Unifying Advective and Diffusive Descriptions of Bedform Pumping in the Benthic Biolayer of Streams-Reference-Cited by-同舟云学术

Unifying Advective and Diffusive Descriptions of Bedform Pumping in the Benthic Biolayer of Streams

Published:2020-10-27 Issue:11 Volume:56 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Grant Stanley B.¹²^ORCID,Monofy Ahmed³^ORCID,Boano Fulvio³^ORCID,Gomez‐Velez Jesus D.⁴^ORCID,Guymer Ian⁵^ORCID,Harvey Judson⁶^ORCID,Ghisalberti Marco⁷^ORCID

Affiliation:

1. Occoquan Watershed Monitoring Laboratory, The Charles E. Via Jr. Department of Civil and Environmental Engineering Virginia Tech Manassas VA USA

2. Center for Coastal Studies Virginia Tech Blacksburg VA USA

3. Department of Environment, Land and Infrastructure Engineering Politecnico di Torino Torino Italy

4. Department of Civil and Environmental Engineering Vanderbilt University Nashville TN USA

5. Department of Civil and Structural Engineering, Sir Frederick Mappin Building University of Sheffield Sheffield UK

6. U.S. Geological Survey, Earth System Processes Division Reston VA USA

7. Oceans Graduate School University of Western Australia Perth Western Australia Australia

Funder

Compagnia di San Paolo

Pacific Northwest National Laboratory

Directorate for Engineering

Directorate for Geosciences

UK National Ion Beam Centre

U.S. Geological Survey

Virginia Polytechnic Institute and State University

Australian Respiratory Council

Office of the President, University of California

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020WR027967

Reference63 articles.

1. Ambient groundwater flow diminishes nitrate processing in the hyporheic zone of streams

2. Bedforms as Biocatalytic Filters: A Pumping and Streamline Segregation Model for Nitrate Removal in Permeable Sediments

3. Hyporheic flow and transport processes: Mechanisms, models, and biogeochemical implications

4. Reduction of the hyporheic zone volume due to the stream-aquifer interaction

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