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  4. /Hohmann Transfer Orbit Calculator

Hohmann Transfer Orbit Calculator

Calculator

Results

Transfer Direction

1

Target-to-Initial Radius Ratio

6.2207

x

Transfer Semi-Major Axis

24,471

km

Initial Circular Velocity

7.6686

km/s

Target Circular Velocity

3.0747

km/s

Transfer Velocity at Inner Radius

10.0661

km/s

Transfer Velocity at Outer Radius

1.6182

km/s

Departure Burn Magnitude

2.3975

km/s

Arrival Burn Magnitude

1.4565

km/s

Total Delta-V

3.854

km/s

Total Delta-V

3,854

m/s

Transfer Time

19,048.4

s

Transfer Time

5.291

h

Transfer Time

0.2205

days

Results

Transfer Direction

1

Target-to-Initial Radius Ratio

6.2207

x

Transfer Semi-Major Axis

24,471

km

Initial Circular Velocity

7.6686

km/s

Target Circular Velocity

3.0747

km/s

Transfer Velocity at Inner Radius

10.0661

km/s

Transfer Velocity at Outer Radius

1.6182

km/s

Departure Burn Magnitude

2.3975

km/s

Arrival Burn Magnitude

1.4565

km/s

Total Delta-V

3.854

km/s

Total Delta-V

3,854

m/s

Transfer Time

19,048.4

s

Transfer Time

5.291

h

Transfer Time

0.2205

days

The Hohmann Transfer Orbit Calculator computes the two velocity changes (delta-v) and transfer time needed to move a spacecraft between two coplanar circular orbits using the most fuel-efficient two-burn maneuver. Named after German engineer Walter Hohmann who described it in 1925, the Hohmann transfer is the foundation of orbital mechanics and is used for virtually every orbital altitude change and many interplanetary missions.

A Hohmann transfer works as follows: Starting in a circular orbit of radius r1, the spacecraft fires its engine prograde (in the direction of motion), increasing velocity and entering an elliptical transfer orbit. The periapsis (closest point) of this ellipse is at r1 and the apoapsis (farthest point) is at r2. After traveling half the ellipse (half the orbital period of the transfer orbit), the spacecraft reaches r2 with a velocity lower than the circular orbital velocity at r2. A second prograde burn accelerates it to the circular orbital velocity at r2, completing the transfer.

The first burn delta-v = v_transfer_periapsis - v_circle_r1, and the second burn delta-v = v_circle_r2 - v_transfer_apoapsis. Both burns are positive (prograde) when moving to a higher orbit (r2 > r1). When moving to a lower orbit, both burns are retrograde (the spacecraft decelerates). The total delta-v is the minimum possible for a two-impulse transfer between circular coplanar orbits.

The gravitational parameter GM (mu) is the product of the gravitational constant G and the central body's mass M. For Earth: GM = 398,600.4418 km^3/s^2. For the Sun: GM = 1.327 x 10^11 km^3/s^2. For Mars: GM = 42,828 km^3/s^2. Change this value to compute Hohmann transfers around other planets or the Sun.

Visual Analysis

How It Works

Transfer orbit semi-major axis: a = (r1+r2)/2. Velocities: v_circle = sqrt(GM/r). Transfer ellipse velocities: v = sqrt(GM*(2/r - 1/a)) from vis-viva equation. Delta-v1 = v_transfer_at_r1 - v_circle_r1. Delta-v2 = v_circle_r2 - v_transfer_at_r2. Transfer time = pi*sqrt(a^3/GM) (half the ellipse orbital period, in seconds, converted to hours/days).

Understanding Your Results

For Earth satellites, LEO (400 km altitude, r = 6778 km) to GEO (35786 km altitude, r = 42164 km): total delta-v = about 3.94 km/s, transfer time = about 5.25 hours. For interplanetary transfers using the Sun as central body, use solar GM and planetary orbital radii. Earth-Mars Hohmann: total delta-v ~5.6 km/s relative to Earth orbit, transfer time ~259 days.

