Abstract

Despite limitations in reproducing complex bedload sediment transport processes in rivers, formulas have been preferred over collection and analysis of field data due to the high cost and time-consuming nature of bedload discharge measurements. However, the performance of such formulas depends on the hydraulic and sedimentological conditions they attempt to describe. The availability of field measurements provides a unique opportunity to test bedload transport formulas to better guide formula selection. Hydraulic parameters and bedload discharge data from the Lower Minnesota River and two of its tributaries were used to evaluate nine bedload transport formulas using three different indices. The bedload data for the different sites were collected by the United States Geological Survey (USGS) from 2011 through 2014, with bed material varying from very coarse to medium sand. The formulas calculated higher bedload rates than were measured due to a combination of site-specific physical characteristics, including the presence of bed forms (dunes), and sampling uncertainties. Because of the lack of reproducibility of the tested formulas, five power functions, based on the relation between the specific unit power (independent hydraulic variable) and the USGS measured data (dependent variable), were derived as provisional equations to estimate the bedload discharge on the Lower Minnesota River and tributaries.

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Data Availability Statement

All data used during the study are available in a repository online in accordance with funder data retention policies (https://doi.org/10.3133/sir20165174).

Acknowledgments

The authors acknowledge CNPq-Brazil for their financial support to Elisa Armijos (Post-Doctoral Grant project number 405759/2015) and extend deep gratitude to Peter R. Wright (USGS-Wyoming-Montana Water Science Center) and Faith A. Fitzpatrick (USGS-Upper Midwest Water Science Center) for their valuable contributions to improving this article. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the US Government.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 26Issue 7July 2021

History

Received: Aug 31, 2020
Accepted: Mar 16, 2021
Published online: Apr 26, 2021
Published in print: Jul 1, 2021
Discussion open until: Sep 26, 2021

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Hydrologist, Dept. of Atmospheric Sciences and Hydrosphere, Instituto Geofísico del Perú, 169 Badajoz, Lima 15023, Perú. ORCID: https://orcid.org/0000-0003-4839-6924. Email: [email protected]
Gustavo H. Merten, Ph.D., Aff.M.ASCE [email protected]
Assistant Professor, Dept. of Civil Engineering, Univ. of Minnesota Duluth, 1405 University Dr., Duluth, MN 55812 (corresponding author). Email: [email protected]; [email protected]
Hydrologist, Upper Midwest Water Science Center, United States Geological Survey, 2280 Woodale Dr., Mounds View, MN 55112. ORCID: https://orcid.org/0000-0002-0441-8442. Email: [email protected]
Christopher A. Ellison [email protected]
Supervisory Hydrologist, Wyoming-Montana Water Science Center, United States Geological Survey, 3162 Bozeman Ave., Helena, MT 59601. Email: [email protected]
Luke U. Lisiecki [email protected]
Undergraduate Student, Dept. of Civil Engineering, Univ. of Minnesota Duluth, 1405 University Dr., Duluth, MN 55812. Email: [email protected]

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