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Correction for the 17O interference in δ(13C) measurements when analyzing CO2 with stable isotope mass spectrometry (IUPAC Technical Report)
Open accessAbstract
Measurements of δ( 13 C) determined on CO 2 with an isotope-ratio mass spectrometer (IRMS) must be corrected for the amount of 17 O in the CO 2 . For data consistency, this must be done using identical methods by different laboratories. This report aims at unifying data treatment for CO 2 IRMS by proposing (i) a unified set of numerical values, and (ii) a unified correction algorithm, based on a simple, linear approximation formula. Because the oxygen of natural CO 2 is derived mostly from the global water pool, it is recommended that a value of 0.528 be employed for the factor λ, which relates differences in 17 O and 18 O abundances. With the currently accepted N ( 13 C)/ N ( 12 C) of 0.011 180(28) in VPDB (Vienna Peedee belemnite) reevaluation of data yields a value of 0.000 393(1) for the oxygen isotope ratio N ( 17 O)/ N ( 16 O) of the evolved CO 2 . The ratio of these quantities, a ratio of isotope ratios, is essential for the 17 O abundance correction: [ N ( 17 O)/ N ( 16 O)]/[ N ( 13 C)/ N ( 12 C)] = 0.035 16(8). The equation [δ( 13 C) ≍ 45 δ VPDB-CO2 + 2 17 R / 13 R ( 45 δ VPDB-CO2 – λ 46 δ VPDB-CO2 )] closely approximates δ( 13 C) values with less than 0.010 ‰ deviation for normal oxygen-bearing materials and no more than 0.026 ‰ in extreme cases. Other materials containing oxygen of non-mass-dependent isotope composition require a more specific data treatment. A similar linear approximation is also suggested for δ( 18 O). The linear approximations are easy to implement in a data spreadsheet, and also help in generating a simplified uncertainty budget.
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“Due to the possible large uncertainties related to Assonov 17 O calibration parameters (50-53), we calculated raw Δ 47 values using the 17 O calibration parameters reported in ref. 53, which have been shown to improve interlaboratory data consistency (54).”
From Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the "dolomite problem" (2020) · cites this paper as [53]
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“The preceding interlaboratory bias correction of the temperature calibration for dolomites based on a single standard may not be optimal, but it is still better for Δ 47 temperature calculations than direct use of the original calibration in ref. 50, which was not given in the Brand parametric framework nor calibrated to the ETH standard values reported in ref. 53.”
From Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the "dolomite problem" (2020) · cites this paper as [53]
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Items 101–200 of 284
Zhang, N., Yamada, K., Kano, A., Matsumoto, R., & Yoshida, N. (2018) · Chemical Geology · doi:10.1016/j.chemgeo.2018.05.001 · Cited by 21
Xia, L.-J., Zhou, L.-X., Tans, P., Liu, L.-X., Zhang, G., Wang, H.-Y., & Luan, T. (2015) · doi:10.1016/j.atmosenv.2015.07.008 · Cited by 21
Pilecky, M., Wassenaar, L., Taipale, S., & Kainz, M. (2023) · MethodsX · doi:10.1016/j.mex.2023.102283 · Cited by 20
Fosu, B. R., Ghosh, P., & Viladkar, S. G. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.01.020 · Cited by 19
Mangenot, X., Deçoninck, J., Bonifacie, M., Rouchon, V., Collin, P., Quesne, D., Gasparrini, M., & Sizun, J. (2018) · Basin Research · doi:10.1111/bre.12324 · Cited by 21
“Note that using the 17O parameters from Brand, Assonov, and Coplen (2010) would only lead to small differences in Δ47 values of both of our standards and samples (i.e. less than ±0.010‰), well within the analytical uncertainty on Δ47 measurements.”
