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The CODATA 2017 values of h, e, k, and NA for the revision of the SI

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Published 29 January 2018 © 2018 BIPM & IOP Publishing Ltd
, , Citation D B Newell et al 2018 Metrologia 55 L13 DOI 10.1088/1681-7575/aa950a

0026-1394/55/1/L13

Abstract

Sufficient progress towards redefining the International System of Units (SI) in terms of exact values of fundamental constants has been achieved. Exact values of the Planck constant h, elementary charge e, Boltzmann constant k, and Avogadro constant NA from the CODATA 2017 Special Adjustment of the Fundamental Constants are presented here. These values are recommended to the 26th General Conference on Weights and Measures to form the foundation of the revised SI.

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1. Introduction

The international system of units (SI) has been slowly evolving from an artifact based system to one based on values of fundamental constants and invariant properties of atoms. The quantitative limitations of the last remaining base unit of the SI defined by an artifact, the kilogram, have been known since at least the third verification of national kilogram prototypes (Quinn 1991, Girard 1994). As a consequence the possible role of the fundamental constants in replacing the kilogram has been discussed in earnest for nearly three decades. International consensus on the foundation of a new system of units based on exactly defined values of the Planck constant h, elementary charge e, Boltzmann constant k, and Avogadro constant $N_{\rm A}$ was reached during the 24th meeting of the General Conference on Weights and Measures (CGPM 2011). Progress in the accuracy and consistency of the research results has enabled the 106th International Committee for Weights and Measures (CIPM) to recommend proceeding with the adoption of the revised SI (CIPM 2017).

The Committee on Data for Science and Technology (CODATA), through its Task Group on Fundamental Constants (TGFC), periodically provides the scientific and technological communities with a self-consistent set of internationally recommended values of the basic constants and conversion factors of physics and chemistry. Because of this role, the CGPM invited the CODATA TGFC to carry out a special least-squares adjustment (LSA) of the values of the fundamental physical constants to provide values for defining constants to form the foundation for the revised SI (CGPM 2011). The results of that adjustment are given here, namely, the numerical values of h, e, k, and NA, each with a sufficient number of digits to maintain consistency between the present and revised SI as proposed by the Consultative Committee for Units (CCU) and agreed to by the CIPM (CIPM 2016). These numbers are recommended to the 26th CGPM to establish the revised SI when it convenes in November 2018.

2. The CODATA 2017 special adjustment

The input data for the CODATA 2017 Special Adjustment includes the input data used in the final CODATA 2014 regular adjustment on which the 2014 recommended values are based. Of these data, which are given in tables XV-XIX of Mohr et al (2016a), the following were omitted: the four cyclotron frequency ratios, items B8, B9, B11, and B12 that have been superseded by the 2016 atomic mass evaluation (Huang et al 2017, Wang et al 2017), and all measurements of the Newtonian constant of gravitation G. Key data that were published or accepted for publication before the 1 July 2017 closing date of the CODATA 2017 Special Adjustment and have a significant impact on the determination of h, e, k, and NA are listed in table 1. The full list of data considered for the CODATA 2017 Special Adjustment is given in tables 2–5 in Mohr et al (2018). Of note are data that are not included for the same reasons they were omitted from the 2014 adjustment. In particular, the measurements in muonic hydrogen and deuterium that have led to the proton radius 'puzzle' were not included. These data would have no effect on the 2017 values of h, e, k, and NA, but will be reconsidered for the next CODATA periodic adjustment.

Table 1. Key data for the determination of h, e, k, and NA in the CODATA 2017 Special Adjustment. See Mohr et al (2017) for a complete list of input data.

