INTERNATIONAL UNION OF PURE AND APPLIED CHEMISTRY INORGANIC CHEMISTRY DIVISIOI COMMISSION ON ATOMIC WEIGHTS AND ISOTOPIC ABUNDANCES* SUBCOMMITTEE FOR ISOTOPIC ABUNDANCE MEASUREMENTS *N ISOTOPIC COMPOSITIONS OF THE ELEMENTS 1997 by KJR ROSMAN AND PDP TAYLOR2 Department of Applied Physics, Curtin University of Technology, GPO Box U1987, Perth 6001 australia 2Institute for Reference Materials and Measurements, European Commission-JRC, B-2440Geel Belgium Membership of the Commission for the period 1996-1997 was as follows L. Schultz (FRG, Chairman); R D. Vocke, Jr ( USA, Secretary); J.K. Bohlke(USA, Associate), H.J. Dietze (FRG, Associate); T. Ding(China, Associate) M. Ebihara(Japan, Titular); J W. Gramlich (USA, Associate A N. Halliday (USA, Associate), H. R Krouse( Canada, Titular ); H K Kluge(FRG, Associate,R D. Loss (Australia, Titular): G. I. Ramendik(Russia, Titular); D. E. Richardson(USA, Associate); M. Stievenard (France, Associate); P. D. P. Taylor( Belgium, Titular), J. R de Laeter(Australia, National Representative); P De Bievre(Belgium, National Representative Y. Xiao(China, National Representative); M. Shima (Japan, National Representative), A. Pres de matos(Portugal, National Representative); N.N. Greenwood (UK National Representative), H. S Peiser (USA, National Representative) Membership of the Subcommittee for Isotopic Abundance Measurements 1991-1997: P. D. P. Taylor (Belgium, Chairman 1995-97;R. D. Loss(Australia, Secretary 1995-97): Members: P De Bievre myI o AIrone d do/Autroli u i ni (EDa M CKihoro /TononI III
INTERNATIONAL UNION OF PURE AND APPLIED CHEMISTRY INORGANIC CHEMISTRY DIVISION COMMISSION ON ATOMIC WEIGHTS AND ISOTOPIC ABUNDANCES* SUBCOMMITTEE FOR ISOTOPIC ABUNDANCE MEASUREMENTS** ISOTOPIC COMPOSITIONS OF THE ELEMENTS 1997 Prepared for publication by K.J.R. ROSMAN1 AND P.D.P. TAYLOR2 1 Department of Applied Physics, Curtin University of Technology, GPO Box U1987, Perth 6001, Australia. 2 Institute for Reference Materials and Measurements, European Commission-JRC, B-2440 Geel, Belgium. * Membership of the Commission for the period 1996–1997 was as follows: L. Schultz ( F RG , Chair m an) ; R. D . V ocke, Jr .( U S A , Secretar y) ; J. K . Böhlke (U S A , A ss ociate) ; H . J . D ietze ( F RG, A s s ociate) ; T. D ing ( China, A s sociate), M . Ebihar a ( J apan, Titular ) ; J . W. G r amlich (U S A , As s ociate) ; A . N. H alliday ( US A , A s sociate), H . R. K r ouse ( Canada, Titular ) ; H .K K luge ( FRG , A s sociate); R. D. Los s ( A ustr alia, T itular ) ; G . I . Ramendik ( Rus s ia, Titular ) ; D. E. Richardson (USA, Associate); M . S tiévenar d ( F r ance, A ss ociate) ; P . D . P . Taylor ( Belgium, Titular ) ; J . R. de Laeter ( A ustr alia, N ational Repr es entative) ; P . D e Bièvr e ( Belgium, N ational Repr es entative); Y . X iao ( China, N ational Repr esentative) ; M . S hima ( J apan, N ational R epr es entative); A . P ir es de M atos ( P or tugal, N ational Repr es entative) ; N . N . G r eenw ood ( U K , N ational Repr es entative); H . S . P eis er ( U S A , N ational Repr es entative) . ** Membership of the Subcommittee for Isotopic Abundance Measurements 1991-1997: P. D. P. Taylor (Belgium, Chairman 1995-97); R. D . Los s ( A us tralia, Secretary 1995-97); Members: P.De Bièvre (Belgium) J Césario (France) J R de Laeter (Australia) H J Dietze (FRG) M Ebihara (Japan) J W
T.J. Murphy (USA), H.S. Peiser(USA), D. E. Richardson (USA), D.J. Rokop (USA), E. R. Roth (France),KJ.R. Rosman(Australia), M. Shima(Japan ),R D. Vocke(USA)
T. J. Murphy (USA), H . S. P eis er ( U S A) , D. E. Richardson (USA), D. J. Rokop (USA), E. R. Roth (France), K. J. R. Rosman (Australia), M . Shima ( Japan ), R. D. Vocke (USA)
