Pressure head

Source: Wikipedia, the free encyclopedia.

In fluid mechanics, pressure head is the height of a liquid column that corresponds to a particular pressure exerted by the liquid column on the base of its container. It may also be called static pressure head or simply static head (but not static head pressure).

Mathematically this is expressed as:

where

is pressure head (which is actually a
centimetres of water
)
is fluid pressure (i.e. force per unit area, typically expressed in pascals)
is the specific weight (i.e. force per unit volume, typically expressed in N/m3 units)
is the density of the fluid (i.e. mass per unit volume, typically expressed in kg/m3)
is acceleration due to gravity (i.e. rate of change of velocity, expressed in m/s2).

Note that in this equation, the pressure term may be

absolute pressure
, depending on the design of the container and whether it is open to the ambient air or sealed without air.

Head equation

Pressure head is a component of

incompressible fluids
:

where

is velocity head,
is elevation head,
is pressure head, and
is a constant for the system

Practical uses for pressure head

Venturi meter
with two pressure instruments open to the ambient air. ( and ) If the meter is turned upside down, we say by convention that and the fluid inside the vertical columns will pour out the two holes. See discussion below.

physical properties
.

For example, if the original fluid was

cm H2O
", then an equivalent measurement is "1.00 cm Hg".

This example demonstrates why there is some confusion surrounding pressure head and its relationship to pressure. Scientists frequently use columns of water (or mercury) to measure pressure (manometric

inches of water" makes sense for instrumentation
, but these raw measurements of head must frequently be converted to more convenient pressure units using the equations above to solve for pressure.

In summary pressure head is a measurement of length, which can be converted to the units of pressure (force per unit area), as long as strict attention is paid to the density of the measurement fluid and the local value of g.

Implications for gravitational anomalies on ψ

We would normally use pressure head calculations in areas in which is constant. However, if the gravitational field fluctuates, we can prove that pressure head fluctuates with it.

  • If we consider what would happen if gravity decreases, we would expect the fluid in the venturi meter shown above to withdraw from the pipe up into the vertical columns. Pressure head is increased.
  • In the case of weightlessness, the pressure head approaches infinity. Fluid in the pipe may "leak out" of the top of the vertical columns (assuming ).
  • To simulate negative gravity, we could turn the venturi meter shown above upside down. In this case gravity is negative, and we would expect the fluid in the pipe to "pour out" the vertical columns. Pressure head is negative (assuming ).
  • If and , we observe that the pressure head is also negative, and the ambient air is sucked into the columns shown in the venturi meter above. This is called a siphon, and is caused by a partial vacuum inside the vertical columns. In many venturis, the column on the left has fluid in it (), while only the column on the right is a siphon ().
  • If and , we observe that the pressure head is again positive, predicting that the venturi meter shown above would look the same, only upside down. In this situation, gravity causes the working fluid to plug the siphon holes, but the fluid does not leak out because the ambient pressure is greater than the pressure in the pipe.
  • The above situations imply that the Bernoulli equation, from which we obtain static pressure head, is extremely versatile.

Applications

Static

A

absolute pressure
using the above equations.

If we had a column of mercury 767 mm high, we could calculate the atmospheric pressure as (767 mm)•(133 kN/m3) = 102 kPa. See the

millimeter of mercury, and pascal (unit)
articles for barometric pressure measurements at standard conditions.

Differential

manometer
) and partially filled with water. The meter is "read" as a differential pressure head in centimeters or inches of water.

The

gauge pressure
, using the above equations.

Velocity head

The pressure of a fluid is different when it flows than when it is not flowing. This is why

velocity head, which is a term of the Bernoulli equation that is zero when there is no bulk motion of the fluid. In the picture on the right, the pressure differential is entirely due to the change in velocity head of the fluid, but it can be measured as a pressure head because of the Bernoulli principle. If, on the other hand, we could measure the velocity of the fluid, the pressure head could be calculated from the velocity head. See the Derivations of Bernoulli equation
.

See also

External links