MethodInfluentialBahnan, A. E., Carpentier, C., Pironon, J., Ford, M., Ducoux, M., Barré, G., Mangenot, X., & Gaucher, E. (2020) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2019.08.047 · Cited by 20
Tagliavento, M., John, C., Anderskouv, K., & Stemmerik, L. (2020) · Sedimentology · doi:10.1111/sed.12802 · Cited by 19
“For 17O correction, parameters from Brand et al. (2010) as reported in Da€eron et al. (2016) were used.”
MethodZhang, N., Lin, M., Yamada, K., Kano, A., Liu, Q., Yoshida, N., & Matsumoto, R. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119352 · Cited by 22
Quade, J., Rasbury, E., Huntington, K., Hudson, A., Vonhof, H., Anchukaitis, K., Betancourt, J., Latorre, C., & Pepper, M. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.05.004 · Cited by 19
“∆47 values were calculated using the methods of Huntington et al. (2009), with the exception that data were calculated using the 17 O correction parameters of Brand et al. (2010), as recommended by Schauer et al. (2016) and Daëron et al. (2016).”
MethodThaler, C., Katz, A., Bonifacie, M., Ménez, B., & Ader, M. (2020) · Biogeosciences · doi:10.5194/bg-17-1731-2020 · Cited by 18
Li, P., Zou, H., Hao, F., Yu, X., Wang, G., & Eiler, J. M. (2020) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2020.104660 · Cited by 19
Thaler, C., Katz, A., Bonifacie, M., Ménez, B., & Ader, M. (2019) · Biogeosciences · doi:10.5194/bg-2019-461-supplement · Cited by 18
“For the correction from 17O interferences, we used the 17O correction parameters from Brand et al. (2010), as recently recommended (Daëron et al., 2016; Schauer et al., 2016).”
MethodChang, B., Defliese, W. F., Li, C., Huang, J., Tripati, A., & Algeo, T. J. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8678 · Cited by 17
Three certified sugar reference materials for carbon isotope delta measurements
Chartrand, M. M. G., Meija, J., Kumkrong, P., & Mester, Z. (2018) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8357 · Cited by 25
Dunn, P. J. H., Malinovsky, D., & Infante, H. G. (2014) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-014-7926-1 · Cited by 22
Katō, H., Amekawa, S., Kano, A., Mori, T., Kuwahara, Y., & Quade, J. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.10.016 · Cited by 25
O'Hora, H., Petersen, S., Vellekoop, J., Jones, M. M., & Scholz, S. R. (2022) · Climate of the past · doi:10.5194/cp-18-1963-2022 · Cited by 20
“As above, raw beam intensities of masses 44–49 were converted to bulk isotopic values (δ45 to δ49) and clumped isotopic values (147, 148, and 149) using IUPAC (Brand) parameters (Brand et al., 2010) with an R code presented in Petersen et al.”
MethodPaleotemperature reconstructions using speleothem fluid inclusion analyses from Hungary
Demény, A., Rinyu, L., Kern, Z., Hatvani, I. G., Czuppon, G., Surányi, G., Leél‐Őssy, S., Shen, C., & Koltai, G. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2020.120051 · Cited by 35
“…2016), using the CO2 clumped ETH PBL replicate analyses method and “Brand parameters” (Baertschi, 1976; Gonfiantini et al., 1995; Meijer and Li, 1998; Assonov and Brenninkmeijer, 2003; Brand et al., 2010), also called the “IUPAC” parameters (International Union of Pure and Applied Chemistry).”
