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Q1: Why are pressure differences normalized with dynamic pressure in the pitch and yaw equations?
Normalizing the differential pressures by the average dynamic pressure allows for:
Dimensionless calibration curves (∆P/𝑝_dyn), which generalize the relationship across varying flow speeds.
Reduced sensitivity to fluctuations in flow conditions.
Better polynomial fitting across different Mach numbers.
Q2: What could be the impact of incorrect alignment between the probe and flow in determining pitch/yaw angles?
Incorrect alignment introduces systematic error:
Skews the pressure distribution, which leads to wrong ∆P_pitch/∆P_yaw.
Causes incorrect estimation of local flow direction, leading to flawed calibration.
Errors propagate into mass flow estimation when velocity vectors are reconstructed later.
Q3: Why is a 5th-degree polynomial used to relate pressures to α, β, and velocity?
Captures the nonlinear and coupled effects of flow angle and speed on pressure distribution.
5th-degree is a compromise: flexible enough for good accuracy, but not overly prone to overfitting.
Also aligns with literature and previous calibration practices (e.g., Wörrlein).
Q4: What is the significance of the β parameter in ISO 5167-2, and how does it affect flow rate calculation?
β = d/D is the orifice diameter to pipe diameter ratio.
Affects the discharge coefficient C and expansion factor ε, which are critical in the mass flow equation.
Extreme β values (too small or too large) can lead to:
Flow separation,
Increased uncertainty,
Breakdown of the ISO 5167 assumptions.
Q5: Why must barometric pressure and temperature be recorded for the orifice method?
Needed to compute fluid density from ideal gas law:
ρ=p/RT
Accurate density is essential to convert volumetric flow to mass flow.
Pressure deviations or uncorrected temperature drifts would cause systematic mass flow error.
Q6: Why do we need to compute the Reynolds number and viscosity, and how are they used?
Reynolds number affects the discharge coefficient C, which is Re-dependent.
Viscosity (μ) is used in Re = ρVD/μ.
Accurate Re → accurate C → correct mass flow estimate.
Q7: Why is ring-wise integration used, and what assumptions does it rely on?
Assumes axisymmetric jet → simplifies 2D integral into 1D over radius:
Q˙=2π∑uiriΔri
Efficient and accurate for symmetric flows, reducing computational complexity.
If jet is asymmetric, ring-wise integration may underestimate localized features.
Q8: What are possible sources of error in this numerical integration method?
Insufficient spatial resolution (too large ∆r).
Interpolation errors between grid points.
Non-ideal jet alignment or turbulence.
Probe misalignment or drift during scan.
Q9: Why is dynamic pressure computed locally for each node in Measurement C?
Each node may have different flow speed and direction.
Using a single global dynamic pressure would misrepresent local conditions.
Local P_dyn → accurate local velocity → accurate volume integration.
Q10: How would you increase the accuracy of Measurement C results?
Use finer grid resolution (smaller ∆r).
Repeat measurements at each grid point and average.
Cross-check with Pitot or orifice-based results.
Ensure precise probe alignment and calibration.