Constants library
12 values, each with its units, its uncertainty, and where it came from.
Electromagnetic 12
Vacuum magnetic permeability measured
N/A² (H/m)How strongly a current magnetises empty space — the constant in Ampère's law, no longer exactly 4π×10⁻⁷ since the 2019 SI redefinition.
Bohr magneton measured
J/TThe natural quantum of magnetic moment for an electron, eħ/2mₑ — the yardstick for atomic magnetism and electron spin.
Nuclear magneton measured
J/TThe magnetic-moment unit for nuclei, eħ/2mₚ — smaller than the Bohr magneton by the full proton-to-electron mass ratio of 1836.
Electron magnetic moment measured
J/TThe magnetic moment of a free electron, negative because its charge is, and about 0.116% larger than one Bohr magneton.
Proton magnetic moment measured
J/TThe magnetic moment of the proton, 2.79 nuclear magnetons rather than the 1 a point particle would show — evidence of quark structure.
Neutron magnetic moment measured
J/TA neutral particle with a magnetic moment of −1.913 nuclear magnetons — proof on its own that the neutron has charged internal structure.
Proton gyromagnetic ratio measured
s⁻¹·T⁻¹The proton's precession rate per unit magnetic field in angular frequency — the constant that turns a magnet strength into an NMR frequency.
Proton gyromagnetic ratio over 2π measured
Hz/TThe proton Larmor frequency per tesla, 42.577 MHz/T — the number every NMR spectroscopist and MRI physicist works in directly.
Electron gyromagnetic ratio measured
s⁻¹·T⁻¹The electron's spin precession rate per tesla, 658 times the proton's — the basis of electron spin resonance and of spin-qubit control.
Relative permeability of iron measured
—Typical maximum relative permeability of commercial soft iron — a wildly variable figure spanning roughly 200 to 5000 with purity and field level.
Relative permeability of mu-metal measured
—Typical relative permeability of annealed mu-metal in weak fields — the nickel-iron alloy used to shield instruments from stray magnetic fields.
Earth's magnetic field strength measured
TTypical magnitude of the geomagnetic field at the surface, near 50 μT but ranging from about 25 μT at the equator to 65 μT near the poles.