Triangular V-notch weirs are a fundamental tool in hydraulic engineering, providing a cost-effective and reliable method for measuring flow in open channels. Accurate flow measurement is essential for managing water resources, monitoring the environment, and conducting hydraulic research.
These weirs operate on the principle that the flow rate is related to the opening angle of the V-shaped notch. To ensure precise and reliable measurements, calibration is necessary. This process establishes a quantitative relationship between the weir’s geometric parameters and the corresponding flow rates, compensating for variations in hydraulic conditions and notch geometry.
Theoretical and Empirical Discharge Equations
The theoretical discharge Qt over a triangular V-notch is given by:where:
- = head of water above the notch crest (m)
- = angle of the V-notch (degrees)
- = acceleration due to gravity (m/s²)
For a weir with a fixed angle, the termis constant.
The actual discharge Qa is related to the theoretical discharge by the coefficient of discharge Cd:Substituting Equation (1) gives the actual discharge as:By letting , the discharge equation simplifies to:where the theoretical value of the exponent n is 5/2.
Linearization and Determination of Constants
To determine the empirical constants K and n from experimental data, Equation (6) is linearized by taking the logarithm of both sides: Plotting logQa versus logH on log-log graph paper yields a straight line. From the graph, two points and are selected, yielding the equations:Subtracting Equation (8) from Equation (9) gives:Therefore, the exponent n is calculated as:After finding n, its value is substituted back into Equation (8) or (9) to solve for logK and thus K. Finally, the coefficient of discharge Cd is found using the relation:
