We explain what the pressure is and the types that exist. In addition, examples of this physical magnitude and its relation to temperature.
It is known as pressure to physical scalar represented by the symbol p , designating a projection force exerted perpendicularly on a unit area; In other words, it represents how to apply a resulting force on a line.
It relates a continuous force of action and a surface on which it acts, so it is measured in the International System (SI) in pascals (Pa), each equivalent to a newton (N) of force acting on a cubic meter (m3) of surface. In the English system, on the other hand, the measure of pounds ( pounds ) per inches ( inches ) is preferred .
It is also one of the forces which are commonly subjected matter (such as temperature), and whose handling has numerous practical applications. One of them is that the increase in pressure at which matter is found can force it to change from aggregation state , that is, to pass from gas to liquid, for example, as is usually done with hydrocarbon gases.
Other units of it, measurement include bar (10N / cm3), atm or atmosphere (equivalent to about 101325 pa), or Torr (equivalent to 133.32 pascals) and measurable in millimeters of mercury (mmHg). The device designed to measure it, is known as a tensiometer .
Depending on the conditions in which it occurs, it can be classified according to the following types:
Some everyday examples of the action of it can be:
Both are intimately connected . When a compressible substance (such as a liquid, or better still, a gas) is subjected to high pressures that force its ordinarily dispersed particles to approach each other and vibrate faster, an accumulation of energy occurs that It is usually released as heat.
This relationship is described by the Gay-Lussac Law, which establishes a direct ratio between the pressure of a fixed volume of a gas and its temperature, according to the formula:
P / T = k
Where P is pressure, T is temperature and k is a constant.
Other evidence of this occurs when ascending in the atmosphere , where a loss of pressure is experienced, not having so much air on top of it, and at the same time a loss of heat is experienced.
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