Abstract
AbstractDie Änderung der DK von α‐FeOOH, β‐FeOOH und γ‐FeOOH mit der adsorbierten Wassermenge wird bei 30°C im Frequenzbereich 200 H2 bis 100 kHz untersucht, um Einblick in den Wasseradsorptionsmechanismus zu gewinnen.
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