Process Variables: Pressure

"Pressure" is the ratio of a normal force to the area on which the force acts. Units are thus psi or Pa.

Hydrostatic Pressure

Hydrostatic Pressure

Think of a column of fluid of height h and cross sectional area A. The fluid has a density rho. The pressure P at the base of the column is by definition the force exerted on the base divided by the area A; that force is the weight of the column plus any force acting on the top.

Hydrostatic Pressure
This is the formula for the pressure due to a column of fluid, or "hydrostatic pressure".

EXAMPLE: What is the hydrostatic pressure exerted by the water in a 6.00 ft diameter cylindrical tank which contains 90.0 gal?

If we look at the hydrostatic pressure formula, we see that we need the pressure at the top of the column, the density of the fluid, and the height of the column.

The density we look up: 62.4 lbm/ft3 for water

We aren't given the height of the column, but we do have dimensions on the tank. Since the volume is the product of the area and the height, we should be able to back out the desired number.

Assume: tank has constant cross-section

area and height
Assume: no pressure acting on top of column
We do this because we're given no better information. Actually, the air above the column exerts a pressure.
pressure

Atmospheric Pressure

Air is a fluid -- so the air above the earth exerts a hydrostatic pressure on the surface. This is atmospheric pressure. If you look at the hydrostatic pressure equation, you can see that the pressure exerted will depend on the height of the column and the density of the air. At sea level the pressure is

atmospheric pressure
It will decrease as as the altitude increases. The reduced pressure is why breathing is more difficult ("at altitude" for athletes).

For many calculations, it is useful to have a fixed reference value for atmospheric pressure. The sea-level value is used. It is called the "standard atmosphere". This value is also used as a unit of pressure measurement (atm). It may be used in homework problems, etc., if there is no other information given about atmospheric conditions.

"Head"

In your chemistry classes, you've probably seen pressures measured in mm Hg (a.k.a. Torr). These aren't "natural" pressure units (force/area) -- so where did they come from? We just observed that a column of fluid produces a pressure, so that the height of the column is an indicator of the pressure produced. This principle is the basis of one of the traditional methods of measuring pressure: the manometer. When pressure is expressed in terms of a height of fluid, it is called fluid "head". Usually, water or mercury is used.

fluid head
Head units are mostly used for very low pressures and expressed as "mm Hg" or "in H2O".

Converting between force/are and head units is simple. You use the fluid weight term from the hydrostatic pressure equation:

head conversion

EXAMPLE: Take the result from above and express it in "head".

head example

Manometers

An old, simple way of measuring pressure is with a "manometer". A u-shaped tube is partially filled with liquid, usually water or mercury. Each end is connected to a pressure source, and the difference in liquid height corresponds to the difference in pressure.

Manometer

At the bottom of the manometer, the force exerted by one leg balances against the force exerted by the other. The force balance equation can be written:

manometer equation
This is the general form of the "manometer equation" and can be used to solve just about any manometer type problem. If you learn this equation, you can readily simplify it for any case you encounter -- multiple fluids, tap pressures, etc.

Often, a manometer is connected so that the same fluid is present at the tops of both legs. In this case, and if only a single manometer fluid is used, there are only two densities, and the terms can be lumped together. You can also group the two height terms and express them as a difference. This gives the "differential manometer equation":

differential manometer equation

The differential manometer equation is frequently used to help determine a flow rate. If a restriction (an orifice, valve, etc.) is placed in a line carrying a flowing fluid, it will produce a pressure drop. A manometer can then be used to measure the pressure drop. The pressure difference is proportional to the flow rate squared.

Absolute vs. Gage

If you look at the manometer, you'll see that it doesn't really measure a pressure, but instead detects the difference in pressure between the taps. Almost all pressure measurement devices have the same limitation. Thus, most pressures are measured with reference to some known value.

Getting "zero" pressure can be complicated and expensive. For most measurements, it is more practical to measure with respect to atmospheric pressure. For example, to use a manometer, you may attach one end to the pressure source to be measured and leave the other open to the atmosphere. This is so common that pressures measured in this way are designated gage pressure. If absolute pressure is to be measured, it is necessary to evacuate one end of the manometer so that the fluid works against vacuum.

absolute pressure

Thus, a "closed end" manometer measures absolute pressure, while an "open end" manometer measures gage pressure. A "barometer" measures atmospheric pressure.

Pressures less than atmospheric are "vacuums". Common practice is to state negative gage pressures as positive vacuum. Vacuums are frequently listed in head units.

vacuum

The chart below may help keep track of things.

Pressure Chart

References:

  1. R.M. Felder and R.W. Rousseau, Elementary Principles of Chemical Processes (2nd edition), John Wiley, 1986, pp. 55-62.

R.M. Price
Original: 6/3/94
Modified: 9/1/94,6/21/96,7/13/98, 9/1/98; 5/25/2004

Copyright 1998, 2004 by R.M. Price -- All Rights Reserved

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