Planetary Sphere of Influence Calculator

Model planetary dominance where orbits transition to satellites. Choose units, include eccentricity, and validate inputs. Save outputs for missions, homework, and quick comparisons today.

Calculator

Choose which radius to highlight in the result.
For planets, use the orbit about the primary body.
Used for Hill-at-periapsis; keep 0 for circular.
This is the planet or moon you are testing.
This is the star or planet being orbited.

Example data

Approximate reference cases for quick testing.

Case a e m M SOI (Laplace), km Hill (circular), km
Earth about Sun 1 AU 0.0167 1 Earth 1 Solar ~ 9.29e5 ~ 1.50e6
Moon about Earth 384,400 km 0.0549 0.0123 Earth 1 Earth ~ 6.61e4 ~ 6.16e4
Jupiter about Sun 5.204 AU 0.0489 1 Jupiter 1 Solar ~ 4.82e7 ~ 5.31e7

Formula used

This tool reports three related radii. The highlighted one depends on your model selection.

  • Laplace sphere of influence: rSOI = a · (m/M)2/5
  • Hill radius (circular): rH = a · (m/(3M))1/3
  • Hill radius at periapsis: rH,p = a · (1 − e) · (m/(3M))1/3

Here, a is the semi-major axis, e is eccentricity, m is the secondary mass, and M is the primary mass.

How to use this calculator

  1. Select the model you want to highlight: Laplace SOI, Hill (circular), or Hill (periapsis).
  2. Enter the semi-major axis a of the secondary’s orbit about the primary.
  3. Enter masses for the secondary m and primary M using the unit menus.
  4. If the orbit is eccentric, enter e; otherwise keep it near zero.
  5. Click Calculate. The result panel appears above the form, with CSV/PDF export buttons.

Article

1) Why a sphere of influence is useful

Gravity from the primary and secondary overlaps everywhere, so trajectory work uses a practical boundary to decide which two-body model is dominant. A sphere of influence supports clean reference-frame handoffs, quick sizing of approach arcs, and consistent assumptions in reports and coursework.

2) Laplace radius for patched-conic handoffs

The Laplace sphere of influence is commonly used in patched-conic navigation because it scales as r = a (m/M)^{2/5}. It is not a strict stability limit, but it often provides a reasonable distance to switch from heliocentric propagation to planetocentric hyperbolic arrival and departure geometry.

3) Hill radius for stability intuition

The Hill radius comes from the circular restricted three-body problem and scales as r = a (m/(3M))^{1/3}. It relates to regions where long-lived bound motion around the secondary is more plausible. It is frequently used to screen whether moons, rings, or close satellites can remain bound over many orbits.

4) Using the correct orbital distance

The semi-major axis a should describe the secondary’s orbit about the primary. For a planet, use the planet–star semi-major axis. For a moon, use the moon–planet semi-major axis. Mixing distances from different frames is a common mistake that can shift radii by large factors.

5) Mass ratio drives the scale

Both models depend mainly on the mass ratio m/M, but with different exponents. Because these are power laws, increasing secondary mass by a factor of 10 raises Laplace SOI by about 10^{0.4} and Hill by about 10^{1/3}. The calculator reports the ratio to make sensitivity checks straightforward.

6) Eccentricity and periapsis conservatism

When the secondary orbit is eccentric, the tightest environment occurs at periapsis. A conservative stability estimate scales the Hill radius by (1 − e). This can be helpful for quick safety margins when choosing satellite altitudes, estimating capture robustness, or comparing candidates for temporary moonlets.

7) Typical Solar System magnitudes

As a reference, Earth’s Laplace SOI is roughly 9.3×10^5 km, while its Hill radius is about 1.5×10^6 km. Jupiter’s values are tens of millions of kilometers, enabling large satellite systems. Small bodies can have Hill regions comparable to their orbital separations, limiting stable companions.

8) Recommended workflow

Use Laplace SOI for patched-conic switching and flyby planning, and use Hill (especially periapsis Hill) when you need conservative stability intuition. After screening with these radii, validate final trajectories with n-body numerical integration and any needed non-gravitational forces. Export CSV or PDF to document inputs and assumptions.

FAQs

1) Is the sphere of influence a hard boundary?

No. It is an approximation used to simplify calculations. Real gravitational dominance changes gradually and depends on trajectory geometry and perturbations from other bodies.

2) When should I use the Hill radius instead?

Use the Hill radius when you care about long-term orbital stability around the secondary, such as satellite retention, ring stability, or approximate stable regions in three-body dynamics.

3) Why does the Laplace model use the 2/5 exponent?

It comes from a classical scaling argument balancing perturbations in patched-conic contexts. The exponent is not derived from strict stability, but it works well for engineering handoffs.

4) What does “Hill at periapsis” mean?

It multiplies the circular Hill radius by (1 − e), shrinking the stable region to reflect the closest approach to the primary. It is a conservative estimate.

5) Can I use this for moons orbiting planets?

Yes. Treat the moon as the secondary and the planet as the primary, and set a to the moon’s orbital semi-major axis around the planet.

6) Why do Laplace and Hill outputs differ?

They are based on different approximations and physical goals. Laplace is designed for reference-frame switching in transfers, while Hill is connected to three-body stability.

7) Does a larger radius guarantee stable satellites?

No. Stability also depends on orbital inclination, resonances, perturbations, and non-gravitational forces. Use these radii for screening, then validate with detailed dynamics.

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Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.