Apolonio Ordaz Resume
← Back to all projects

Wind tunnel testing · ME 347 · Cal Poly

Measured the drag on a cylinder two different ways.

In Cal Poly’s wind tunnel, my team of four measured air pressure around a cylinder and the wake behind it. One method matched published data and the other didn’t. Figuring out why was the real lesson.

Role
Testing & analysis
Team
4 students
Equipment
Wind tunnel, Pitot-static probe
Course
ME 347, Cal Poly
Flow over a pressure-tapped circular cylinder Parallel streamlines approach a circular cylinder, split around it, and form an expanding wake downstream. Pressure tap locations are shown around the cylinder. U∞ = 13.75 m/sD = 1.50 inVELOCITY DEFICIT+ TURBULENT WAKE
Test article and measurement logic — pressure taps map the surface load; a traversing Pitot-static probe maps the downstream wake.

The problem

Drag is hard to measure directly, so engineers infer it from pressure. But which measurement can you trust?

What I did

Recorded surface pressure every 10° around the cylinder and surveyed the wake at two distances behind it.

The result

The pressure data matched known behavior. I traced the wake mismatch to specific measurement error sources.

19surface pressure points
13.75m/s wind speed
2independent drag methods
2wake survey stations

How I did it

  1. 01

    Set up

    Mounted a brass cylinder across the flow and located its stagnation point.

  2. 02

    Measure

    Recorded pressure every 10° from front to back.

  3. 03

    Survey

    Traversed a probe through the wake at two downstream distances.

  4. 04

    Compare

    Computed drag both ways and explained why they disagreed.

Skills I used

Full engineering write-up

Worked with a team of four on this lab, and I measured how air moves around a brass cylinder and compared two independent drag estimates. The pressure result matched published behavior; the wake result did not, making measurement quality as important as the final number.

01

Test setup and method

One cylinder, two ways to measure drag

A 1.50 in brass cylinder was mounted perpendicular to the flow in the Cal Poly mechanical engineering wind tunnel. After locating the stagnation point, the team recorded surface pressure in 10-degree increments from 0 to 180 degrees.

A Pitot-static probe on an x-y traverse then sampled the wake at 17.5 in and 25.0 in downstream. Ambient conditions and free-stream dynamic pressure established air density, velocity, and a cylinder Reynolds number of 3.49 × 104.

1.50 inBrass cylinder diameter
13.75 m/sCalculated free-stream velocity
3.49 × 104Diameter-based Reynolds number
02

Surface pressure

The expected signature of separation

The stagnation point produced the largest pressure coefficient, Cp = 1.03. Pressure fell as the flow accelerated around the cylinder, reached Cp = -1.54 near 70 degrees, and remained negative across the rear surface—a broad low-pressure region consistent with separated flow.

Line chart of pressure coefficient versus cylinder angle, falling from 1.03 at zero degrees to a minimum of negative 1.54 near seventy degrees
Nineteen surface measurements captured the high-pressure stagnation point, acceleration around the side, and separated rear region.
Interpretation: the nearly flat, negative pressure on the back side indicates that the boundary layer separated and left a wide turbulent wake rather than recovering to the ideal-flow pressure distribution.
03

Wake development

Velocity deficit and downstream recovery

Both wake surveys showed their lowest normalized velocity near the cylinder centerline and recovery toward free-stream velocity away from the wake. The profile farther downstream appeared broader and smoother, which is consistent with turbulent mixing.

Two normalized velocity profiles showing a central wake deficit at seventeen and a half and twenty-five inches downstream
Normalized velocity u/U plotted against normalized vertical position y/D for both traverse locations.
04

Drag comparison

A good result and a useful discrepancy

Numerically integrating the surface pressure distribution gave CD = 1.256, close to the expected value of approximately 1.2. Integrating the wake momentum deficit produced much lower values, so those results were treated as evidence of an incomplete or inconsistent wake survey—not as validated drag coefficients.

MethodLocation / sourceDrag coefficient, CDAssessment
Wake momentumx = 17.5 in0.179Underestimated
Wake momentumx = 25.0 in0.031Underestimated
Reference behaviorReD = 3.49 × 104≈ 1.2Expected range
Likely error sources: unsteady vortex shedding, probe misalignment, pressure-zero drift, an incomplete vertical integration range, and free-stream inconsistency. Several measured u/U values above 1 outside the wake support that diagnosis.
05

Engineering takeaway

Validate the method, not only the arithmetic

The experiment connected surface pressure, separation, wake formation, and pressure drag in one test. More importantly, comparing independent methods exposed a measurement problem that a single calculation would have hidden.

A stronger repeat test would re-zero the transducer before each traverse, verify probe alignment, extend the survey beyond the full velocity deficit, and repeat multiple passes to quantify the unsteadiness of the wake.