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To convert Earth masses to kg: multiply by 5.9722 × 10²⁴.
M⊕ = 5.9722 × 10²⁴ kg ≈ 5.972 Yg (yottagrams). Earth = 1 M⊕ by definition.
For example, 1 Earth's Mass (M⊕) = 2.744030e+32 Planck Mass (mₚ).
| Earth's Mass (M⊕) | Planck Mass (mₚ) |
|---|---|
| 0.1 | 2.744030e+31 |
| 0.5 | 1.372015e+32 |
| 1 | 2.744030e+32 |
| 2 | 5.488060e+32 |
| 5 | 1.372015e+33 |
| 10 | 2.744030e+33 |
| 25 | 6.860075e+33 |
| 50 | 1.372015e+34 |
| 100 | 2.744030e+34 |
| 500 | 1.372015e+35 |
| 1000 | 2.744030e+35 |
The Earth mass is the mass of planet Earth, approximately 5.972 × 10²⁴ kilograms.
M⊕ = 5.9722 × 10²⁴ kg ≈ 5.972 Yg (yottagrams). Earth = 1 M⊕ by definition.
To convert Earth masses to kg: multiply by 5.9722 × 10²⁴.
Expressing exoplanet masses (e.g., 'a planet of 3 Earth masses'), moon masses, and asteroid masses.
Earth gains about 40,000 tonnes of mass per year from cosmic dust — but that's only 10⁻¹⁷ of its total mass.
Earth's mass is hard to visualize. The key insight: it's known from G × M⊕ (the gravitational parameter), not M⊕ alone.
Cavendish 'weighed the Earth' by measuring G. If you know g (9.8 m/s²) and Earth's radius, you can calculate M⊕ = gR²/G.
The Planck mass is the fundamental natural unit of mass, approximately 2.176 × 10⁻⁸ kg (about 21.76 micrograms).
mₚ = √(ℏc/G) ≈ 2.176 × 10⁻⁸ kg ≈ 21.76 µg ≈ 1.31 × 10¹⁹ proton masses.
To convert Planck masses to kg: multiply by 2.176434 × 10⁻⁸.
No direct practical applications — a Planck mass is roughly the mass of a flea egg, but its significance is theoretical.
Unusually, the Planck mass is macroscopic (~22 µg) — about the mass of a flea egg, a grain of sand, or a small dust mite.
Expecting Planck mass to be extremely small like other Planck units — it's actually macroscopic (~22 µg).
Other Planck units are absurdly small or large, but the Planck mass is surprisingly human-scale: about 20 micrograms.



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