Worked Examples

LEO to GEO Transfer (Earth Orbit)

Inputs

r1 km6778
r2 km42164
gm km3s2398600.4418

Results

v1 kms7.669
v2 kms3.075
dv1 kms2.456
dv2 kms1.466
total dv kms3.922
transfer time h5.256
transfer time days0.219

The classic LEO-to-GEO Hohmann transfer requires 3.92 km/s total delta-v and takes about 5.25 hours (half the GTO orbital period).

Earth to Mars Transfer (Heliocentric)

Inputs

r1 km149597870.7
r2 km227936640
gm km3s2132712440018

Results

v1 kms29.784
v2 kms24.13
dv1 kms2.946
dv2 kms2.648
total dv kms5.594
transfer time h6280
transfer time days261.7

The Earth-Mars Hohmann transfer takes about 262 days and requires 5.6 km/s relative to the planets' orbital velocities.

Frequently Asked Questions

Hohmann proved mathematically that for two coplanar circular orbits, no two-impulse maneuver can achieve the transfer with less total delta-v. The proof involves showing that the optimal departure and arrival points are exactly at periapsis and apoapsis of the transfer ellipse, which minimizes the velocity changes needed.

For very large radius ratio changes (r2/r1 > 11.94), a bi-elliptic transfer using three burns can be more efficient. However, the bi-elliptic transfer takes much longer (it goes out to a very large intermediate orbit). For typical Earth orbital maneuvers and most interplanetary missions, Hohmann is essentially optimal for two burns.

The vis-viva equation gives the speed at any point in an orbit: v^2 = GM*(2/r - 1/a), where r is the current distance from the central body and a is the semi-major axis. For a circular orbit (a = r), this simplifies to v = sqrt(GM/r). For the periapsis and apoapsis of the transfer ellipse, r = r1 or r2 and a = (r1+r2)/2.

The transfer time is half the orbital period of the transfer ellipse: T/2 = pi*sqrt(a^3/GM), where a = (r1+r2)/2. This ranges from about 5 hours for LEO-to-GEO to 259 days for Earth-to-Mars. During this time, the target body must have moved to exactly the right position to be at the arrival point when the spacecraft arrives — this defines the launch window.

For an interplanetary Hohmann transfer, the target planet must be ahead of the spacecraft by the right angle at departure, so that it arrives at the destination when the spacecraft does. For Mars, the optimal phase angle is about 44 degrees (Mars must be 44 degrees ahead of Earth at departure). This alignment repeats every synodic period (~26 months for Mars).

The Hohmann transfer assumes coplanar circular orbits. If the initial and target orbits have different inclinations, a combined plane change and altitude change is needed. Performing the plane change at the point of highest velocity is most efficient, but plane changes are very expensive in delta-v. The Hohmann transfer provides a baseline; inclination corrections add significantly to the total cost.

The Oberth effect means burns at high velocity (low altitude) are most efficient. In a Hohmann transfer, the first burn at periapsis (lowest altitude, highest velocity) benefits from the Oberth effect. Missions that use a low perigee for departure (lunar and interplanetary) exploit this by firing at periapsis rather than from a higher circular parking orbit.

GTO (Geostationary Transfer Orbit) is the transfer ellipse used to move from LEO to GEO. Its periapsis is in LEO and apoapsis is at GEO altitude. The launch vehicle delivers the satellite to GTO; the satellite's own apogee kick motor fires the second burn to circularize at GEO. This is the standard commercial satellite launch profile.

The Hohmann calculation assumes circular coplanar orbits and instantaneous (impulsive) burns. Real planets orbit in slightly elliptical, inclined orbits. Real burns take minutes to hours. Real missions use patched-conic approximation or full numerical integration to compute accurate trajectories. The Hohmann result is an excellent first estimate for mission planning.

A porkchop plot is a contour map showing total delta-v (or C3 launch energy) versus departure date and arrival date for an interplanetary mission. It reveals the optimal launch window (minimum delta-v) and how much extra propellant is needed for off-optimal departure dates. The shape of the minimum-delta-v region resembles a porkchop, giving the plot its name.

Sources & Methodology

Hohmann, W. Die Erreichbarkeit der Himmelskorper, 1925. Bate, R.R., Mueller, D.D., White, J.E. Fundamentals of Astrodynamics. Dover, 1971.
R

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