90° Triangular Sharp-Crested Weir Plate
Precision milled brass plate with 90° notch angle and 45° downstream beveled knife edge.
Calibrate a 90° V-notch sharp-crested weir in an open irrigation flume and evaluate the weir discharge coefficient C_d and proportionality constant C_w. Explore interactive farm machinery simulation, irrigation hydraulics, and agricultural engineering telemetry.
Ready to sample with H^2.5 = 0.021 m^2.5.
Adjust H^2.5, then execute agricultural trial.
Agricultural engineering telemetry and biosystems states are evaluated rigorously using 64-bit IEEE 754 precision. Residuals reflect ordinary least-squares regression across successive observations. Continuous data structures support high-fidelity agricultural and environmental modeling.
The 5/2 power law applies strictly for heads H > 0.05 m; below 5 cm, water surface tension and fluid viscosity dominate. Evaluated using a precision brass 90° V-notch plate mounted in a rectangular flume across water heads from 0.12 m to 0.28 m (H^2.5 from 0.005 to 0.045 m^2.5).
Precision milled brass plate with 90° notch angle and 45° downstream beveled knife edge.
Recirculating water flume with wave-damping baffles and upstream calming section.
Measures upstream water surface elevation H with 0.1 mm precision.
Captures discharged water over timed intervals to determine true benchmark flow rate Q.
Supplies ambient air beneath the falling nappe to prevent vacuum cling and calibration distortion.
Monitors flume inflow rate continuously for flow stability verification.
Calibrate a 90° V-notch sharp-crested weir in an open irrigation flume and evaluate the weir discharge coefficient C_d and proportionality constant C_w. Standardized parameter settings: 0.005, 0.013, 0.021, 0.029, 0.037, 0.045 m^2.5.
Fill the flume until water is exactly level with the vertex of the V-notch. Lower the vernier point gauge until its tip touches the meniscus at the notch vertex and record the zero datum reading H_0.
Place mesh calming baffles 3.0 meters upstream of the weir to dissipate surface waves and establish uniform approach velocity.
Start the supply pump to establish an upstream head H = 0.120 m (H^2.5 = 0.0050 m^2.5), verifying that the nappe springs clear of the crest and is fully aerated.
Divert the weir discharge into the gravimetric weigh tank for exactly 60.0 seconds, measuring collected mass to calculate volumetric flow rate Q (m³/s).
Systematically increase pump flow across five additional stages up to H = 0.280 m (H^2.5 = 0.0450 m^2.5), logging H and Q for each trial.
Plot measured discharge Q against H^2.5, perform linear regression through the origin, and determine the Thomson weir discharge coefficient C_w and C_d.
Points are your recorded observations. The solid regression line validates V-Notch Weir Calibration mathematical scaling.
| # | Head Raised to 2.5 Power H^2.5 (m^2.5) | Measured Weir Discharge Q (m³/s) | Head raised to 2.5 power H^2.5 (m^2.5) | Discharge Q (m³/s) | Remove |
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