MethodTörök, Á., Claes, H., Brogi, A., Liotta, D., Tóth, Á., Mindszenty, A., Kudó, I., Kele, S., Huntington, K. W., Shen, C., et al. (2019) · Geomorphology · doi:10.1016/j.geomorph.2019.106836 · Cited by 19
Srivastava, A., & Verkouteren, R. M. (2018) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-018-1064-0 · Cited by 19
Absolute age and temperature of belemnite rostra: Constraints on the Early Cretaceous cooling event
Wang, T., Yang, P., He, S., Hoffmann, R., Zhang, Q., Farnsworth, A., Feng, Y., Randrianaly, H. N., Xie, J., Yue, Y., et al. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104353 · Cited by 21
Davies, A., Davis, S., & John, C. M. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120317 · Cited by 19
Leaf-scale quantification of the effect of photosynthetic gas exchange on Δ17O of atmospheric CO2
Adnew, G., Pons, T., Koren, G., Peters, W., & Röckmann, T. (2020) · Biogeosciences · doi:10.5194/egusphere-egu2020-3064 · Cited by 16
“117O= ln ( δ17O+ 1 ) − λ× ln ( δ18O+ 1 ) (3) The choice of λ is in principle arbitrary, and in this study we use λ= 0.528, which was established for meteoric waters (Meijer and Li, 1998; Landais et al., 2008; Brand et al., 2010; Luz and Barkan, 2010; Barkan and Luz, 2012; Sharp et al., 2018).”
BackgroundMethodInfluentialLessons learned from inter-laboratory studies of carbon isotope analysis of honey
Dunn, P. J. H., Hill, S., Cowen, S., Infante, H. G., Sargent, M., Gören, A. C., Bílsel, M., Şimşek, A., Ogrinc, N., Potočnik, D., et al. (2018) · Science & Justice · doi:10.1016/j.scijus.2018.08.003 · Cited by 20
“The final approach, which is endorsed by the Commission on Isotopic Abundances and Atomic Weights (CIAAW) of the International Union of Pure and Applied Chemistry (IUPAC), is a linear approximation rather than an exact solution and also uses more up-to-date values for the absolute isotope ratios of VPDB than the SSH a…”
MethodLacroix, B. J., Baumgartner, L. P., Bouvier, A., Kempton, P. D., & Vennemann, T. W. (2018) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2018.09.016 · Cited by 20
Isotope exchange rates in dissolved inorganic carbon between 40 °C and 90 °C
Weise, A., & Kluge, T. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.09.032 · Cited by 19
Peral, M., Bassinot, F., Daëron, M., Blamart, D., Bonnin, J., Jorissen, F. J., Kissel, C., Michel, É., Waelbroeck, C., Rebaubier, H., et al. (2022) · EarthArXiv (California Digital Library) · doi:10.1016/j.gca.2022.10.030
Harper, D., Suarez, M., Uglesich, J., You, H., Li, D.-Q., & Dodson, P. (2021) · Climate of the Past · doi:10.5194/cp-17-1607-2021 · Cited by 15
Bajnai, D., Coplen, T. B., Methner, K., Löffler, N., Krsnik, E., & Fiebig, J. (2021) · Geophysical Research Letters · doi:10.1029/2021gl093257 · Cited by 19
Self-citationTriple oxygen isotope distribution in modern mammal teeth and potential geologic applications
Lehmann, S., Levin, N., Passey, B., Hu, H.-T., Cerling, T., Miller, J., Arppe, L., Beverly, E., Hoppe, K. A., Huth, T., et al. (2021) · Geochimica et Cosmochimica Acta · doi:10.1002/essoar.10506275.1 · Cited by 15
Acid digestion of carbonates using break seal method for clumped isotope analysis
Fosu, B. R., Ghosh, P., Mishra, D., Banerjee, Y., Prasanna, K., & Sarkar, A. (2018) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8304 · Cited by 21
Malinovsky, D., Dunn, P. J. H., Holcombe, G., Cowen, S., & Infante, H. G. (2018) · Journal of Analytical Atomic Spectrometry · doi:10.1039/c8ja00281a · Cited by 33
Assessment of Factors Controlling Clumped Isotopes and δ18O Values of Hydrothermal Vent Calcites
Kluge, T., John, C. M., Boch, R., & Kele, S. (2018) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2017gc006969 · Cited by 14
“Assessing the updated isotope parameters of Brand et al. (2010) for evaluation did not show large differences for the selected data set (supporting information).”
BackgroundWichern, N., de Winter, N. D., Johnson, A., Goolaerts, S., Wesselingh, F., Hamers, M., Kaskes, P., Claeys, P., & Ziegler, M. (2023) · Biogeosciences · doi:10.5194/bg-20-2317-2023 · Cited by 14
“The calculated δ values were then corrected for 17O using the values presented in Brand et al. (2010).”
