The electron mass was used to calculate the
Avogadro constant before its value was fixed as a defining constant in the
2019 revision of the SI: : N_{\rm A} = \frac{M_{\rm u} A_{\rm r}({\rm e})}{m_{\rm e}} = \frac{M_{\rm u} A_{\rm r}({\rm e})c\alpha^2}{2R_\infty h} . Hence it is also related to the
atomic mass constant : : m_{\rm u} = \frac{M_{\rm u}}{N_{\rm A}} = \frac{m_{\rm e}}{A_{\rm r}({\rm e})} = \frac{2R_\infty h}{A_{\rm r}({\rm e})c\alpha^2} , where • is the
molar mass constant (defined in
SI); • is a directly measured quantity, the
relative atomic mass of the electron. is defined in terms of , and not the other way round, and so the name "electron mass in atomic mass units" for involves a circular definition (at least in terms of practical measurements). The electron relative atomic mass also enters into the calculation of all other relative atomic masses. By convention, relative atomic masses are quoted for neutral atoms, but the actual measurements are made on positive
ions, either in a
mass spectrometer or a
Penning trap. Hence the mass of the electrons must be added back on to the measured values before tabulation. A correction must also be made for the mass equivalent of the
binding energy . Taking the simplest case of complete ionization of all electrons, for a nuclide X of
atomic number , It involves the measurement of the frequencies of the
cyclotron radiation emitted by electrons and by {{chem2|^{12}C(6+)}} ions in a Penning trap. The ratio of the two frequencies is equal to six times the inverse ratio of the masses of the two particles (the heavier the particle, the lower the frequency of the cyclotron radiation; the higher the charge on the particle, the higher the frequency): : \frac{\nu_c ({}^{12}{\rm C}^{6+})}{\nu_c ({\rm e})} = \frac{6A_{\rm r}({\rm e})}{A_{\rm r}({}^{12}{\rm C}^{6+})} = 0.000\,274\,365\,185\,89(58) As the relative atomic mass of {{chem2|^{12}C(6+)}} ions is very nearly 12, the ratio of frequencies can be used to calculate a first approximation to
Ar(e), . This approximate value is then used to calculate a first approximation to
Ar(12C6+), knowing that \tfrac{E_\text{b}(^{12}\mathrm{C})}{m_{\rm u}c^2} (from the sum of the six ionization energies of carbon) is : . This value is then used to calculate a new approximation to
Ar(e), and the process repeated until the values no longer vary (given the relative uncertainty of the measurement, 2.1): this happens by the fourth cycle of iterations for these results, giving for these data. == References ==