Hohmann Transfer Calculations: Earth to Mars and Venus | Orbital Mechanics with Python

Added:

Transfer Basics
Orbital Math
Delta-V Values
Python Results
Model Limits
Mission Design

Transfer Basics

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Playing Section
  • 1

    Introduces Earth-to-Mars and Earth-to-Venus transfers.

  • 2

    Explains Hohmann transfer efficiency for orbit raising/lowering.

  • 3

    Sets scope for delta-v, semi-major axis, and flight time calculations.

Fundamental Keplerian orbital mechanics, including Kepler's Laws of Planetary Motion and orbital elements.
The Vis-Viva equation and its application to calculating velocities at specific points in circular and elliptical orbits.
Basic physics concepts of Delta-v (change in velocity), gravitational parameters (standard gravitational parameter, mu), and specific orbital energy.
Intermediate Python programming skills, particularly defining functions, working with the math or NumPy libraries, and basic plotting.
Calculating synodic periods and designing launch windows using porkchop plots.
Understanding the Patched Conics Approximation to model entering and leaving a planet's Sphere of Influence (SOI).
Solving Lambert's Problem to calculate transfer orbits when launch and arrival times are constrained.
Exploring alternative transfer methods, such as Bi-elliptic transfers and low-thrust continuous propulsion trajectories.
Developing multi-body orbital simulations in Python using numerical integration techniques like Runge-Kutta.
11.1K views226likes10:10@alfonsogonzalez-astrodynam2207Original Release: 2020-11-16

Hohmann transfers are the most efficient two-impulse method for transferring between two circular orbits around a central body, where the spacecraft performs two velocity changes (delta-V burns) at specific points in its trajectory; for orbit-raising transfers like Earth to Mars, both burns increase velocity in the direction of motion, while for orbit-lowering transfers like Earth to Venus, both burns decrease velocity opposite to motion; the calculations involve determining the semi-major axis of the transfer orbit as the average of the two planetary distances, computing velocities using the vis-viva equation v² = μ(2/r - 1/a), and finding the time of flight as half the orbital period π√(a³/μ); however, this analysis assumes two-body dynamics and ignores gravitational perturbations from other planets, requiring more sophisticated methods like Lambert's problem and patch conics for higher fidelity simulations.