for ${\delta}^{18}O$) is essential for comparisons between data sets obtained by other groups on other mass spectrometers. However, one often finds difficulties in getting well-calibrated standard gases, because of their production time and high price. Additional difficulty is that fractionation processes can occur inside the gas cylinder most likely due to pressure drop in long-term use. Therefore, studies on laboratory production of pure $CO_2$ isotope standard gas from stable solid calcium carbonate standard materials, have been performed. For this study, we propose a method to extract pure $CO_2$ gas without isotope fractionation from a solid calcium carbonate material. The method is similar to that suggested by Coplen et al., (1983), but is better optimized particularly to make a large amount of pure $CO_2$ gas from calcium carbonate material. The $CaCO_3$ releases $CO_2$ in reaction with 100% pure phosphoric acid at $25^{\circ}C$ in a custom designed, evacuated reaction vessel. Here we introduce optimal procedure, reaction conditions, and samples/reactants size for calcium carbonate-phosphoric acid reaction and also provide the details for extracting, purifying and collecting $CO_2$ gas out of the reaction vessel. The measurements for ${\delta}^{18}O$ and ${\delta}^{13}C$ of $CO_2$ were performed at Seoul National University using a stable isotope ratio mass spectrometer (VG Isotech, SIRA Series II) operated in dual-inlet mode. The entire analysis precisions for ${\delta}^{18}O$ and ${\delta}^{13}C$ were evaluated based on the standard deviations of multiple measurements on 15 separate samples of purified $CO_2$. The pure $CO_2$ samples were taken from 100-mg aliquots of a solid calcium carbonate (Solenhofen-ori $CaCO_3$) during 8-day experimental period. The multiple measurements yielded the $1{\sigma}$ precisions of ${\pm}0.01$‰ for ${\delta}^{13}C$ and ${\pm}0.05$‰ for ${\delta}^{18}O$, comparable to the internal instrumental precisions of SIRA. Therefore, we conclude the method proposed in this study can serve as a way to produce an accurate secondary and/or laboratory $CO_2$ standard gas. We hope this study helps resolve difficulties in placing a laboratory working standard onto the international isotope scales and does make accurate comparisons with other data sets from other groups.
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      The isotope ratios of $^{13}C/^{12}C$ and $^{18}O/^{16}O$ for a sample in a mass spectrometer are measured relative to those of a pure $CO_2$ reference gas (i.e., laboratory working standard). Thus, the calibration of a laboratory working standard gas...

      The isotope ratios of $^{13}C/^{12}C$ and $^{18}O/^{16}O$ for a sample in a mass spectrometer are measured relative to those of a pure $CO_2$ reference gas (i.e., laboratory working standard). Thus, the calibration of a laboratory working standard gas to the international isotope scales (Pee Dee Belemnite (PDB) for ${\delta}^{13}C$ and Vienna Standard Mean Ocean Water (V-SMOW) for ${\delta}^{18}O$) is essential for comparisons between data sets obtained by other groups on other mass spectrometers. However, one often finds difficulties in getting well-calibrated standard gases, because of their production time and high price. Additional difficulty is that fractionation processes can occur inside the gas cylinder most likely due to pressure drop in long-term use. Therefore, studies on laboratory production of pure $CO_2$ isotope standard gas from stable solid calcium carbonate standard materials, have been performed. For this study, we propose a method to extract pure $CO_2$ gas without isotope fractionation from a solid calcium carbonate material. The method is similar to that suggested by Coplen et al., (1983), but is better optimized particularly to make a large amount of pure $CO_2$ gas from calcium carbonate material. The $CaCO_3$ releases $CO_2$ in reaction with 100% pure phosphoric acid at $25^{\circ}C$ in a custom designed, evacuated reaction vessel. Here we introduce optimal procedure, reaction conditions, and samples/reactants size for calcium carbonate-phosphoric acid reaction and also provide the details for extracting, purifying and collecting $CO_2$ gas out of the reaction vessel. The measurements for ${\delta}^{18}O$ and ${\delta}^{13}C$ of $CO_2$ were performed at Seoul National University using a stable isotope ratio mass spectrometer (VG Isotech, SIRA Series II) operated in dual-inlet mode. The entire analysis precisions for ${\delta}^{18}O$ and ${\delta}^{13}C$ were evaluated based on the standard deviations of multiple measurements on 15 separate samples of purified $CO_2$. The pure $CO_2$ samples were taken from 100-mg aliquots of a solid calcium carbonate (Solenhofen-ori $CaCO_3$) during 8-day experimental period. The multiple measurements yielded the $1{\sigma}$ precisions of ${\pm}0.01$‰ for ${\delta}^{13}C$ and ${\pm}0.05$‰ for ${\delta}^{18}O$, comparable to the internal instrumental precisions of SIRA. Therefore, we conclude the method proposed in this study can serve as a way to produce an accurate secondary and/or laboratory $CO_2$ standard gas. We hope this study helps resolve difficulties in placing a laboratory working standard onto the international isotope scales and does make accurate comparisons with other data sets from other groups.

