TDH Flashcards
Pump
A mechanical device that converts forms of energy into hydraulic energy.
Pump Classifications
Generally pumps can be classified into two classifications.
Positive Displacement
Centrifugal
POSITIVE DISPLACEMENT PUMPS
Operate by reducing the volume of space within the pump that the liquid can occupy. In a reciprocating pump the piston forces the liquid from the cylinder into the discharge line.
Centrifugal Pumps
Move liquid by increasing their speed rather than displacing or pushing them. The vanes do work on the fluid to increase the velocity without decreasing the pressure. The increased velocity is then recovered in the casing as increased pressure.
Centrifugal Force
According to Webster’s, it is the force which tends to impel a thing, or parts of a thing outward from the center of rotation.
Sump
A hydraulic structure that acts as a reservoir from which single of multiple pumps, arrange in parallel, may draw water.
Vortex
The phenomenon by which air enters a submerged suction pipe from the water surface. Usually a cause of poor pump performance when the suction pipe is not adequately submerged.
Manifold
A hydraulic structure used to distribute water under pressure. Can be used to supply fluid to or receive fluid from a parallel arrangement of multiple pumps.
RECIPROCATING Examples
Single or multiple design Piston Plunger Diaphragm Rotary Gear Rotary Screw Rotary Cam
CENTRIFUGAL Examples
These can be single or multi-stage, open or closed impeller
Radial Flow
Mixed Flow
Axial Flow
ATMOSPHERIC PRESSURE Definition
The force exerted on a unit area by weight of the atmosphere.
Standard atmospheric pressure at sea level is 14.7 pounds per square inch.
ATMOSPHERIC PRESSURE
1 Atmosphere = 14.7 PSI or 34 Feet of Water
ATMOSPHERIC PRESSURE - Higher Elevations
At higher elevations atmospheric pressure decreases because the imaginary square tube become shorter, therefore it’s weight decreases.
ATMOSPHERIC PRESSURE
Below sea level
The atmospheric pressure increases at elevations below sea level.
Equilibrium
Equilibrium Exists at the ocean surface because the atmosphere and pushes down and the ocean pushes up air by an equal but opposite amount.