Conclusion for atmospheric pressure.
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Atmospheric pressure is defined as the pressure exerted by atmospheric air on the
surface area of earth, due to the force of gravitational attraction. Therefore, it is
related to the weight of the air column on the earth’s surface. However, air is a gas
mixture and expands to use the entire volume available, exerting pressure, not only
on the ground, but in all directions.
Normal atmospheric pressure is equal to the pressure exerted by a mercury column
at a sea level of 76 cm, at 0 °C. We call this value atmosphere (atm.) and use it as a
relative unit for pressure. Besides atmospheres, other pressure units are the mercury
millimeters (mmHg), milibars (mbar) and kilopascals (kPa).
So we have:
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