ISOTOPIC COMPOSITIONS OF THE ELEMENTS 1997 Abstract- The Commission's Subcommittee for the Isotopic Composition of the Elements(SIAM) has carried out its biennial review of isotopic compositions, as determined by mass spectrometry and other relevant methods. This involves a critical evaluation of the published literature, element by element, and forms the basis of the Table of Isotopic Compositions of the Elements as Determined by Mass Spectrometry presented here. New guidelines have been used to arrive at the uncertainties on the isotopic abundances and there are numerous changes to the Table since it was last published in 1991. Atomic Weights calculated from this table are consistent with Ar(E) values listed in the Table of Standard Atomic Weights 1997 INTRODUCTIO Previous compilations of"The isotopic compositions of the elements"were published in 1983(ref. 1) 1984(ref. 2)and 1991(ref. 3) for the purpose of yielding atomic weights consistent with the Commissions " Table of Standard Atomic Weights"[4, 5, 6 During the past six years the Commission, through its Subcommittee for Isotopic Abundance Measurements(SIAM), has continued to assemble and evaluate new data which has led to improvements to the tabulated isotopic composition of a number of elements. In 1993, the statistical guidelines for assigning uncertainties to the representative abundances were revised and extended by the Commissions Working Party on Statistical Evaluation of Isotopic Abundances(members: K J. R Rosman( Chairman) P De Bievre and J. w. Gramlich). All the data presented in the Table were reassessed according to these guidelines The present table was assembled for publication following the meeting of SIAM held at Kloster Seeor Germany), just prior to the 39th IUPAC General Assembly held at Geneva(Switzerland )in 1997 and is presented here as a companion paper to the Atomic Weights of the Elements 1997 REFERENCES 1. N.E. Holden, R L. Martin and I L. Barnes, Pure Appl. Chem., 55, 1119-1136(1983) 2. N.E. Holden, R.L. Martin and l.L. Barnes, Pure Appl. Chem., 56, 675-694(1984) 3. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 63, 991-1002 (1991) 4. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 55, 1101-1118 (1983) 5. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 56, 653-674 (1984) 6. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 63, 975-990 (1991)
ISOTOPIC COMPOSITIONS OF THE ELEMENTS 1997 Abstract- The Commission’s Subcommittee for the Isotopic Composition of the Elements (SIAM) has carried out its biennial review of isotopic compositions, as determined by mass spectrometry and other relevant methods. This involves a critical evaluation of the published literature, element by element, and forms the basis of the Table of Isotopic Compositions of the Elements as Determined by Mass Spectrometry presented here. New guidelines have been used to arrive at the uncertainties on the isotopic abundances and there are numerous changes to the Table since it was last published in 1991. Atomic Weights calculated from this table are consistent with Ar(E) values listed in the Table of Standard Atomic Weights 1997. INTRODUCTION Previous compilations of “The isotopic compositions of the elements” were published in 1983 (ref. 1), 1984 (ref. 2) and 1991 (ref. 3) for the purpose of yielding atomic weights consistent with the Commission's “Table of Standard Atomic Weights ” [4, 5, 6]. During the past six years the Commission, through its Subcommittee for Isotopic Abundance Measurements (SIAM), has continued to assemble and evaluate new data which has led to improvements to the tabulated isotopic composition of a number of elements. In 1993, the statistical guidelines for assigning uncertainties to the representative abundances were revised and extended by the Commission's Working Party on Statistical Evaluation of Isotopic Abundances (members: K. J. R. Rosman (Chairman), P. De Bièvre and J. W. Gramlich). All the data presented in the Table were reassessed according to these guidelines. The present table was assembled for publication following the meeting of SIAM held at Kloster Seeon (Germany), just prior to the 39th IUPAC General Assembly held at Geneva (Switzerland) in 1997 and is presented here as a companion paper to the Atomic Weights of the Elements 1997. REFERENCES 1. N.E. Holden, R.L. Martin and I.L. Barnes, Pure Appl. Chem., 55, 1119-1136 (1983). 