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    Theoretical basics of thermography

    Thermography: knowledge and practice

    Any object with a temperature above absolute zero (0 Kelvin = -273.15 °C) emits infrared radiation (IR radiation). However, the human eye cannot perceive this because it is virtually blind in this wavelength range. Not so with the thermal imaging camera. Their core, the infrared detector, is sensitive to IR radiation. Based on the intensity of the IR radiation, it determines the temperature of the object surface and makes it visible to the human eye using a thermal image. This process is called thermography.

    To make the IR radiation visible, the detector detects it, converts it into electrical signals and gives each signal a specific color, which is then shown on the thermal imaging camera's display. Basically, thermal imaging cameras translate wavelengths from the infrared spectrum into wavelengths (colors) that humans can perceive.

    Contrary to a relatively common misunderstanding, you cannot use a thermal imaging camera to look into objects, but rather only make their surface temperature visible.

    Emission, Reflection, Transmission

    In order to use a thermal imaging camera as a tool efficiently, you should be able to understand these terms.

    Setting the emissivity

    Each material has a different emissivity. And for optimal thermal images you have to set this on the camera.

    Field of view and measuring spot

    Crucial know-how to be able to assess the technical properties of a thermal imaging camera.

    Thermography in practice

    Find out in our compact tutorial how theoretical basics and the right thermal imaging camera can be used to create meaningful thermal images in practice.

    Thermography in Practice