MethodClumped isotopic compositions of cultured and natural land-snail shells and their implications
Dong, J., Eiler, J. M., An, Z., Li, X., Liu, W., & Hu, J. (2021) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2021.110530 · Cited by 16
Yao, P., Ni, H., Paul, D., Mašalaitė, A., Huang, R., Meijer, H. A. J., & Dusek, U. (2021) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2021.150031 · Cited by 17
Dennis, P., Myhill, D. J., Marca, A., & Kirk, R. (2018) · Journal of the Geological Society · doi:10.1144/jgs2016-117 · Cited by 14
“Recent attempts to standardize data correction using the ratio values and parameters suggested by Brand et al. (2010) indicate that much of the discrepancy between studies is eliminated.”
Pliocene CO2 rise due to sea-level fall as a mechanism for the delayed ice age
Yang, S.-L., Wang, Y.-D., Huang, X.-F., Sun, M., Han, J.-T., Wang, X., Chen, Z.-L., Zhang, S., Jiang, W.-Y., Tang, Z., et al. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2024.104431 · Cited by 13
Wang, T., Hoffmann, R., He, S., Zhang, Q., Li, G., Randrianaly, H. N., Xie, J., Yue, Y., & Ding, L. (2023) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104220 · Cited by 16
Nehme, C., Todisco, D., Breitenbach, S., Couchoud, I., Marchegiano, M., Peral, M., Vonhof, H., Hellstrom, J., Tjallingi, R., Claeys, P., et al. (2023) · Social Science Research Network · doi:10.2139/ssrn.4172978 · Cited by 13
High-dimensional isotomics, part 1: A mathematical framework for isotomics
Csernica, T., & Eiler, J. (2022) · Chemical Geology · doi:10.1016/j.chemgeo.2022.121235 · Cited by 13
Brenner, D. C., Passey, B. H., Holder, R., & Viete, D. R. (2021) · Geochemistry Geophysics Geosystems · doi:10.1029/2020gc009238 · Cited by 14
Peral, M., Blamart, D., Bassinot, F., Daëron, M., Dewilde, F., Rebaubier, H., Nomade, S., Girone, A., Marino, M., Maiorano, P., et al. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2020.109603 · Cited by 14
Kelson, J. R., Watford, D., Bataille, C. P., Huntington, K. W., Hyland, E. G., & Bowen, G. J. (2018) · Paleoceanography and Paleoclimatology · doi:10.1029/2018pa003391 · Cited by 17
“Our Δ47 values are calculated using updated 17O correction parameters (Brand et al., 2010) following recent recommendations (Daëron et al., 2016; Schauer et al., 2016) and are normalized to the absolute reference frame (Dennis et al., 2011), which is now standard practice.”
MethodTaking the Temperature of Hydrothermal Ore Deposits Using Clumped Isotope Thermometry
Mering, J. A., Barker, S. L. L., Huntington, K. W., Simmons, S., Dipple, G., Andrew, B., & Schauer, A. (2018) · Economic Geology · doi:10.5382/econgeo.2018.4608 · Cited by 13
“The CDES-corrected D47 values are converted to temperature using the Kluge et al. (2015) relationship recalculated using Brand et al. (2010) 17O correction parameters.”
Nomura, S., Naja, M., Ahmed, M. K., Mukai, H., Terao, Y., Machida, T., Sasakawa, M., & Patra, P. (2021) · doi:10.5194/acp-2021-317 · Cited by 12
“The δ(18)O-CO2 for atmospheric CO2 in this study is expressed against the value of CO2 evolved from VPDB calcite (i.e., VPDB-CO2 scale, IAEA, 1993; Brand et al., 2010).”
