Award Abstract # 1632938
Qualitative Hydraulics and Transport from Strata and Dynamics of Sandy Bedforms

NSF Org: EAR
Division Of Earth Sciences
Recipient: UNIVERSITY OF WYOMING
Initial Amendment Date: June 22, 2016
Latest Amendment Date: June 22, 2016
Award Number: 1632938
Award Instrument: Standard Grant
Program Manager: Justin Lawrence
jlawrenc@nsf.gov
 (703)292-2425
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: August 1, 2016
End Date: July 31, 2020 (Estimated)
Total Intended Award Amount: $260,649.00
Total Awarded Amount to Date: $260,649.00
Funds Obligated to Date: FY 2016 = $260,649.00
History of Investigator:
  • Brandon McElroy (Principal Investigator)
    bmcelroy@uwyo.edu
Recipient Sponsored Research Office: University of Wyoming
1000 E UNIVERSITY AVE
LARAMIE
WY  US  82071-2000
(307)766-5320
Sponsor Congressional District: 00
Primary Place of Performance: University of Wyoming
WY  US  82071-2000
Primary Place of Performance
Congressional District:
00
Unique Entity Identifier (UEI): FDR5YF2K32X5
Parent UEI: FDR5YF2K32X5
NSF Program(s): Geomorphology & Land-use Dynam,
Sedimentary Geo & Paleobiology
Primary Program Source: 01001617DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 9150
Program Element Code(s): 745800, 745900
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Bed forms, ripples and dunes, are key indicators of water flow and sediment transport in sandy rivers, and therefore they are vital to understanding river management, coastal restoration, and surface water reservoir sedimentation. Additionally, they leave deposits that are a record of the ancient river conditions that create sedimentary rocks. These deposits can be used to determine the conditions of formation of subsurface reservoirs for water and hydrocarbons. To date, almost ubiquitously, models applied to bed form problems have used constant geometries representing bed forms that migrate to move sediment and create strata. This is in stark contrast to models of river processes that capture the dynamic nature of Earth's surface environments.

This project will test a set of hypotheses derived by applying a dynamic model of bed form behavior to problems in 1) sediment transport mechanics, 2) bed material sediment flux, and 3) generation of fluvial stratigraphy. This will be accomplished through a suite of laboratory experiments, and relationships developed in these experiments will then be applied to interpreting ancient fluvial strata. The results of this project will benefit modern river planning, subsurface reservoir modeling, understanding of Earth's natural history, and the applied problems associated with these topics.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

Note:  When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher. Some full text articles may not yet be available without a charge during the embargo (administrative interval).

Some links on this page may take you to non-federal websites. Their policies may differ from this site.

Ashley, Thomas C. and Naqshband, Suleyman and McElroy, Brandon "LowerStage Plane Bed Topography Is an Outcome of Rarefied, Intermittent Sediment Transport" Journal of Geophysical Research: Earth Surface , v.126 , 2021 https://doi.org/10.1029/2020JF005754 Citation Details
Mahon, Robert C. and McElroy, Brandon "Indirect estimation of bedload flux from modern sand-bed rivers and ancient fluvial strata" Geology , 2018 10.1130/G40161.1 Citation Details

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The focus of this project has been to develop quantitative understanding of rivers from their sedimentary deposits as related to conditions for moving sediment.

For Intellectual Merit, the project has been successful from the standpoint of not falsifying our three main hypotheses. We conclude that ripples and dunes in river are explicitly related to conditions within rivers and that they are also a quantitative predictor of the deposits that rivers leave behind. We developed models to estimate sand transport in rivers from a variety of data types. These models are likely to be used by a wide range of geologists, hydrologists, and engineers. The project partially supported two dissertations as well as 4 peer-reviewed manuscripts to-date. The dissemination of information learned has also occurred through a short course. This was offered once through the University of Wyoming, was canceled once along with its hosting conference in spring 2020, and will be offered again in the future.

For Broader Impact, the project supported at various times, a group 7 individuals that hav gone on to faculty and research science positions, advanced degrees, and other scholarly pursuits. It also contributed to the maintenance of experimental facilities at the University of Wyoming for studying rivers. The project was a major supporter of an art-science collaboration around patterns that used a miniature river tank to create ripples in a classroom to inspire art students to find and communicate about patterns in nature. Finally, the project has added to the curriculum at the University of Wyoming.


Last Modified: 09/29/2021
Modified by: Brandon Mcelroy

Please report errors in award information by writing to: awardsearch@nsf.gov.

Print this page

Back to Top of page