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      참고문헌 (Reference)

      1 Urey H. C., 62 : 399-, 1951

      2 Lorius, C., "The ice-core record: Climate sensitivity and future greenhouse warming" 347 : 139-145, 1990

      3 Crowley, T. J., "The geological record of climatic change" 21 : 828-877, 1983

      4 Keeling, C. D., "The concentration and isotopic abundance of atmospheric carbon dioxide in rural areas" 13 : 322-334, 1958

      5 Rundel, R. W., "Stable Isotopes in Ecological Research" Springer-Verlay 513-, 1988

      6 Epstein, S., "Revised carbonate-water isotopic temperature scale" 64 : 1315-1325, 1953

      7 Kroopnick, P., "Oxygen isotope fractionation in dissolved oxygen in the deep sea" 32 : 375-388, 1976

      8 Kim, K. -R., "Nitrogen-15 and Oxygen-18 Characteristics of Nitrous Oxide: A Global Perspective" 267 : 1855-1857, 1993

      9 Shelly A. Rayback, "Multiproxy reconstructions of climate for three sites in the Canadian High Arctic using Cassiope tetragona" 114 : 593-619, 2012

      10 Craig, H., "Isotopic variations in meteoric waters" 133 : 1702-1703, 1961

      1 Urey H. C., 62 : 399-, 1951

      2 Lorius, C., "The ice-core record: Climate sensitivity and future greenhouse warming" 347 : 139-145, 1990

      3 Crowley, T. J., "The geological record of climatic change" 21 : 828-877, 1983

      4 Keeling, C. D., "The concentration and isotopic abundance of atmospheric carbon dioxide in rural areas" 13 : 322-334, 1958

      5 Rundel, R. W., "Stable Isotopes in Ecological Research" Springer-Verlay 513-, 1988

      6 Epstein, S., "Revised carbonate-water isotopic temperature scale" 64 : 1315-1325, 1953

      7 Kroopnick, P., "Oxygen isotope fractionation in dissolved oxygen in the deep sea" 32 : 375-388, 1976

      8 Kim, K. -R., "Nitrogen-15 and Oxygen-18 Characteristics of Nitrous Oxide: A Global Perspective" 267 : 1855-1857, 1993

      9 Shelly A. Rayback, "Multiproxy reconstructions of climate for three sites in the Canadian High Arctic using Cassiope tetragona" 114 : 593-619, 2012

      10 Craig, H., "Isotopic variations in meteoric waters" 133 : 1702-1703, 1961

      11 Koch, PL., "Isotopic study of the biology of modern and fossil vertebrates, Stable Isotopes in Ecology and Environmental Science" 99-139, 2007

      12 Kim, K. H., "Geochemistry" Minumsa 442-, 1996

      13 Ferronsky, V. I., "Environmental Isotopes in the Hydrosphere" John Wiley & Sons. Ltd 466-, 1982

      14 Coplen T.B., "Comparison of stable isotope reference samples" 302 : 236-238, 1983

      15 Kuang H., "Carbon and Oxygen Isotopic Stratigraphy of Mesoproterozoic Carbonate Sequences (1.6–1.4 Ga) from Yanshan in North China" 1-11, 2011

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2027 평가예정 재인증평가 신청대상 (재인증)
      2021-01-01 평가 등재학술지 유지 (재인증) KCI등재
      2018-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2015-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2011-01-01 평가 등재 1차 FAIL (등재유지) KCI등재
      2009-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2007-09-04 학술지명변경 외국어명 : 미등록 -> JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY KCI등재
      2006-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2005-05-30 학술지명변경 한글명 : 한국해양학회지 바다 -> 바다 KCI등재후보
      2005-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
      2004-01-01 평가 등재후보학술지 유지 (등재후보2차) KCI등재후보
      2003-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
      2002-01-01 평가 등재후보학술지 유지 (등재후보1차) KCI등재후보
      1999-07-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.6 0.6 0.56
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.54 0.59 0.933 0.13
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