MethodKele, S., Sallam, E., Capezzuoli, E., Rogerson, M., Wanas, H., Shen, C.-C., Lone, M., Yu, T.-L., Schauer, A., & Huntington, K. (2020) · Journal of the Geological Society · doi:10.1144/jgs2020-147 · Cited by 12
Parrish, J. T., Hyland, E. G., Chan, M. A., & Hasiotis, S. T. (2018) · Sedimentology · doi:10.1111/sed.12540 · Cited by 13
“These values are reported in the absolute reference frame (ARF; Dennis et al., 2011), with oxygen isotope (Brand et al., 2010) corrections recommended in Da€eron et al. (2016) and Schauer et al. (2016).”
BackgroundCCQM-K140: carbon stable isotope ratio delta values in honey
Dunn, P., Goenaga-Infante, H., Gören, A., Simsek, A., Bilsel, M., Ogrinc, N., Armishaw, P., & Hai, L. (2017) · doi:10.1088/0026-1394/54/1a/08005 · Cited by 12
“The final approach is the 17O algorithm endorsed by IUPAC which is a linear approximation rather than an exact solution and also uses more up-to-date values for the absolute isotope ratios of VPDB than the SSH approach (Brand et al, 2010).”
MethodInfluentialSaenger, C. P., Schauer, A. J., Heitmann, E. O., Huntington, K. W., & Steig, E. J. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120059 · Cited by 11
Swart, P., Mackenzie, G., Eberli, G., Lüdmann, T., & Betzler, C. (2019) · Sedimentology · doi:10.1111/sed.12580 · Cited by 11
“The CO2 gas produced from the carbonate was calibrated using NBS-19 (National Bureau of Standards) corrected for the usual isobaric interferences (Brand et al., 2010) and reported relative to VPDB (Vienna Pee-Dee Belemnite) using the conventional notation.”
MethodYue, J., Xiao, J., Wang, X., Meckler, A. N., Modestou, S., & Fan, J. (2022) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2022.107767 · Cited by 11
Suarez, M., Knight, J. A., Godet, A., Ludvigson, G., Snell, K., Murphy, L., & Kirkland, J. (2020) · Special Publications · doi:10.1144/sp507-2020-85 · Cited by 10
“…19.8 (+4.6) RRR-44B 5 −5.5 −7.4 RRR-44C 5 −5 −8.6 RRR-50A2 5 −5.2 −8.9 0.672 (0.012) −4.79 −9.24 31 (+3.5) RRR-50B2 5 −5.2 −8.8 Temperatures are calculated for Δ47 values corrected to CDES, as described by Dennis et al. (2011), and with Brand et al. (2010) 17O correction and utilizing the acid…”
MethodInfluentialPeral, M., Marchegiano, M., Verheyden, S., Goderis, S., Helden, T. V., Vanhaecke, F., Acker, T. V., Jia, X., Cheng, H., Fiebig, J., et al. (2024) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2024.108564 · Cited by 9
Sun, Z., Perez-Beltran, S., Zaheer, W., Defliese, W. F., Banerjee, S., & Grossman, E. L. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.118467 · Cited by 10
Parvez, Z. A., El-Shenawy, M., Lucarelli, J., Kim, S.-T., Johnson, K., Wright, K., Gebregiorgis, D., Montanez, I. P., Wortham, B., Asrat, A., et al. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.11.017 · Cited by 9
Parvez, Z. A., Lucarelli, J. K., Matamoros, I. W., Rubi, J., Miguel, K., Elliott, B., Flores, R., Ulrich, R. N., Eagle, R. A., Watkins, J. M., et al. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.06.022 · Cited by 9
Temovski, M., Rinyu, L., Futó, I., Molnár, K., Túri, M., Demény, A., Otoničar, B., Dublyansky, Y. V., Audra, P., Polyak, V. J., et al. (2022) · Scientific Reports · doi:10.1038/s41598-022-12929-4 · Cited by 10
Kato, H., Amekawa, S., Hori, M., Shen, C.-C., Kuwahara, Y., Senda, R., & Kano, A. (2021) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2020.106746 · Cited by 9
Recalculation of stable isotope expressions for HCNOS: EasyIsoCalculator
Skrzypek, G., & Dunn, P. J. H. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8892 · Cited by 12
Leitner, S., Hood-Nowotny, R. C., & Watzinger, A. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8929 · Cited by 12
Skrzypek, G., & Dunn, P. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8890 · Cited by 9
Exploring the Temperature Dependence of Clumped Isotopes in Modern Porites Corals
Guo, Y., Deng, W., Wei, G., Chen, X., Liu, X., Wang, X., Lo, L., Cai, G., & Zeng, T. (2019) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2019jg005402 · Cited by 8
“The 17O correction method of Brand et al. (2010) was used during the data calculation as previous studies (Daëron et al., 2016; Schauer et al., 2016).”
