Agricultural Engineering / Parshall Flume Calibration
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LABORATORY 14 · AGRICULTURAL ENGINEERING

Parshall Flume Calibration theory

Understand parshall flume calibration: governing agricultural mechanics, soil-water conservation equations, and post-harvest models.

Agricultural and physical foundations of Parshall Flume Calibration.

Accurate measurement of open-channel water discharge is essential for fair water allocation in irrigation districts, monitoring canal conveyance efficiency, and preventing canal bank overtopping. The Parshall flume, developed by Ralph L. Parshall, is a specialized self-cleaning Venturi-type open channel constriction widely recognized as the international standard for irrigation flow measurement. It features a converging contracting entrance section with a level floor, a contracted throat section with a downward-sloping floor, and a diverging expanding exit section with an upward-sloping floor. The drop in throat elevation induces critical depth and supercritical flow, establishing a unique relationship between the upstream water depth H_a (measured in a stilling well at two-thirds the length of the converging section) and discharge Q. In free-flow conditions, the rating equation follows a power law Q = C·H_a^n (or ln Q = n·ln H_a + ln C). When downstream tailwater rises such that the submergence ratio S = H_b / H_a exceeds the critical limit (0.60 for small flumes, 0.70 for medium flumes), flow transitions to submerged flow requiring a submergence correction. In this experiment, a calibrated flume is tested across multiple flow rates to extract n and C.

ln(Q) = n · ln(H_a) + ln(C) = 1.5500 · ln(H_a) + 0.3800

Viva voce questions & analytical theory

What are the primary operational advantages of a Parshall flume over a sharp-crested weir?

Parshall flumes have low head loss (about one-fourth that of a weir), high velocity through the throat that makes them self-cleaning (preventing sediment and debris accumulation), and the ability to operate under substantial submergence without losing calibration.

Explain the difference between free flow and submerged flow in a Parshall flume.

In free flow, critical velocity occurs in the throat, creating a hydraulic drop such that downstream tailwater has zero effect on the upstream head H_a (discharge depends solely on H_a). In submerged flow, high tailwater submerges the throat, causing backwater that elevates H_a and requires both H_a and H_b to compute discharge.

What is the critical submergence ratio for a 6-inch Parshall flume?

For throat widths between 6 inches and 9 inches, the critical submergence limit is S_c = H_b / H_a = 0.60 (60%). Below 60%, free-flow equations apply; above 60%, a submergence correction must be subtracted.

Where is the upstream head measurement location H_a located?

H_a is measured in a stilling well connected to a tap located on the side wall of the converging section at a distance equal to two-thirds of the converging section length upstream from the throat crest.

How does sediment deposition in the approach canal affect flume accuracy?

Sediment deposition upstream can distort the approach velocity profile and create excessive approach velocity, causing the flume to under-read discharge relative to standard calibration tables.

Why is the throat floor of a Parshall flume sloped downward?

The downward slope of the throat (slope 3:8) accelerates water rapidly through critical depth into supercritical flow, ensuring a stable, well-defined free-flow rating relation.

Experimental precautions and agricultural field safety

  • Verify that the flume crest floor is perfectly level across both lateral and longitudinal directions using a precision spirit level.
  • Ensure stilling well piezometer tubes are free of trapped air bubbles and sediment silt.
  • Maintain approach flow conditions smooth and symmetrical without surface waves or cross-currents.
  • Check that the flume operates under free-flow conditions (H_b / H_a < 0.60) during calibration runs.

Theoretical assumptions & biological limits

  • Flumes must be fabricated strictly to standardized ASTM/USBR dimensions; geometric scaling errors invalidate published discharge coefficients.
  • At very low heads (H_a < 0.03 m), surface tension and boundary layer viscosity distort the power-law exponent.
  • Submerged flow corrections introduce higher measurement uncertainty (±5%) compared to free-flow calibration (±2%).
  • High approach velocities (> 0.5 m/s) require baffle straighteners to prevent kinetic energy head distortion.
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Connect biosystems theory to empirical field data.

Evaluated using a standard 6-inch (15.2 cm) throat width Parshall flume in free-flow regime across upstream heads from 0.05 m to 0.40 m.