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Pressure is a fundamental concept in fluid mechanics, with significant implications across various industries. Static pressure, dynamic pressure, and total pressure are three interrelated measures that characterize the behavior of fluids in motion.
This article will explore the definitions, formulas, and practical applications of static, dynamic, and total pressure.
Static pressure is the pressure exerted by a fluid at rest. In other words, it is the force per unit area that a fluid exerts on the walls of its container or any other surface in contact with it, when there is no relative motion between the fluid and the surface.
Static pressure is a scalar quantity, meaning it has magnitude but no specific direction. It acts equally in all directions at a given point within a fluid. In a static fluid, the pressure at any point is the same in all directions.
The static pressure at a given point in a fluid depends on the depth of that point from the surface, the density of the fluid, and the acceleration due to gravity. As depth increases, the static pressure increases linearly, as there is more fluid above exerting its weight.
The static pressure at a point in a fluid can be calculated using the hydrostatic pressure equation:
P = ρgh
Where:
This equation shows that static pressure is directly proportional to the depth and density of the fluid. For example, in a water tank, the static pressure at a depth of 10 meters would be higher than at a depth of 5 meters, assuming the density remains constant.
Static pressure can be measured using various instruments such as pressure gauges, manometers, and pressure transducers. These devices typically measure the difference between the static pressure at a point and a reference pressure, such as atmospheric pressure.
Dynamic pressure, also known as velocity pressure, is the kinetic energy of a fluid particle due to its motion. It is the pressure a fluid exerts as it moves, which is always positive. The dynamic pressure is a function of fluid velocity and density.
Conceptually, dynamic pressure represents the pressure increase from converting all of a fluid’s kinetic energy at a point to pressure. In other words, if the fluid was brought to rest isentropically at a point, dynamic pressure is the increase in pressure above the original static pressure.
The dynamic pressure q is given by:
q = 1/2 * ρ * v^2
Where:
The units of dynamic pressure are Pascals (Pa) in the SI system, which is equivalent to N/m^2. To calculate dynamic pressure, the velocity must be measured relative to the fluid. In wind tunnel testing, dynamic pressure is calculated using the air velocity relative to the model being tested.
Total pressure, also known as stagnation pressure, is the sum of static pressure and dynamic pressure in a fluid flow system. It represents the maximum pressure that can be obtained if a flowing fluid is brought to rest isentropically, without any energy losses. The total pressure is constant along a streamline in an inviscid flow, as stated by Bernoulli’s principle.
The total pressure (P₀) can be calculated using the following formula:
P₀ = P + ½ρv²
Where:
This equation demonstrates that the total pressure is the sum of the static pressure and the dynamic pressure (½ρv²).
The relationship between static pressure, dynamic pressure, and total pressure is defined by the Bernoulli equation. In an inviscid, steady flow, the total pressure along a streamline remains constant. The static pressure decreases as the fluid velocity increases, while the dynamic pressure increases. Conversely, when the fluid velocity decreases, the static pressure increases, and the dynamic pressure decreases.