   Source Identificationa Quantityb       Value Rel. stand. uncert ur
Schlamminger et al (2015) NIST-15 h $ 6.626\, 069\, 36(38)\times 10^{-34}$ J s $ 5.7\times 10^{-8}$
Wood et al (2017) NRC-17 h $ 6.626\, 070\, 133(60)\times 10^{-34}$ J s $ 9.1\times 10^{-9}$
Haddad et al (2017) NIST-17 h $ 6.626\, 069\, 934(88)\times 10^{-34}$ J s $ 1.3\times 10^{-8}$
Thomas et al (2017) LNE-17 h $ 6.626\, 070\, 40(38)\times 10^{-34}$ J s $ 5.7\times 10^{-8}$
Azuma et al (2015) IAC-11 NA $ 6.022\, 140\, 95(18)\times 10^{23}$ mol−1 $ 3.0\times 10^{-8}$
Azuma et al (2015) IAC-15 NA $ 6.022\, 140\, 70(12)\times 10^{23}$ mol−1 $ 2.0\times 10^{-8}$
Bartl et al (2017) IAC-17 NA $ 6.022\, 140\, 526(70)\times 10^{23}$ mol−1 $ 1.2\times 10^{-8}$
Kuramoto et al (2017) NMIJ-17 NA $ 6.022\, 140\, 78(15)\times 10^{23}$ mol−1 $ 2.4\times 10^{-8}$
Moldover et al (1988) NIST-88 R $ 8.314\, 470(15)$ J mol−1 K−1 $ 1.8\times 10^{-6}$
Pitre et al (2009) LNE-09 R $ 8.314\, 467(23)$ J mol−1 K−1 $ 2.7\times 10^{-6}$
Sutton et al (2010) NPL-10 R $ 8.314\, 468(26)$ J mol−1 K−1 $ 3.2\times 10^{-6}$
Pitre et al (2011) LNE-11 R $ 8.314\, 455(12)$ J mol−1 K−1 $ 1.4\times 10^{-6}$
Pitre et al (2015) LNE-15 R $ 8.314\, 4615(84)$ J mol−1 K−1 $ 1.0\times 10^{-6}$
Gavioso et al (2015) INRIM-15 R $ 8.314\, 4743(88)$ J mol−1 K−1 $ 1.1\times 10^{-6}$
Pitre et al (2017) LNE-17 R $ 8.314\, 4614(50)$ J mol−1 K−1 $ 6.0\times 10^{-7}$
Podesta et al (2017) NPL-17 R $ 8.314\, 4603(58)$ J mol−1 K−1 $ 7.0\times 10^{-7}$
Feng et al (2017) NIM-17 R $ 8.314\, 459(17)$ J mol−1 K−1 $ 2.0\times 10^{-6}$
Gaiser et al (2017) PTB-17 $ \newcommand{\e}{{\rm e}} {A_{\epsilon}({\hspace{0pt}}^4{\rm He})/R}$ $ 6.221\, 140(12)\times 10^{-8}$ m3 K J−1 $ 1.9\times 10^{-6}$
Qu et al (2017) NIM/NIST-17 k/h $ 2.083\, 6630(56)\times 10^{10}$ Hz K−1 $ 2.7\times 10^{-6}$

aIAC: International Avogadro Coordination; INRIM: Istituto Nazionale di Ricerca Metrologica, Torino, Italy; LNE: Laboratoire national de métrologie et d'essais, Trappes and La Plaine-Saint-Denis, France; NIM: National Institute of Metrology, Beijing, PRC; NIST: National Institute of Standards and Technology, Gaithersburg, MD, and Boulder, CO, USA; NMIJ: National Metrology Institute of Japan, Tsukuba, Japan; NPL: National Physical Laboratory, Teddington, UK; NRC: National Research Council Canada, Ottawa, Canada; PTB: Physikalisch-Technische Bundesanstalt, Braunschweig and Berlin, Germany. bh: Planck constant; NA: Avogadro constant;R: molar gas constant;$ \newcommand{\e}{{\rm e}} {A_{\epsilon}({\hspace{0pt}}^4{\rm He})/R}$ : molar polarizability of ${\hspace{0pt}}^4{\rm He}$ gas to the molar gas constant quotient;k/h: Boltzmann constant to Planck constant quotient.

The CODATA 2017 Special Adjustment follows the same procedures as the previous periodic CODATA adjustments of the fundamental constants (Mohr and Taylor 2000, 2005, Mohr et al 2008a, 2008b, Mohr et al 2012a, 2012b, Mohr et al 2016a, 2016b). Details of the Special Adjustment analysis are given in Mohr et al (2018). In general, the measure the CODATA TGFC uses for consistency of an input datum is the normalized (or reduced) residual of that datum given by the LSA, that is, the difference between an input datum and its adjusted value divided by the input datum uncertainty. If a residual for an input datum is larger than two, the TGFC identifies the fundamental constant primarily influenced by that datum as well as other input data that influence the same constant. The uncertainties of this subset of input data are multiplied by a factor that is large enough that the relevant residuals are two or less. To achieve consistency, multiplicative expansion factors were applied to the uncertainties of two subsets of input data corresponding to two adjusted constants for the 2017 Special Adjustment.

The first subset consists of the eight input data for the Planck and Avogadro constants listed in table 1, relevant to the adjusted value of the Planck constant. The uncertainties of these input data are multiplied by a factor of 1.7. With this expansion of the uncertainties of the eight data, five have relative standard uncertainties ur at or below $50\times10^{-9}$ , with two at or below $20\times10^{-9}$ , where the latter includes results from both the Kibble balance and the x-ray crystal density (XRCD) methods.

