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ASTM D1941 – 21 establishes a standardized procedure for measuring the volumetric flow rate of water and wastewater in open channels using the Parshall flume. Issued under the fixed designation D1941, this test method falls under the jurisdiction of ASTM Committee D19 on Water. The flume itself is defined as the primary instrument, creating a specific hydrodynamic condition, while the secondary instrument measures the depth of flow at the appropriate location (Sections 3.2.5 and 3.2.7). All values in inch-pound units are regarded as standard.
Related methodologies for liquid flow measurement are found in ISO 1438 and ISO 4359, which address thin-plate weirs and various flume shapes, respectively.
Per Section 3.2.1, free flow is a condition where the flow rate is governed by the state of flow at the crest overfall. When operating under this regime, discharge is calculated from a single upstream head measurement. A hydraulic jump—an abrupt transition from supercritical to subcritical flow—frequently occurs downstream and confirms the free-flow regime (Section 3.2.3). The normal depth is defined as the uniform depth for a given flow rate in a long open channel of specific shape, roughness, and slope (Section 3.2.4).
The secondary instrument, such as a scow float mounted on a hinged cantilever, measures the head precisely at the flume crest. This setup aligns with the measurement standards detailed in ISO 4359:2013.
| 🟦 Term | 📏 Definition (D1941 – 21) | 🎯 Measurement Role |
|---|---|---|
| Free Flow | Flowrate governed by the state of flow at the crest overfall. | Enables discharge determination from a single upstream head measurement. |
| Head | The height of a liquid above a specified point (the flume crest). | Primary variable measured by the secondary instrument. |
| Hydraulic Jump | An abrupt transition from supercritical to subcritical flow. | Confirms the free flow regime downstream of the flume. |
This standard relies on several key ASTM documents: D1129 (Terminology Relating to Water) for general definitions, D2777 (Practice for Determination of Precision and Bias of Applicable Test Methods of Committee D19 on Water) for accuracy protocols, and D3858 (Test Method for Open-Channel Flow Measurement of Water by Velocity-Area Method) for alternative measurement approaches. Internationally, ISO 1438:2017 (thin-plate weirs) and ISO 4359:2013 (rectangular, trapezoidal, and U-shaped flumes) are referenced for broader context.
Strict adherence to the roles of the primary and secondary instruments is required. The secondary instrument must capture the depth accurately at the designated upstream location. Float mechanisms, ultrasonic sensors, or pressure transducers can serve this purpose provided they meet the precision requirements established in D2777.
🔍 What is the primary instrument in a Parshall flume system?
Per Section 3.2.5, the primary instrument is the Parshall flume itself. It creates the specific hydrodynamic condition that can be sensed by the secondary instrument.
💡 How is “head” defined for flow measurement in this standard?
Head is defined in Section 3.2.2 as the height of a liquid above a specified point, specifically the flume crest. This single upstream measurement defines the flow rate under free flow conditions.
⚡ What is the primary benefit of free flow conditions?
Free flow conditions allow the entire discharge to be determined from a single upstream head measurement, simplifying the instrumentation and data reduction required for accurate flow monitoring.
📌 What key ISO standards are specifically referenced by D1941?
The standard aligns with ISO 1438:2017 for thin-plate weirs and ISO 4359:2013 for rectangular, trapezoidal, and U-shaped flumes. ISO 555-2:1987 is also referenced for steady flow dilution methods.