Meaning
Constant baseline moisture measurements over extended periods indicate the absence of atmospheric ingress in a closed analytical system. The metric referred to as drift stability reflects the rate of background water absorption measured in micrograms per minute during a blank titration run. High stability is required to distinguish the genuine moisture released by heated polymer samples from the ambient humidity of the laboratory.
Achieving a low and steady background rate is the prerequisite for reliable trace analysis.
Titration Baseline
Titration cells must maintain a background moisture rate below ten micrograms per minute. Fluctuations in drift stability can obscure the water content of resins with very low dryness limits. If the baseline is unstable, the start of the sample measurement must be delayed until the system stabilizes.
This pre-conditioning step ensures the accuracy of subsequent runs.
Ambient Moisture
Humid laboratory air can infiltrate the titration vessel through worn septa or loose glass joints. To maintain drift stability, all seals must be regularly inspected and replaced when worn. Desiccant traps containing molecular sieves absorb incoming moisture before it can enter the reaction chamber.
These preventative measures keep the cell dry.
Calibration Frequency
Periodic evaluation of the background moisture rate helps determine when the titration reagents must be replaced. A loss of drift stability often indicates that the solvent is saturated or the generator electrode is fouled. Monitoring the daily baseline performance ensures consistent testing.