The second subset of expanded data consists of the input data that determine the relative atomic mass of the proton: the 2016 atomic mass evaluation value of ${\hspace{0pt}}^1{\rm H}$ and the cyclotron frequency ratio of hydrogenic carbon to the proton, items B2 and B12, respectively, of table 4 in Mohr et al (2018). Coincidentally, an expansion factor of 1.7 was also appropriate in this case, although its application has no effect on the 2017 values of h, e, k, and NA.

3. Results

Figure 1 shows values of h inferred from the key input data in table 1 and the final CODATA 2017 value. The values of k inferred from the key input data in table 1 and the final CODATA 2017 value are shown in figure 2. The final values and uncertainties of h, e, k, and NA from the 2017 CODATA Special Adjustment are given in table 2.

Figure 1.

Figure 1. Values of the Planck constant h inferred from the input data in table 1 and the CODATA 2017 value in chronological order from top to bottom. The inner green band is  ±20 parts in 109 and the outer grey band is  ±50 parts in 109. KB: Kibble balance; XRCD: x-ray-crystal-density.

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Figure 2.

Figure 2. Values of the Boltzmann constant k inferred from the key input data in table 1 and the CODATA 2017 value in chronological order from top to bottom. The inner green band is  ±5 parts in 107 and the outer grey band is  ±15 parts in 107. AGT: acoustic gas thermometry; DCGT: dielectric constant gas thermometry; JNT: Johnson noise thermometry.

Standard image High-resolution image

Table 2. The CODATA 2017 adjusted values of h, e, k, and NA.

Quantity        Value Rel. stand. uncert ur
h $ 6.626\, 070\, 150(69)\times 10^{-34}$ J s $ 1.0\times 10^{-8}$
e $ 1.602\, 176\, 6341(83)\times 10^{-19}$ C $ 5.2\times 10^{-9}$
k $ 1.380\, 649\, 03(51)\times 10^{-23}$ J K−1 $ 3.7\times 10^{-7}$
NA $ 6.022\, 140\, 758(62)\times 10^{23}$ mol−1 $ 1.0\times 10^{-8}$

A requirement by the CGPM (2011) is that the revised SI be consistent with the present SI. In the SI prior to redefinition, the following quantities have exactly defined values: the international prototype of the kilogram $m(\mathcal{K}) =1~{\rm kg}$ , the vacuum magnetic permeability $\mu_{0} = 4{\pi}\times10^{-7}~{\rm H~m^{-1}}$ , the triple point of water $T_{\rm TPW} = 273.16~{\rm K}$ , and the molar mass of carbon-12, $M({\hspace{0pt}}^{12}{\rm C}) = 0.012~{\rm kg~mol^{-1}}$ . In the revised SI, these quantities are determined experimentally with associated uncertainties. As stated in the agreed upon CCU recommendation (CIPM 2016), the number of digits for the exact numerical values of h, e, and NA to define the revised SI are determined by requiring that the numerical values of $m(\mathcal{K})$ , $\mu_{0}$ , and $M({\hspace{0pt}}^{12}{\rm C})$ remain consistent with their previous exact values within their relative standard uncertainties given by the CODATA 2017 Special Adjustment. The number of digits for k is chosen such that $T_{\rm TPW}$ is equal to 273.16 K within a relative standard uncertainty at the level which TTPW can be realized (CCT 2017). The recommended exact numerical values of h, e, k, and NA to establish the revised SI are given in table 3.

Table 3. The CODATA 2017 values of h, e, k, and NA for the revision of the SI.

Quantity      Value
h $6.626\, 070\, 15\times10^{-34}~{\rm J~s}$
e $1.602\, 176\, 634\times10^{-19}~{\rm C}$
k $1.380\, 649\times10^{-23}~{\rm J~K^{-1}}$
NA $6.022\, 140\, 76\times10^{23}~{\rm mol^{-1}}$

4. Summary

Sufficient progress has been achieved towards meeting the recommendations for redefining the SI in terms of exact values of fundamental constants. The recommended exact numerical values of h, e, k, and NA to establish the revised SI based on fundamental constants are given. A detailed description of the unique 2017 CODATA special adjustment is given by Mohr et al (2017). The next regular CODATA periodic adjustment of the fundamental constants, CODATA 2018, will also be unique as it will be the first one based on the exact fundamental constants of the revised SI.

Acknowledgment

The CODATA Task Group on Fundamental Constants thanks the CGPM for inviting it to play a significant role in the international effort to establish a revised SI for the 21st century, arguably the most important change to the International System of Units since its formal adoption in 1960.

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