Mass of the Earth

M⊕=5.9722×1024 kgM_\oplus = 5.9722 \times 10^{24}\ \text{kg}
Value5.9722e24 kg
StatusMeasured: ± 6.00e+20 kg (0.0001 relative)
SourceIAU/IERS Conventions (2010); GM⊕ divided by CODATA 2022 G
CategoriesAstronomical
Mass of the Earth in every mass unit
unified atomic mass unit (dalton)3.5965429e+51 u
picogram5.9722000e+39 pg
nanogram5.9722000e+36 ng
microgram5.9722000e+33 μg
milligram5.9722000e+30 mg
centigram5.9722000e+29 cg
grain9.2165131e+28 gr
metric carat2.9861000e+28 ct
gram5.9722000e+27 g
pennyweight3.8402138e+27 dwt
dram3.3706105e+27 dr
ounce2.1066316e+26 oz
troy ounce1.9201069e+26 oz t
troy pound1.6000891e+25 lb t
pound1.3166447e+25 lb
kilogram5.9722000e+24 kg
stone9.4046052e+23 st
slug4.0922569e+23 slug
US hundredweight1.3166447e+23 cwt
UK long hundredweight1.1755756e+23 cwt (UK)
quintal5.9722000e+22 q
US short ton6.5832236e+21 ton
metric tonne5.9722000e+21 t
UK long ton5.8778782e+21 long ton
kilotonne5.9722000e+18 kt
megatonne5.9722000e+15 Mt
gigatonne5,972,200,000,000 Gt
Earth mass1 Mearth
solar mass0.0000030035053 Msun

Learning zone

Henry Cavendish's 1798 torsion-balance experiment was reported not as a measurement of G but under the title of weighing the Earth: measure the tiny attraction between lead spheres, compare it with the planet's pull on the same masses, and the Earth's density follows. He got 5.48 times water, within one per cent of the modern 5.514 — a stunning result for an apparatus so sensitive he operated it from another room through a telescope.

The situation is unchanged in principle today. Satellite geodesy gives GM⊕ to nine digits, but converting to kilograms still means dividing by G, so Earth's mass is quoted to only five. Roughly a third of that mass is the iron core, and the whole planet is 81.3 times the mass of the Moon.