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Principle of operation:
The moisture uptake or loss of a material is determined by measuring the increase or loss of weight.
The samples are in an atmoshere with defined relative humidity at room temperature
- The sample is placed in a Hygrostate with defined relative Humidity
- The Hygrostate contains a saturated salt solution which sets
a defined relative humidity within the airspace above the solution
- The sample inside the Hygrostate is weighted with an analytical balance using a specially designed suspension
- The weight of the sample is continuously measured and the results are transferred to ExcelŽ
- Decrease and increase of weight characterize the humidity induced kinetics of a material
- When equilibrium between the sample and the atmosphere inside the Hygrostate is reached, the user may
change the Hygrostate and continue the measurements at a new relative humidity
- The equilibrium values over the chosen humidity standards define the sorption isotherm of a material
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