'by using this formula , Q=A*V, M3/Sec=M2*M/Sec'
i think it is width X depth X velocity=discharge ?
Typically, 0.3 psi below atmospheric pressure. No pump can pull more pressure than what is available in the atmosphere, because the number of molecules available for movement is so low.
Static pressure is .434 X height Example 10 ft x .434 4.34 PSI to prove take 2.31 PSI x 4.34 To find FORCE to need to calculate the diameter of the piping and the height and then the weight of the water inside the pipe
Blue
Inlet pressure/discharge pressure
for a simple reason because it has high discharge than any other available pump. the centrifugal pump uses the centrifugal force to push out the fluid centrifugal force = (mass *velocity2)/radius. hence centrifugal force is directly proportional to the square of the velocity, in this case being the velocity of the fluid. power provided to pump proportional to the force exerted by the impeller.hence higher the power results in higher centrifugal force implying square of the velocity of the fluid. higher the velocity of the fluid higher the discharge of the pump.
Q (Discharge in m3/s) = A (cross-sectional area in m2) x u (velocity - a corrected value in m/s)
Discharge Velocity is obtained by Dividing the Total Discharge by the total cross Sectional Area , Where Total cross sectional area Consists of void+solid. In contrast .. Seepage Velocity is defined as the total discharge by the Area of voids only. So Seepage velocity always greater than Discharge Velocity.
When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
When a stream's discharge increases, erosive energy increases.
The carrying capacity of a stream is influenced by its discharge and velocity. A higher discharge and velocity typically allow a stream to transport larger sediments and materials downstream, increasing its carrying capacity. Conversely, lower discharge and velocity may limit the stream's ability to carry sediment and materials.
To calculate the change in velocity of an object, you subtract the initial velocity from the final velocity. The formula is: Change in velocity Final velocity - Initial velocity.
The calculation will depend on how deep in the ground the submersible pump is installed and where the outlet for the water is e.g. is it above ground. Speak to the company that installed the pump to see if they can provide you with that data.
i think it is width X depth X velocity=discharge ?
discharge velocity is the quantity of flow that flows through a unit cross sectional area of the soil in a unit time discharge velocity is used to determine the quantity of flow through soil seepage velocity the actual rate of movement of the water as measured with dye tracer for instance, is the seepage velocity
The carrying capacity of a stream is influenced by its discharge and velocity. Higher discharge and faster velocity can increase the stream's ability to transport sediment and debris, thus raising its carrying capacity. Conversely, lower discharge and slower velocity may result in a reduced carrying capacity as the stream has less energy to move material.
There isn't, you have to measure it directly or via a flow measuring device, or refer to the manufacturer's tables and calculate it from those.