MethodGagnon, C. A., Butler, K. L., Robertson, K., Emproto, C. R., Gans, P. B., Eden, R., Ibarra, D. E., & Benson, T. R. (2025) · Economic Geology · doi:10.5382/econgeo.5174 · Cited by 2
Seep carbonate clumped isotopes revealing ocean warming-induced gas hydrate dissociation
Liu, L., Guan, H., Wu, N.-Y., Chang, B., Chen, F.-Q., Feng, D., & Li, S. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2024.104439 · Cited by 8
Marchegiano, M., Peral, M., Venderickx, J., Martens, K., García‐Alix, A., Snoeck, C., Goderis, S., & Claeys, P. (2024) · Geophysical Research Letters · doi:10.1029/2023gl107426 · Cited by 16
“The raw measured Δ 47 values are processed using the IUPAC Brand's isotopic parameters (Brand et al., 2010; Daëron et al., 2016; Petersen et al., 2019) and converted to the ICDES 90° C scale, using the most recent values for the ETH‐1, ETH‐2, and ETH‐3 carbonate reference materials (Ber-nasconi et…”
MethodCalibration of the carbonate clumped isotope thermometer of land snail shells
Bao, R., Sheng, X., Li, C., Cui, C., Yan, H., Ji, J., & Chen, J. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121773 · Cited by 8
Taylor, V., Wilson, P. A., Bohaty, S. M., & Meckler, A. N. (2023) · Paleoceanography and Paleoclimatology · doi:10.1029/2023pa004650 · Cited by 10
“We used the IUPAC 17O correction parameters (Brand et al., 2010; Daëron et al., 2016) and all raw data processing was performed using the Easotope software package (John & Bowen, 2016).”
Mutlu, H., Karabacak, V., Deniz, K., & Erkkila, B. R. (2022) · Applied Geochemistry · doi:10.1016/j.apgeochem.2022.105260 · Cited by 8
Tracing carbon and nitrogen microbial assimilation in suspended particles in freshwaters
Mena‐Rivera, L., Lloyd, C. E. M., Reay, M. K., Goodall, T., Read, D. S., Johnes, P. J., & Evershed, R. P. (2022) · Biogeochemistry · doi:10.1007/s10533-022-00915-x · Cited by 9
Ning, Z., Zhang, L., Huntington, K. W., Wang, C., Dai, J., Han, Z., Passey, B. H., Qian, X., & Zhang, J. (2018) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2018.12.009 · Cited by 8
“Δ47 calculations were made using the methods of Huntington et al. (2009), except that the 17O correction parameters of Brand et al. (2010) were used based on the recommendations of Daëron et al. (2016) and Schauer et al. (2016), with R13 (VPDB) of 0.011180, R17 (VSMOW) of 0.00038475, and the λ…”
MethodInfluentialClumped isotope measurements reveal aerobic oxidation of methane below the Greenland ice sheet
Adnew, G., Röckmann, T., Blunier, T., Jørgensen, C., Sapper, S., van der Veen, C., Sivan, M., Popa, M. E., & Christiansen, J. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.11.009 · Cited by 7
Chaillot, J., Kassi, S., Clauzel, T., Pesnin, M., Casado, M., Landais, A., & Daëron, M. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122450 · Cited by 9
Guo, Y.-R., Kong, K., Liu, X., Deng, W.-F., & Wei, G.-J. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122036 · Cited by 7
Prasanna, K., Ghosh, P., Eagle, R., Tripati, A., Kapur, V., Feeney, R. F., Fosu, B., & Mishra, D. (2021) · Geochemistry Geophysics Geosystems · doi:10.1029/2020gc009601 · Cited by 7
Leaf scale quantification of the effect of photosynthetic gas exchange on Δ47of CO2
Adnew, G., Hofmann, M., Pons, T., Koren, G., Ziegler, M., Lourens, L., & Röckmann, T. (2021) · Scientific Reports · doi:10.1038/s41598-021-93092-0 · Cited by 7
Savard, M., Jautzy, J., Lavoie, D., Dhillon, R., & Defliese, W. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.01.041 · Cited by 7
Sperlich, P., Moossen, H., Geilmann, H., Bury, S., Brown, J. C. S., Moss, R., Brailsford, G., & Brand, W. (2020) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8944 · Cited by 7
Self-citationModeling the Measurement: Δ47, Corrections, and Absolute Ratios for Reference Materials
Olack, G. A., & Colman, A. S. (2019) · Geochemistry Geophysics Geosystems · doi:10.1029/2018gc008166 · Cited by 8
“…were developed (Affek & Eiler, 2006; Huntington et al., 2009) before the 2010 paper describing the new values for the 17O and 18O relationship (Brand et al., 2010) and used the previously accepted values (Gonfiantini et al., 1995) along with the updated value for 13RVPDB (Coplen et al.,…”
BackgroundMethodResultInfluentialHu, B., Gao, J.-F., Fan, C., Li, Y.-H., Qin, Y.-J., Zhao, Y., & Tian, Y.-R. (2018) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8289 · Cited by 7
Temperature dependence of the kinetic isotope effect in -pinene ozonolysis
Gensch, I., Laumer, W., Stein, O., Kammer, B., Hohaus, T., Saathoff, H., Wegener, R., Wahner, A., & Kiendler-Scharr, A. (2011) · doi:10.1029/2011jd016084 · Cited by 7
“[15] The ion currents at mass‐to‐charge ratios m/z 44, 45 and 46 were corrected for the contribution of (17)O‐containing isotopologues [Brand et al., 2010].”
MethodQuantifying the impacts of rainfall and evaporation on Lake Bonneville
Mering, J., Arnold, A. J., Chari, L., Lee, H., Lerback, J., Ajoku, O., Ibarra, D., Nelson, S. T., Farnsworth, A., Valdes, P., et al. (2026) · Science Advances · doi:10.1126/sciadv.adw4951 · Cited by 6
“Data were processed using the Easotope software using the brand parameter set ( 58 , 59 ).”
Chirakal, T., Messaoud, J. H., Alibrahim, A., Ibrahim, K., Grélaud, C., Kalifi, A., Powell, J., & van Buchem, F. (2025) · Cretaceous research (Print) · doi:10.1016/j.cretres.2025.106207 · Cited by 6
Adineh, S., Závada, P., Mukherjee, S., Bruthans, J., & Zare, M. (2024) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2024.107228 · Cited by 6
Affek, H., Vieten, R., Barkan, E., Levi, Y., Ayalon, A., Bar-Matthews, M., Fishman, E., & Assor, A. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.118366 · Cited by 6
Kato, H., Mori, T., Amekawa, S., Wu, C.-C., Shen, C.-C., & Kano, A. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121390 · Cited by 6
Quesnel, B., Jautzy, J. J., Scheffer, C., Raymond, G., Beaudoin, G., Jørgensen, T. R. C., & Pinet, N. (2022) · Chemical Geology · doi:10.1016/j.chemgeo.2022.121099 · Cited by 7
Final report on CCQM-K167: carbon isotope delta measurements of vanillin
Chartrand, M., Chubchenko, I., Dunn, P., Garrido, B., Lu, H., Liu, F.-H., Ogrinc, N., Simsek, A., Fasciotti, M., Goenaga-Infante, H., et al. (2022) · Metrologia · doi:10.1088/0026-1394/59/1a/08004 · Cited by 6
“In the instructions to participants, it was stated that the (17)O correction should be done using the procedure recommended by IUPAC [17].”
