Infrared thermography
What it is ...


How does the camera “see” heat?
All objects, cold or hot, radiate heat in the form of infrared energy. As an object increases in temperature, it radiates more energy and the wavelength gets shorter. Infrared radiation, visible light and ultraviolet light are all forms of energy in the electromagnetic spectrum. The only difference is their wavelength or frequency.

The human eye can only see a narrow range of wavelength in the electromagnetic spectrum. These wavelengths range in length from 0.4 to 0.7 microns (a micron is one millionth of a metre). Most of what the eye sees is reflections from objects that high energy from the sun or an incandescent light bulb is striking. If the temperature of an object gets hot enough, however, above 525°C the energy from that object will radiate energy in the visible spectrum and we will see it. This is when we see an object like the burner on an electric stove “glowing” red. In fact any time an object will emit or reflect energy in the same frequency of our eyes we will see it. Mostly, however we see reflections.

Taking thermal images and gathering thermal information is quite easy these days, just push the auto button and there is an image! This is simple on the surface, but it is not as easy as it sounds. The real work — and value — is what the thermographer understands about the object of interest, how it operates, the heat transfer within and to the surface of the object and how to adjust the camera to enhance the thermal details necessary to evaluate the image once it is stored and downloaded on to the computer. Then it is usually necessary to prepare a report that is accurate, clearly presented and easy to read by the maintenance personnel, who generally do not know anything about infrared thermography. As in any method of non-destructive testing, the interpretation of the information gathered takes both education and experience.
A good thermographer must thoroughly understand all the variables.