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Data for: A novel and enhanced calibration of the tilting weir as a flow measurement structure

Cite this dataset

Pugh, Joseph E. et al. (2023). Data for: A novel and enhanced calibration of the tilting weir as a flow measurement structure [Dataset]. Dryad. https://doi.org/10.5061/dryad.xksn02vn4

Abstract

To achieve reliable and equitable water distribution it is necessary to accurately estimate the volumetric discharge of water flow through rivers and canals. One such method of accomplishing this is by using hydraulic structures, such as the tilting weir. This structure not only can be used to measure the discharge of water on a continuous basis, but also allows for regulating the water level upstream of the structure. Presently, tilting weirs are often used to control water levels, but the literature on their utilization as flow measurement structures has remained sparse. This study presents a thorough analysis of laboratory experiments on scaled models of tilting weirs, where the flow depth upstream of the structure (i.e., head) and the inclination angle are used to calibrate an equation to estimate the discharge to a high degree of accuracy. Operational guidelines to ensure minimum uncertainty in measurement are also given.

The data published here include head and discharge measurements for all experiments conducted, including information on the experimental location, date, and model dimensions. Publication of this data is intended to allow other researchers to verify the calibration procedure laid out in the primary article, and as a comparative dataset for future calibrations.

README: DATA FOR: A NOVEL AND ENHANCED CALIBRATION OF THE TILTING WEIR AS A FLOW MEASUREMENT STRUCTURE

https://doi.org/10.5061/dryad.xksn02vn4

The data published include head and discharge measurements for all experiments conducted, including information on the experimental location, date, and model dimensions.

Description of the data and file structure

Data are comma delineated with the first row indicating header names. Total number of observations is 440.
Q (m^3/s) = Steady discharge in cubic meters per second, recorded at an accuracy of +/- 0.0003 m^3/s
h (m) = Water surface elevation in meters measured 0.8 m upstream of crest location, taken relative to the crest elevation, p. Accuracy +/- 0.001 m.
theta (degrees) = Angle of inclination of weir plate with respect to the horizontal channel bed. In degrees.
p (m) = Elevation of weir crest above the horizontal channel bed. In meters.
b (m) = The length of the weir crest in the transversal direction. In meters.
Experiment = Refers to experimental code given in Table 1 of published article.
Date = Date of experimentation
Location = Facility where experimentation was completed.
EFML = Environmental Fluid Mechanics Laboratory at Colorado State University
HHLab = Hydrology and Hydromorphology Laboratory at the Lyon-Villeurbanne Centre Recherche, INRAE, France

Funding

Colorado Agricultural Experiment Station, Award: COL00424

Embassy of France in Washington, D.C