2. N.E. Holden, R.L. Martin and I.L. Barnes, Pure Appl. Chem., 56, 675-694 (1984). 3. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 63, 991-1002 (1991). 4. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 55, 1101-1118 (1983). 5. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 56, 653-674 (1984). 6. IUPAC Commission on Atomic Weights and Isotopic Abundances, Pure Appl. Chem. 63, 975-990 (1991)
THE TABLE OF ISOTOPIC COMPOSITIONS OF THE ELEMENTS AS DETERMINED BY MASS SPECTROMETRY The Subcommittee for Isotopic Abundance Measurements(SiAM) has examined the literature available to it through July 1997 and has evaluated these data to produce a table of recommended isotopic abundances for the elements. The table is intended to include values for normal terrestrial samples and does not include values published for meteoritic or other extra-terrestrial materials The column contents are as follows: Column I: The elements are tabulated in ascending order of their atomic numbers Column 2: The symbols for the elements are listed using the abbreviations recommended by IUPac Column 3: The mass number for each isotope is listed Column 4: Range of natural variations Given are the highest and lowest abundances published for each isotope from measurements which have been accepted by the Subcommittee. No data are given in this Column unless a range has been reliably established. The limits given do not include certain exceptional samples, these are noted with a"g"in Column 5 Column 5: Annotations The letters appended in this Column have the following significance g geologically exceptional specimens are known in which the element has an isotopic composition outside the reported range (refers to column 4 m modified isotopic compositions may be found in commercially available material because it has been subjected to an undisclosed or inadvertent isotopic fractionation. Substantial deviations from the isotopic compositions given can occur. (refers to column 9) r range in isotopic composition existing in normal terrestrial material limits the precision of the isotopic abundances (refers to column 9) Column 6: The best measurement from a single terrestrial source The values are reproduced from the original literature. The uncertainties on the last digits are given in parenthesis as reported in the original publication. As they are not reported in any uniform manner in the literature. SIAM indicates this as follows: Is 2s. 3s indicates 1. 2 or 3 standard deviations, P indicates some other error as defined by the author, and indicates standard error(standard deviation of the mean). Where data are published as isotopic ratios, they, including their uncertainties, are converted to abundances using orthodox procedures C"is appended when calibrated mixtures have been used to correct the mass spectrometer for bias, giving an"absolute"result within the errors stated in the original publication
THE TABLE OF ISOTOPIC COMPOSITIONS OF THE ELEMENTS AS DETERMINED BY MASS SPECTROMETRY The Subcommittee for Isotopic Abundance Measurements (SIAM) has examined the literature available to it through July l997 and has evaluated these data to produce a table of recommended isotopic abundances for the elements. The table is intended to include values for normal terrestrial samples and does not include values published for meteoritic or other extra-terrestrial materials. The column contents are as follows: Column l: The elements are tabulated in ascending order of their atomic numbers. Column 2: The symbols for the elements are listed using the abbreviations recommended by IUPAC. Column 3: The mass number for each isotope is listed. Column 4: Range of natural variations. Given are the highest and lowest abundances published for each isotope from measurements which have been accepted by the Subcommittee. No data are given in this Column unless a range has been reliably established. The limits given do not include certain exceptional samples, these are noted with a "g" in Column 5. Column 5: Annotations The letters appended in this Column have the following significance: g geologically exceptional specimens are known in which the element has an isotopic composition outside the reported range. (refers to column 4) m modified isotopic compositions may be found in commercially available material because it has been subjected to an undisclosed or inadvertent isotopic fractionation. Substantial deviations from the isotopic compositions given can occur. (refers to column 9) r range in isotopic composition existing in normal terrestrial material limits the precision of the isotopic abundances. (refers to column 9) Column 6: The best measurement from a single terrestrial source. The values are reproduced from the original literature. The uncertainties on the last digits are given in parenthesis as reported in the original publication. As they are not reported in any uniform manner in the literature, SIAM indicates this as follows: ls, 2s, 3s indicates l, 2, or 3 standard deviations, P indicates some other error as defined by the author, and ¢se¢ indicates standard error (standard deviation of the mean). Where data are published as isotopic ratios, they, including their uncertainties, are converted to abundances using orthodox procedures. "C" is appended when calibrated mixtures have been used to correct the mass spectrometer for bias, giving an "absolute" result within the errors stated in the original publication
L"is appended when the linearity of the mass spectrometer has been established for the relevant abundance ratios by using synthetic mixtures of isotopes or certified materials produced by an appropriate Standards laborator N"is appended when none of the above requirements are met The user is cautioned that a)Since the data are reproduced from the literature, the sum of the isotopic abundances may not equal 100 percent b)When a range of compositions has been established, the samples used for the best measurement may come from any part of the range c)An uncalibrated"Best Measurement"is not necessarily free of systematic errors Column 7: The reference shown is that from which the data shown in column 6 were taken(Appendix A Column 8: Reference materials or samples with normal terrestrial isotopic values which are known to be available are listed. An asterisk indicates the reference material used for the best measurement. When additional reference materials are available. the distributors are listed in lieu of specific reference materials(Appendix B) Column 9: Representative Isotopic Composition In this column are listed the values which, in the opinion of SIAM, represent the isotopic composition of the chemicals and/or materials most commonly encountered in the laboratory They may not, therefore, correspond to the most abundant natural material. For example, in the case of hydrogen, the deuterium abundance quoted corresponds to that in fresh water in temperate climates rather than to ocean water. The uncertainties listed in parenthesis cover the range of probable variations of the materials as well as experimental errors. The number of significant figures is chosen to be consistent with the uncertainties, which in turn are derived by applying the statistical guidelines SIAM uses for assigning uncertainties to published isotope abundance measurements. An Atomic Weight calculated from these abundances will be consistent with A(E)values listed in the Table of Standard Atomic Weights 1997 Warning 1)Values in column 9 should be used to determine the average properties of material of unspecified natural terrestrial origin, though no actual sample having the exact composition listed may be 2)When precise work is to be undertaken, such as assessment of individual properties, samples with more precisely known isotopic abundances(such as those listed in column 8)should be obtained or suitable measurements should be made
"L" is appended when the linearity of the mass spectrometer has been established for the relevant abundance ratios by using synthetic mixtures of isotopes or certified materials produced by an appropriate Standards laboratory. "N" is appended when none of the above requirements are met. The user is cautioned that: a) Since the data are reproduced from the literature, the sum of the isotopic abundances may not equal l00 percent. b) When a range of compositions has been established, the samples used for the best measurement may come from any part of the range. c) An uncalibrated "Best Measurement" is not necessarily free of systematic errors. Column 7: The reference shown is that from which the data shown in column 6 were taken (Appendix A). Column 8: Reference materials or samples with normal terrestrial isotopic values which are known to be available are listed. An asterisk indicates the reference material used for the best measurement. When additional reference materials are available, the distributors are listed in lieu of specific reference materials (Appendix B). Column 9: Representative Isotopic Composition. In this column are listed the values which, in the opinion of SIAM, represent the isotopic composition of the chemicals and/or materials most commonly encountered in the laboratory. They may not, therefore, correspond to the most abundant natural material. For example, in the case of hydrogen, the deuterium abundance quoted corresponds to that in fresh water in temperate climates rather than to ocean water. The uncertainties listed in parenthesis cover the range of probable variations of the materials as well as experimental errors. The number of significant figures is chosen to be consistent with the uncertainties, which in turn are derived by applying the statistical guidelines SIAM uses for assigning uncertainties to published isotope abundance measurements. An Atomic Weight calculated from these abundances will be consistent with Ar(E) values listed in the Table of Standard Atomic Weights 1997. Warning 1) Values in column 9 should be used to determine the average properties of material of unspecified natural terrestrial origin, though no actual sample having the exact composition listed may be available. 2) When precise work is to be undertaken, such as assessment of individual properties, samples with more precisely known isotopic abundances (such as those listed in column 8) should be obtained or suitable measurements should be made
TABLE 1. Isotopic compositions of the elements as determined by mass spectrometr Best Range of Measurement Representaive Natural from a Single rence Atomic Mass Variations Annot- Terrestrial Source Reference Materials Composition Number Symbol Number (Atom % ations (Atom % (App. A)(App. B) 1H1999816-999975mr99984426(5)2sC7 OHAGI VSMOW* 999885(70) 200184 0015574(5) 00115(0)b IAEA (in water) NIST 34.6x100.0041gr 0.0001343(13)1sC88 SANI Air 0000137(3) 100-999959 999998657(13) 99999863(3) 3 6721-7.71m,r7.589(24)2sC97 QIl IRMM016*[759(4)C 92.7992.29 92411(24) IAEA [92.41(4) RMM NIST 4 Be 9 63LEI1 1018927-20.337 1982(2)2sC 69BIE1 IRMM-011* 199(7) l181.073-79.663 80.18(2) NIST 80.1(7 29885-9902r 988922(28)PC90CHA1NBS19* 9893(8) 13 1.15-0.98 1.1078(28) IAEA 1.07(8) NIST N1499890-99652r996337(4)PC58JUN1Air 996532(7)d 50411-0.348 0.3663(4) 0.368(7) 16997384997756r 99.7628(5)IsN 76BAEI VSMOW* 99757(16) 170.0399-0.0367 0.0372(4)e 88L11 IAEA 0038(1) 180.22170.1877 0.20004(5) NIST 0.205(14) 20ASTI 100 8847gm90.4838(90)lsC84BOT1Air* 90.48(3) 0.266r 0.2696(5) 0.27(1) 925(3) 56WH 78.992(25)2sC66CAT1NsT-SRM980*7899(4) 10003(9) 1000(1) 11.005(19) 13Al2 56WHI1