MethodModeling Bioavailability Limitations of Atrazine Degradation in Soils
Chávez-Rodríguez, L., Ingalls, B., Meierdierks, J., Kundu, K., Streck, T., & Pagel, H. (2021) · Frontiers in Environmental Science · doi:10.3389/fenvs.2021.706457 · Cited by 6
Mizera, M., Little, T., Boulton, C., Katzir, Y., Thiagarajan, N., Prior, D., Biemiller, J., & Smith, E. (2021) · Journal of Geophysical Research - Solid Earth · doi:10.1029/2021jb021916 · Cited by 6
Defliese, W., & Tripati, A. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8666 · Cited by 6
Dunn, P. J. H., Bílsel, M., Şimşek, A., Gören, A. C., Tunç, M., Ogrinc, N., Horvat, M., & Infante, H. G. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8453 · Cited by 6
Affek, H. P., Barkan, E., Tal, Y., Steidle, S. D., Wendt, K. A., Spötl, C., Edwards, R. L., Fishman, E., & Dublyansky, Y. V. (2025) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2025.119528 · Cited by 6
Curley, A. N., Petersen, S., Fricke, H., & Gleason, J. D. (2024) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2024.119180 · Cited by 6
Fabbi, S., Borrelli, M., Innamorati, G., Aldega, L., Daëron, M., Perri, E., & Santantonio, M. (2024) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2024.107115 · Cited by 5
13CH4/12CH4 sensing using Raman spectroscopy.
Petrov, D. V., & Tanichev, A. (2024) · Spectrochimica Acta Part A - Molecular and Biomolecular Spectroscopy · doi:10.1016/j.saa.2024.124253 · Cited by 5
Minnebo, L., Winkelstern, I., Zhang, J. Z., & Petersen, S. (2024) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2024.112195 · Cited by 5
Isotopic measurements of carbon dioxide: the role of measurement science and standards
Meija, J. (2023) · Analytical and Bioanalytical Chemistry · doi:10.1007/s00216-023-05000-2 · Cited by 11
Mangenot, X., Larmier, S., Girard, J.-P., Dyja-Person, V., & Eiler, J. M. (2023) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2023.106630 · Cited by 4
Sanders, C., Eiler, J. C., & Grotzinger, J. P. (2022) · Sedimentary Geology · doi:10.1016/j.sedgeo.2022.106316 · Cited by 5
Metadata
- Authors
- Brand, W. A., Assonov, S. S., & Coplen, T. B.
- Affiliations
- Max Planck Society (DE)
- European Commission (BE)
- United States Geological Survey (US)
- Venue
- Pure and Applied Chemistry
- Publisher
- Walter de Gruyter GmbH
- Published
- 2010-05-26
- Volume
- 82
- Issue
- 8
- Pages
- 1719-1733
- ISSN
- 0033-4545 (ISSN-L)
- 1365-3075
- OpenAlex
- W2129805855
- Cited by
- 385
- References
- 27
- Citations by year
- 2026: 20 · 2025: 27 · 2024: 38 · 2023: 45 · 2022: 48 · 2021: 52 · 2020: 36 · 2019: 36 · 2018: 36 · 2017: 20 · 2016: 6 · 2015: 4 · 2014: 3 · 2013: 5 · 2012: 6
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Pure and Applied Chemistry (publishedVersion)
- Joint Research Centre (European Commission) (submittedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric and Environmental Gas Dynamics
- Physical Sciences › Physics and Astronomy › Instrumentation › Scientific Measurement and Uncertainty Evaluation
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- carbon-13 stable isotopes, carbon dioxide, isotope ratio mass spectrometry, oxygen isotope ratios, uncertainty budget
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