Hot-wire spatial averaging
ID: hot-wire-spatial-averaging
Hot-wire spatial averaging is the loss or alteration of small-scale flow information because a heated sensing wire has finite spatial extent. Even a perfectly fast electronic readout observes a spatially distributed heat-transfer response. The manufacturer's practical guide relates spatial resolution to wire dimensions, flow and instrument frequency response.[ref]
An original small-perturbation model treats the inferred velocity fluctuation as a uniform line average over wire length . With measuring distance along the wire,For a spatial sinusoid , direct integration givesThis is a sinc function transfer factor. It follows from the stipulated uniform weighting and local linearity; a real wire's nonuniform temperature and nonlinear heat transfer require a more detailed spatial kernel.
For spatial wavelength , a fluctuation with has amplitude factor about and variance or power factor . At , the factors are and . At , one complete sinusoidal cycle lies along the wire and its line average is exactly zero. Raising the sample rate cannot restore a component that this spatial average has canceled.
For a wire, these illustrative wavelengths are , and . The result depends on the component of the spatial wavevector along the wire, rather than only on a temporal frequency. Orientation-dependent spatial filtering by a hot wire matters because a moving three-dimensional structure can have different projections along the wire and the mean flow. Under a frozen-advection model, temporal frequency obeys ; substituting into the wire-length factor requires an additional alignment assumption.
Spatial and temporal filters can both reduce measured fluctuation variance. In this single-sinusoid model, the measured variance is times the true variance even with noiseless electronics. A correction obtained by dividing by becomes unstable near its zeros, amplifying measurement noise without recovering independently lost information.
A proposed test compares probes of different active lengths in the same statistically repeatable flow, after separate steady calibrations and matched electronic filtering. Record wire orientation, support geometry, ambient temperature and traverse location; compare fluctuation spectra as well as mean velocity. A difference that tracks wire length supports a spatial-filtering interpretation, but changed thermal response or probe disturbance must also be checked. The observation establishes the filtered response of the actual apparatus over its characterized range, not an unqualified point measurement at every turbulent scale.
New to topics? Read the docs here!
