18  Thermographic measurement techniques

18.1  Introduction

An infrared camera measures and images the emitted infrared radiation from an object. The fact that radiation is a function of object surface temperature makes it possible for the camera to calculate and display this temperature.
However, the radiation measured by the camera does not only depend on the temperature of the object but is also a function of the emissivity. Radiation also originates from the surroundings and is reflected in the object. The radiation from the object and the reflected radiation will also be influenced by the absorption of the atmosphere.
To measure temperature accurately, it is therefore necessary to compensate for the effects of a number of different radiation sources. This is done on-line automatically by the camera. The following object parameters must, however, be supplied for the camera:
  • The emissivity of the object
  • The reflected apparent temperature
  • The distance between the object and the camera
  • The relative humidity
  • Temperature of the atmosphere

18.2  Emissivity

The most important object parameter to set correctly is the emissivity which, in short, is a measure of how much radiation is emitted from the object, compared to that from a perfect blackbody of the same temperature.
Normally, object materials and surface treatments exhibit emissivity ranging from approximately 0.1 to 0.95. A highly polished (mirror) surface falls below 0.1, while an oxidized or painted surface has a higher emissivity. Oil-based paint, regardless of color in the visible spectrum, has an emissivity over 0.9 in the infrared. Human skin exhibits an emissivity 0.97 to 0.98.
Non-oxidized metals represent an extreme case of perfect opacity and high reflexivity, which does not vary greatly with wavelength. Consequently, the emissivity of metals is low – only increasing with temperature. For non-metals, emissivity tends to be high, and decreases with temperature.

18.2.1  Finding the emissivity of a sample

18.2.1.1  Step 1: Determining reflected apparent temperature

Use one of the following two methods to determine reflected apparent temperature:
18.2.1.1.1  Method 1: Direct method
You can not use a thermocouple to measure reflected apparent temperature, because a thermocouple measures temperature, but apparent temperatrure is radiation intensity.
18.2.1.1.2  Method 2: Reflector method

18.2.1.2  Step 2: Determining the emissivity

18.3  Reflected apparent temperature

This parameter is used to compensate for the radiation reflected in the object. If the emissivity is low and the object temperature relatively far from that of the reflected it will be important to set and compensate for the reflected apparent temperature correctly.

18.4  Distance

The distance is the distance between the object and the front lens of the camera. This parameter is used to compensate for the following two facts:
  • That radiation from the target is absorbed by the atmosphere between the object and the camera.
  • That radiation from the atmosphere itself is detected by the camera.

18.5  Relative humidity

The camera can also compensate for the fact that the transmittance is also dependent on the relative humidity of the atmosphere. To do this set the relative humidity to the correct value. For short distances and normal humidity the relative humidity can normally be left at a default value of 50%.

18.6  Other parameters

In addition, some cameras and analysis programs from FLIR Systems allow you to compensate for the following parameters:
  • Atmospheric temperature – i.e. the temperature of the atmosphere between the camera and the target
  • External optics temperature – i.e. the temperature of any external lenses or windows used in front of the camera
  • External optics transmittance – i.e. the transmission of any external lenses or windows used in front of the camera