The composition of gases in exosphere is
Helium and Hydrogen.
The Earth's atmosphere is composed of several layers, each with distinct characteristics, including temperature, pressure, and gas composition. The exosphere is the outermost layer of the Earth's atmosphere, located above the thermosphere. It is the boundary layer between the rest of the atmosphere and outer space.
The exosphere begins at the top of the thermosphere, typically around 500 to 1000 kilometers (310 to 620 miles) above the Earth's surface, and extends upwards for thousands of kilometers. This layer is extremely thin, meaning the particles within it are very far apart. Due to the low density and weak gravitational pull at this altitude, particles can escape into space.
In the lower layers of the atmosphere (like the troposphere, stratosphere, mesosphere, and even the lower thermosphere), the gases are well-mixed, and the composition is primarily Nitrogen (\(\text{N}_2\)) and Oxygen (\(\text{O}_2\)). However, in the exosphere, this changes significantly. The low density and high altitude mean that gas particles are sorted by mass. Lighter gases tend to rise higher.
The primary gases found in the exosphere are the lightest elements: Helium (\(\text{He}\)) and Hydrogen (\(\text{H}_2\) or atomic \(\text{H}\)). Here's why they dominate:
Heavier gases like Nitrogen and Oxygen are much less likely to reach such high altitudes or achieve the escape velocity needed to remain dominant in the exosphere.
Let's look at the given options in the context of the exosphere's composition:
Based on the characteristics of the exosphere and atmospheric escape, Helium and Hydrogen are the main constituents.
The exosphere is characterized by its extremely low density and is primarily composed of light gases. The composition changes with altitude within the exosphere, but overall, Helium and Hydrogen are the most significant components at these uppermost altitudes.
| Atmospheric Layer | Approximate Altitude Range | Key Composition Notes |
|---|---|---|
| Troposphere | 0 - 7-15 km | Mostly N2 & O2; contains most water vapor & weather |
| Stratosphere | 7-15 km - 50 km | Mostly N2 & O2; contains Ozone layer |
| Mesosphere | 50 km - 85 km | Mostly N2 & O2; meteors burn up here |
| Thermosphere | 85 km - 500-1000 km | Atomic O, N, He, H; temperature increases with height |
| Exosphere | 500-1000 km and up | Primarily Helium & Hydrogen; transition to space |
The transition zone between the thermosphere and exosphere, sometimes called the exobase, is where the atmosphere becomes thin enough that particles are more likely to escape collisions than to collide with other particles. Above the exobase, particles follow ballistic trajectories, either falling back to Earth or escaping into space. This is why the lightest particles, Helium and Hydrogen, which have the highest thermal velocities, are most likely to be found in the exosphere and escape.
Satellite orbits, like those of the International Space Station, are typically within the lower parts of the thermosphere, experiencing some drag from the very thin atmosphere present there, which consists of residual Oxygen and Nitrogen as well as Helium and Hydrogen.
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