Name of calculation procedures | Measurements | Original magnitudes | Deviation 1 | Deviation 2 | Deviation 3 | Deviation 4 |
Deviation of ΔTС from the original magnitude | % | 0 | 33 | 67 | 100 | 3.3 |
Difference of the core temperature, ΔTС | К (˚С) | 3000 | 4000 | 5000 | 6000 | 3100 |
Magnetic induction on the planet’s pole, | T | 2.79 ´ 10−3 | 3.72 ´ 10−3/ 2.79 ´ 10−3 | 4.65 ´ 10−3/ 2.79 ´ 10−3 | 5.58 ´ 10−3/ 2.79 ´ 10−3 | 2.88 ´ 10−3/ 2.79 ´ 10−3 |
Deviation of from the original magnitude | % | 0 | 33 | 67 | 100 | 3,3 |
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Deviation of RС from the original magnitude | % | 0 | 10 | 20 | 30 | 40 |
Radius of the metal core, RС | m | 1 × 107 | 1.1 × 107 | 1.2 × 107 | 1.3 × 107 | 1.4 × 107 |
Magnetic induction on the planet’s pole, | T | 2.79 × 10−3 | 3.37 × 10−3/ 2.79 × 10−3 | 4.01 × 10−3/ 2.79 × 10−3 | 4.71 × 10−3/ 2.79 × 10−3 | 5.46 × 10−3/ 2.79 × 10−3 |
Deviation of from the original magnitude | % | 0 | 21 | 44 | 69 | 96 |
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Deviation of σ from the original magnitude | % | 0 | 9 | 18 | 27 | 36 |
Electrical conductivity of the metal core, σ | S/m | 1.1 × 105 | 1.2 × 105 | 1.3 × 105 | 1.4 × 105 | 1.5 × 105 |
Magnetic induction on the planet’s pole, | T | 2.79 × 10−3 | 3.04 × 10−3/ 2.79 × 10−3 | 3.29 × 10−3/ 2.79 × 10−3 | 3.55 × 10−3/ 2.79 × 10−3 | 3.8 × 10−3/ 2.79 × 10−3 |
Deviation of from the original magnitude | % | 0 | 9 | 18 | 27 | 36 |