SUMMARY
Objects entering the ocean do not burn up like those entering the atmosphere due to several key factors. The primary mechanism for atmospheric burnup is the compression of gases in front of the object, which generates significant heat. In contrast, water, being incompressible, absorbs heat and dissipates it quickly, preventing combustion. Additionally, the ocean lacks sufficient free molecular oxygen to sustain a fire, further inhibiting combustion in underwater impacts.
PREREQUISITES
- Understanding of atmospheric entry physics
- Knowledge of fluid dynamics and incompressible fluids
- Familiarity with combustion chemistry
- Basic principles of heat transfer and thermodynamics
NEXT STEPS
- Research the physics of atmospheric entry and its effects on meteoroids
- Explore the properties of incompressible fluids and their impact on heat dissipation
- Study combustion chemistry, focusing on the role of oxygen in sustaining fires
- Investigate the effects of high-energy impacts in both liquid and solid mediums
USEFUL FOR
Students of physics, aerospace engineers, and anyone interested in the dynamics of atmospheric entry and underwater impacts.