Temporal Stability
Temporal stability involves the predictable change in a metrological characteristic over time under constant reference conditions. Most precision instruments exhibit an aging rate linear drift where the value shifts at a constant rate per year or per thousand hours. This movement occurs due to material relaxation or the gradual diffusion of impurities within a sensing element.
A manufacturer specifies this rate to allow users to predict when a device will exceed its stated accuracy limits, which facilitates the planning of maintenance intervals.
Drift Influence
Internal stresses within a resistive film often relax following the manufacturing process. While the aging rate linear drift remains the dominant factor in long-term instability, it is distinct from random fluctuations or thermal hysteresis. Estimating the magnitude of this shift allows for the calculation of an uncertainty budget over a multiyear calibration interval.
High stability components often undergo a burn-in period at elevated temperatures to ensure the drift rate has stabilized into a predictable linear slope before deployment. This pre-conditioning phase removes the initial non-linear behavior seen in new parts.
Calibration Interval
Maintenance schedules for secondary standards depend on the consistency of temporal changes. Because an aging rate linear drift is unidirectional and constant, a laboratory can apply a mathematical correction to the measured value between formal verification events. This approach extends the useful life of a sensor without requiring frequent hardware adjustments.
Verification against a primary standard confirms if the observed shift remains within the predicted linear bounds.
Temperature Sensitivity
Operating temperature influences the speed of chemical and physical changes. An elevated environment typically increases the aging rate linear drift through the Arrhenius effect. Establishing a correlation between temperature and drift allows for the qualification of components in harsh field conditions.
Monitoring the cumulative time at peak temperatures provides a basis for estimating the total drift accumulated.