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Bernoulliās principle describes how pressure, speed, and height (elevation) are related in fluid flow. For steady, incompressible, low-friction (negligible viscous effects) and essentially isentropic flow, the total energy per unit mass along a streamline is constant. In a horizontal flow, this implies that when the fluid speeds up, its static pressure decreases; when it slows down, its static pressure increases. The relationship is commonly expressed by Bernoulliās equation: v^2/2 + gz + p/Ļ = constant. Here v is flow speed, g is gravitational acceleration, z is elevation above a reference plane, p is static pressure, and Ļ is density. The equation shows that increases in kinetic energy (speed) must be balanced by decreases in potential energy (height term gz) and/or pressure energy (p/Ļ). In terms of āhead,ā the same idea can be written as velocity head + elevation head + pressure head = constant, making it clear how changes in height and pressure trade off with changes in speed.
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