A New Equation of Mean Velocity in Flow, Its Verification and Consequences: H.B. Fischer’s Experiment in the Caltech Canal

The Chezy-Manning equation has long been the macroscopic description of flow in real channels, and its foundation is the balance of Newtonian mechanical forces. This Article presents the development and verification of a new equation of average velocity in the flow, defined this time in terms of electric forces (Van der Waals), having the same structure as the classical equation. Its application can be very broad, since in addition to having a new and powerful theoretical tool, in engineering practice it allows reducing the degree of uncertainty in the measurement of natural channels. The validity of the Elder equation, which links hydraulics and Dispersion, is analyzed here and an adjustment to its application is proposed, considering the Longitudinal Transport Coefficient as a function of time.

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Publication Details

Journal
EARTH SCIENCES AND HUMAN CONSTRUCTIONS
Published
2024-10-17
DOI
https://doi.org/10.37394/232024.2024.4.10
Primary Topic
Fluid Dynamics and Turbulent Flows
Type
article
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article

A New Equation of Mean Velocity in Flow, Its Verification and Consequences: H.B. Fischer’s Experiment in the Caltech Canal

Alfredo José Constaín Aragón
EARTH SCIENCES AND HUMAN CONSTRUCTIONS
Fluid Dynamics and Turbulent Flows
article

A New Equation of Mean Velocity in Flow, Its Verification and Consequences: H.B. Fischer’s Experiment in the Caltech Canal

Alfredo José Constaín Aragón
article en

Abstract

The Chezy-Manning equation has long been the macroscopic description of flow in real channels, and its foundation is the balance of Newtonian mechanical forces. This Article presents the development and verification of a new equation of average velocity in the flow, defined this time in terms of electric forces (Van der Waals), having the same structure as the classical equation. Its application can be very broad, since in addition to having a new and powerful theoretical tool, in engineering practice it allows reducing the degree of uncertainty in the measurement of natural channels. The validity of the Elder equation, which links hydraulics and Dispersion, is analyzed here and an adjustment to its application is proposed, considering the Longitudinal Transport Coefficient as a function of time.

EARTH SCIENCES AND HUMAN CONSTRUCTIONSVol. 4
Openalex Percentile: Top 80%
Fluid Dynamics and Turbulent Flows
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A New Equation of Mean Velocity in Flow, Its Verification and Consequences: H.B. Fischer’s Experiment in the Caltech Canal — Alfredo José Constaín Aragón · EARTH SCIENCES AND HUMAN CONSTRUCTIONS (2024) | TGRS Research Map | TGRS