TABLE 1. Isotopic compositions of the elements as determined by mass spectrometry Best Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot-Terrestrial Source Reference Materialsa Composition Number Symbol Number (Atom %) ations (Atom %) (App. A) (App. B) (Atom %) 12 3 4 5 6 7 8 9 1 H 1 99.9816 - 99.9975 m,r 99.984426 (5) 2s C 70HAG1 VSMOW* 99.9885 (70) 2 0.0184 - 0.0025 0.015574 (5) CEA 0.0115 (70) b IAEA (in water) NIST 2 He 3 4.6x10-8-0.0041 g,r 0.0001343(13) 1s C 88SAN1 Air* 0.000137 (3) 4 100 - 99.9959 99.9998657 (13) 99.999863 (3) (in air) 3 Li 6 7.21 - 7.71 m,r 7.589 (24) 2s C 97QI1 IRMM-016* [7.59(4)]c 7 92.79 - 92.29 92.411 (24) IAEA [92.41(4)] IRMM NIST 4 Be 9 100 63LEI1 100 5 B 10 18.927 - 20.337 m,r 19.82 (2) 2s C 69BIE1 IRMM-011* 19.9 (7) 11 81.073- 79.663 80.18 (2) NIST 80.1 (7) 6 C 12 98.85 - 99.02 r 98.8922 (28) P C 90CHA1 NBS19* 98.93 (8) 13 1.15 - 0.98 1.1078 (28) IAEA 1.07 (8) NIST 7 N 14 99.890 -99.652 r 99.6337 (4) P C 58JUN1 Air* 99.632 (7) d 15 0.411 - 0.348 0.3663 (4) IAEA 0.368 (7) NIST 8 O 16 99.7384 -99.7756 r 99.7628 (5) 1s N 76BAEl VSMOW* 99.757 (16) 17 0.0399 - 0.0367 0.0372 (4) e 88LI1 IAEA 0.038 (1) 18 0.2217 - 0.1877 0.20004 (5) NIST 0.205 (14) 9 F 19 100 20AST1 100 10 Ne 20 90.514 - 88.47 g,m 90.4838 (90) 1s C 84BOT1 Air* 90.48 (3) 21 1.71 - 0.266 r 0.2696 (5) 0.27 (1) 22 9.96 - 9.20 9.2465 (90) 9.25 (3) (in air) 11 Na 23 100 56WHI1 100 12 Mg 24 78.992 (25) 2s C 66CAT1 NIST-SRM980* 78.99 (4) 25 10.003 (9) 10.00 (1) 26 11.005 (19) 11.01 (3) 13 Al 27 100 56WHI1 100
Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot- Terrestrial Source Reference Materials Number Symbol Number (Atom % ations (Atom (App. A)(App. B) (Atom % 289221-9225r 9222968(44)2sC97GON1IAEA 922297(7) 4.69-4.67 4.68316(32) IRMM 4.6832(5) 303.10-3.08 3.08716(48 NIST 3.0872(5) 15 63LEI1 163294.537-95.261r95018(4)PC50 MACI CEA 9493(31) 330.7870.731 0.750(7 IAEA 0.76(2) 44655-3.993 4215(4) NIST 4.29(28) 6 0.021-0.015 0.017(2) 002(1) C13575.64-75.86 75771(45)2sC62 SHIl NIST-SRM97575.78(4 37 24.36-24.14 24.229(45) 24.22(4) Ar 36 g 0.3365(6)PC50NHE1Air 03365(30) 00632(1) 0.0632(5) 996003(6) 996003(30) In air K 9325811(292)2sC75 GARI NIST-SRM985*93.2581(44) 0011672(41 00117(1) 6.73022(292) 6.7302(44) 0Ca4096.982-96880gr96.941(6)2sN72MOO1 NIST-SRM915*96941(156 420.656-0.640 0647(3) 0647(23) 0.135(2) 0.135(10) 442.130-2.057 2086(4) 2.086(110) 460.0046-0.0031 0.004(1) 0.004(3) 480.2000.179 0.187(1) 0.187(21) SoLELI 100 8249(21)2sC93SHl 825(3) 744(2) 5409(10) 5.4l(2) 5.185(13) 5.18(2) 23V500.2502-0.2487g0.2497(6)lsF66FLEl 0.250(4) 43452(85)2sC66SH1 NIST-SRM979*4.345(13) 837895(117) 83789(18) 9501(1 23647(48) 2.365(7)
Best Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot-Terrestrial Source Reference Materialsa Composition Number Symbol Number (Atom %) ations (Atom %) (App. A) (App. B) (Atom %) 12 3 4 5 6 7 8 9 14 Si 28 92.21 - 92.25 r 92.22968 (44) 2s C 97GON1 IAEA 92.2297 (7) 29 4.69 - 4.67 4.68316 (32) IRMM 4.6832 (5) 30 3.10 - 3.08 3.08716 (48) NIST 3.0872 (5) 15 P 31 100 63LEI1 100 16 S 32 94.537 - 95.261 r 95.018 (4) P C 50MAC1 CEA 94.93 (31) 33 0.787 - 0.731 0.750 (7) IAEA 0.76 (2) 34 4.655 - 3.993 4.215 (4) NIST 4.29 (28) 36 0.021 -0.015 0.017 (2) 0.02 (1) 17 Cl 35 75.64 - 75.86 m 75.771 (45) 2s C 62SHI1 NIST-SRM975* 75.78 (4) 37 24.36 - 24.14 24.229 (45) 24.22 (4) 18 Ar 36 g 0.3365 (6) P C 50NIE1 Air* 0.3365 (30) 38 0.0632 (1) 0.0632 (5) 40 99.6003 (6) 99.6003 (30) (in air) 19 K 39 93.25811 (292) 2s C 75GAR1 NIST-SRM985* 93.2581 (44) 40 0.011672 (41) 0.0117 (1) 41 6.73022 (292) 6.7302 (44) 20 Ca 40 96.982 - 96.880 g,r 96.941 (6) 2s N 72MOO1 NIST-SRM915* 96.941 (156) h 42 0.656 - 0.640 0.647 (3) 0.647 (23) 43 0.146 - 0.131 0.135 (2) 0.135 (10) 44 2.130 - 2.057 2.086 (4) 2.086 (110) 46 0.0046 - 0.0031 0.004 (1) 0.004 (3) 48 0.200 - 0.179 0.187 (1) 0.187 (21) 2l Sc 45 100 50LEL1 100 22 Ti 46 8.249 (21) 2s C 93SHI1 8.25 (3) 47 7.437 (14) 7.44 (2) 48 73.720 (22) 73.72 (3) 49 5.409 (10) 5.41 (2) 50 5.185 (13) 5.18 (2) 23 V 50 0.2502 - 0.2487 g 0.2497 (6) 1s F 66FLE1 0.250 (4) 51 99.7513 - 99.7498 99.7503 (6) 99.750 (4) 24 Cr 50 4.3452 (85) 2s C 66SHI1 NIST-SRM979* 4.345 (13) 52 83.7895 (117) 83.789 (18) 53 9.5006 (110) 9.501 (17) 54 2.3647 (48) 2.365 (7)
Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot- Terrestrial Source Reference Materials Number Symbol Number (Atom % ations (Atom (App. A)(App. B) (Atom % Mn 55 00 63LEIl 5845(23)2sC92TAY1IRMM014*5.845(35 91.754(24) 91.754(36) 0.2819(27) 0.282 63LEI1 (59)2sC89 62231(51) 26.2231(77) 1399(4) 3.6345(11 36345(17) 64 0.9256(6 0.9256(9) 29Cu636924-6898r69.174(20)2sC64SH1 NIST-SRM976*69.17(3) 6531.02-30.76 30.826(20) 30.83(3 4863(20)2sF72ROSl 27.90(9) 27.90(27 4.10(4) 4.10(13) 68 18.75(17) 18.75(51) 60.1079(62)2sC86 MACI NIST-SRM994*60.108(9) 398921(62) 39892(9) 21.234(31)lsL86GRE1 20.84(87 27.54(34 7.717(5 7.444(14) 7.61(38) 63LEIl 0889(3)1sN89wAC 089(4) 76 937(29) 3772(20) 49.607(17) 4961(41) 8.731(10) 50.686(26)2sC64CAT1 NIST-SRM977*50.69(7 49.314(26) 6Kr78 gm0.35351(7)2sN94VAL1 0.35(1) 2.28(6) 58304(76) 1149533(35) 11.49(6) 5698890(62) 7.00(4) 17.29835(26) 17.30(22)
Best Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot-Terrestrial Source Reference Materialsa Composition Number Symbol Number (Atom %) ations (Atom %) (App. A) (App. B) (Atom %) 12 3 4 5 6 7 8 9 25 Mn 55 100 63LEI1 100 26 Fe 54 5.845(23) 2s C 92TAY1 IRMM-014* 5.845 (35) 56 91.754(24) 91.754 (36) 57 2.1191(65) 2.119 (10) 58 0.2819(27) 0.282 (4) 27 Co 59 100 63LEI1 100 28 Ni 58 68.0769 (59) 2s C 89GRA1 68.0769 (89) 60 26.2231 (51) 26.2231 (77) 61 1.1399 (4) 1.1399 (6) 62 3.6345 (11) 3.6345 (17) 64 0.9256 (6) 0.9256 (9) 29 Cu 63 69.24 - 68.98 r 69.174 (20) 2s C 64SHI1 NIST-SRM976* 69.17 (3) 65 31.02 - 30.76 30.826 (20) 30.83 (3) 30 Zn 64 48.63 (20) 2s F 72ROS1 48.63 (60) 66 27.90 (9) 27.90 (27) 67 4.10 (4) 4.10 (13) 68 18.75 (17) 18.75 (51) 70 0.62 (1) 0.62 (3) 31 Ga 69 m 60.1079 (62) 2s C 86MAC1 NIST-SRM994* 60.108 (9) 71 39.8921 (62) 39.892 (9) 32 Ge 70 21.234 (31) 1s L 86GRE1 20.84 (87)k 72 27.662 (29) 27.54 (34) 73 7.717 (5) 7.73 (5) 74 35.943 (25) 36.28 (73) 76 7.444 (14) 7.61 (38) 33 As 75 100 63LEI1 100 34 Se 74 r 0.889 (3) 1s N 89WAC1 0.89 (4) 76 9.366 (18) 9.37 (29) 77 7.635 (10) 7.63 (16) 78 23.772 (20) 23.77 (28) 80 49.607 (17) 49.61 (41) 82 8.731 (10) 8.73 (22) 35 Br 79 50.686 (26) 2s C 64CAT1 NIST-SRM977* 50.69 (7) 81 49.314 (26) 49.31 (7) 36 Kr 78 g,m 0.35351 (7) 2s N 94VAL1 0.35 (1) 80 2.28086(29) 2.28 (6) 82 11.58304 (76) 11.58 (14) 83 11.49533 (35) 11.49 (6) 84 56.98890 (62) 57.00 (4) 86 17.29835(26) 17.30 (22) (in air)
Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot- Terrestrial Source Reference Materials Number Symbol Number (Atom % ations (Atom (App. A)(App. B) (Atom % 37 Rb 72.1654(132)2sC69CAT1 NIST-SRM98472.17(2) 27.8346(132) 27.83(2) 38Sr840.58-0.55gr 0.5574(16)2sC82MOO1NIST-SRM987*0.56(1) 999-975 9.8566(34) NIST 86(1) 7.14-6.94 7.0015(26) 700(1)h 82.75-82.29 82.5845(66) 82.58(1) 100 57COL1 51452(9)2sN83NOMl 5145(40) 11.223(12) 11.22(5) 17.146 1715(8) 17380(12) 1738(28) 2.799(5) 80(9) 56WHII 100 Mo g14.8362(148)2sN74MOOl 14.84(35) 9.2466(92) 925(12) 15.9201(159) 15.92(13) 166756(167) 1668(2) 9.5551(96) 24.1329(241) 24.13(31) 96335(96) 9.63(23 Ru 55420(1)1sN97HUAl 5.54(14) 8688(2) 87(3) 12.7579(6) 12.76(14) 12.5985(4) 101 17.0600(10) 17.06(2) 31.5519(l1) 31.55(14) 86210(11) 1862(27 Rh103 1.020(8)2sC78SHI1 1.02(1) 14(5) l1.14(8) 105 233(5) 2.33(8) 26.46(6) 26.46(9) g51.8392(51)2sC82 POW1 NIST-SRM978*51839(8) 48.1608(51) 48.161(8)
Best Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot-Terrestrial Source Reference Materialsa Composition Number Symbol Number (Atom %) ations (Atom %) (App. A) (App. B) (Atom %) 12 3 4 5 6 7 8 9 37 Rb 85 g 72.1654 (132) 2s C 69CAT1 NIST-SRM984 72.17 (2) 87 27.8346 (132) 27.83 (2) 38 Sr 84 0.58 - 0.55 g,r 0.5574 (16) 2s C 82MOO1 NIST-SRM 987* 0.56 (1) 86 9.99 - 9.75 9.8566 (34) NIST 9.86 (1) 87 7.14 - 6.94 7.0015 (26) 7.00 (1) h 88 82.75 - 82.29 82.5845 (66) 82.58 (1) 39 Y 89 100 57COL1 100 40 Zr 90 g 51.452 (9) 2s N 83NOM1 51.45 (40) 91 11.223 (12) 11.22 (5) 92 17.146 (7) 17.15 (8) 94 17.380 (12) 17.38 (28) 96 2.799 (5) 2.80 (9) 41 Nb 93 100 56WHI1 100 42 Mo 92 g 14.8362 (148) 2s N 74MOO1 14.84 (35) 94 9.2466 (92) 9.25 (12) 95 15.9201 (159) 15.92 (13) 96 16.6756 (167) 16.68 (2) 97 9.5551 (96) 9.55 (8) 98 24.1329 (241) 24.13 (31) 100 9.6335 (96) 9.63 (23) 43 Tc -- --- ------ 44 Ru 96 g 5.5420 (1) 1s N 97HUA1 5.54 (14) 98 1.8688 (2) 1.87 (3) 99 12.7579 (6) 12.76 (14) 100 12.5985 (4) 12.60 (7) 101 17.0600 (10) 17.06 (2) 102 31.5519 (11) 31.55 (14) 104 18.6210 (11) 18.62 (27) 45 Rh 103 100 63LEI1 100 46 Pd 102 g,r 1.020 (8) 2s C 78SHI1 1.02 (1) 104 11.14 (5) 11.14 (8) 105 22.33 (5) 22.33 (8) 106 27.33 (2) 27.33 (3) 108 26.46 (6) 26.46 (9) 110 11.72 (6) 11.72 (9) 47 Ag 107 g 51.8392 (51) 2s C 82POW1 NIST-SRM978* 51.839 (8) 109 48.1608 (51) 48.161 (8)
Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot- Terrestrial Source Reference Materials Number Symbol Number (Atom % ations (Atom (App. A)(App. B) (Atom % 48Cd106 1.25(2)2sF 80ROS I .25(6) 0.89(1) 0.89(3) 124 111 1280(4) 1280(12) 24.13(7) 24.13(21) 113 12.22(4) 1222(12) 28.73(14) 28.73(42) 749(18) 113 4.288(5)2sN91CHAl 4.29(5) 115 95712(5) 9571(5) l12 0973(3)1sC83DEV1 0.97(1) 114 0.659(3) 84ROS I 066(1) 115 0.339(3) 0.34(1) 116 14.536(31) 14.54 7.676(22) 7.68(7) 24.223(30) 422(9 8585(13) 859(4) 32.58(9) 122 4629(9) 4.63(3) 124 5789(17) 5.79(5) 51Sb121 57213(32)2sC93CHAl 57.21(5) 42.787(32) 42.79(5) Te120 0.096(1)2seN78sMl 009(1 2603(1) 2.55(12) 0908(1) 4.816(2) 4.74(14) 7.139(2) 07(15) 126 18.952(4) 1884(2 33799(3) .08(62) 53 127 49LELI 126 0.08880(2) 009(1) 128 1.91732(12) 192(3) 129 26.43964(17) 2644(24) 4.08(2) 1.17961(19) 132 26.89157(11) 26.89(6) 10.44232(17) 886890(14) 887(16)
Best Range of Measurement Available Representaive Natural from a Single Reference Isotopic Atomic Mass Variations Annot-Terrestrial Source Reference Materialsa Composition Number Symbol Number (Atom %) ations (Atom %) (App. A) (App. B) (Atom %) 12 3 4 5 6 7 8 9 48 Cd 106 g 1.25 (2) 2s F 80ROS1 1.25 (6) 108 0.89 (1) 0.89 (3) 110 12.49 (6) 12.49 (18) 111 12.80 (4) 12.80 (12) 112 24.13 (7) 24.13 (21) 113 12.22 (4) 12.22 (12) 114 28.73 (14) 28.73 (42) 116 7.49 (6) 7.49 (18) 49 In 113 g 4.288 (5) 2s N 91CHA1 4.29 (5) 115 95.712 (5) 95.71 (5) 50 Sn 112 g 0.973 (3) 1s C 83DEV1 0.97 (1) 114 0.659 (3) f 84ROS1 0.66 (1) 115 0.339 (3) f 0.34 (1) 116 14.536 (31) 14.54 (9) 117 7.676 (22) 7.68 (7) 118 24.223 (30) 24.22 (9) 119 8.585 (13) 8.59 (4) 120 32.593 (20) 32.58 (9) 122 4.629 (9) 4.63 (3) l24 5.789 (17) 5.79 (5) 51 Sb 121 g 57.213 (32) 2s C 93CHA1 57.21 (5) 123 42.787 (32) 42.79 (5) 52 Te 120 g 0.096 (1) 2se N 78SMI1 0.09 (1)k 122 2.603 (1) 2.55 (12) 123 0.908 (1) 0.89 (3) 124 4.816 (2) 4.74 (14) 125 7.139 (2) 7.07 (15) 126 18.952 (4) 18.84 (25) 128 31.687 (4) 31.74 (8) 130 33.799 (3) 34.08 (62) 53 I 127 100 49LEL1 100 54 Xe 124 g,m 0.08913(3) 2s N 94VAL1 0.09 (1) 126 0.08880 (2) 0.09 (1) 128 1.91732 (12) 1.92 (3) 129 26.43964 (17) 26.44 (24) 130 4.08271 (15) 4.08 (2) 131 21.17961 (19) 21.18 (3) 132 26.89157 (11) 26.89 (6) 134 10.44232 (17) 10.44 (10) 136 8.86890 (14) 8.87 (16) 55 Cs 133 100 56WHI1 100