A Historical Perspective
From Aristotle to Hawking
Force & Its Effects
Measurement Limitations
 
The Strain Gage
Sensor Designs
Measuring Circuits
Application & Installation
 
Process Pressure Measurement
From Mechanical to Electronic
Transducer Types
Practical Considerations
 
High Pressure & Vacuum
High Pressure Designs
Very High Pressures
Vacuum Instrumentation
 
Pressure Gauges
& Switches
Pressure Gauge Designs
Protective Accessories
Pressure Switches
 
Force, Acceleration,
& Torque
Force Sensors
Acceleration & Vibration
Torque Measurement
 
Load Cell Designs
Operating Principles
New Sensor Developments
Strain Gage Configurations
 
Weighing Applications
Weighing System Design
Installation & Calibration
Specialized Installations
 
Information Resources
Glossary
Index
List of Figures
Data Tables
 
Technical Learning Home

Vacuum Measurement
Engineers first became interested in vacuum measurements in the 1600s, when they noted the inability of pumps to raise water more than about 30 ft. The Duke of Tuscany in Italy commissioned Galileo to investigate the "problem." Galileo, among others, also devised a number of experiments to investigate the properties of air. Among the tools used for these experiments were pistons to measure force and a water barometer (about 34 ft. tall) to measure vacuum pressure.

Figure 4-3: Barometer
Operation

  After Galileo's death in 1642, Evangelista Torricelli carried on the work of vacuum-related investigation and invented the mercury barometer (Figure 4-3). He discovered that the atmosphere exerts a force of 14.7 lb. per square in. (psi) and that, inside a fully evacuated tube, the pressure was enough to raise a column of mercury to a height of 29.9 in. (760 mm). The height of a mercury column is therefore a direct measure of the atmospheric pressure.

Figure 4-4: Vacuum Gauge Measurement Ranges

  In 1644, French mathematician Blaise Pascal asked a group of mountaineers to carry a barometer into the Alps and proved that air pressure decreases with altitude. The average barometric pressure at sea level can balance the height of a 760 mm mercury column, and this pressure is defined as a standard Atmosphere. The value for 1/760th of an atmosphere is called a torr, in honor of Torricelli.
  In 1872, McLeod invented the McLeod vacuum detector gauge, which measures the pressure of a gas by measuring its volume twice, once at the unknown low pressure and again at a higher reference pressure. The pressurized new volume is then an indication of the initial absolute pressure. Versions of the McLeod Gauge continue to be used today as a standard for calibrating vacuum gauges.

Applications
Vacuum gauges in use today fall into three main categories: mechanical, thermal, and ionization. Their pressure ranges are given in Figure 4-4. In general, for high vacuum services (around 10-6 torr), either cold cathode or Bayard-Alpert hot cathode gauges are suitable. Neither is particularly accurate or stable, and both require frequent calibration.
  For vacuums in the millitorr range (required for sputtering applications), one might consider a hot cathode ion gauge. For more accurate measurements in this intermediate range, the capacitance manometer is a good choice. For intermediate vacuum applications (between 10-4 and 10-2 torr), capacitance manometers are the best in terms of performance, but are also the most expensive. The lowest priced gauge is the thermocouple type, but its error is the greatest. Digital Pirani gauges can represent a good compromise solution, with accuracy between that of capacitance and thermocouple sensors.
  For low vacuums (higher pressures) between atmospheric and 10-2 torr, Bourdon tubes, bellows, active strain gages, and capacitance sensors are all suitable.

       
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