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At Higher Altitudes Cosmic Rays

Summary

The Objective: the aim of my experiment is to seek out if there square measure additional cosmic rays at higher altitudes than at lower altitudes. I think that there square measure aiming to be additional cosmic rays at higher altitudes thanks to the agent layer of the atmosphere. For police investigation the cosmic rays, I’ll build a setup.

 

Methods and Materials

To perform this experiment, I took the setup to a few locations in urban center County.
Each one was at totally different altitudes, varied by concerning 3000 linear unit.
At every location, I recorded the number of cosmic rays that I saw withstand the setup in twenty one-minute intervals.
I calculated the typical variety of cosmic rays at every location.

 

Results

The average variety of cosmic rays throughout the primary session at concerning 6000 linear unit. was 20.1 per minute.
The average variety at concerning 3000 linear unit. was 19.8 per minute.
The average variety perplexed level was seven.35 per minute.
During the second session, the typical variety of cosmic rays at concerning 6000 linear unit. was 25.8 per minute.
The average variety of cosmic rays perplexed level was eleven.65 per minute.

 

Conclusions

In conclusion, my hypothesis was verified correctly. I believed that there would be additional cosmic rays at higher altitudes. My experiment showed that the typical variety of cosmic rays at higher altitudes was quite at lower altitudes. I believed that there would be additional cosmic rays at higher altitudes thanks to the agent layer of atmosphere at higher altitudes.
Our conclusion is about this experiment is that there are square measure additional cosmic rays at higher altitudes than at lower altitudes, by employing a setup.

 

TAG
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At Higher Altitudes Cosmic Rays Summary The Objective: the aim of my experiment is to seek out if there square measure additional cosmic rays at higher altitudes than at lower altitudes. I think that there square measure aiming to be additional cosmic rays at higher altitudes thanks to the agent layer of the atmosphere. For […]

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