Organizational Principles of Hyporheic Exchange Flow and Biogeochemical Cycling in River Networks Across Scales

Krause, Stefan; Abbott, Benjamin W.; Baranov, Viktor; Bernal, Susana; Blaen, Phillip; Datry, Thibault; Drummond, Jennifer; Fleckenstein, Jan H.; Velez, Jesus Gomez; Hannah, David M.; Knapp, Julia A.; Kurz, Marie; Lewandowski, Jörg; Martí, Eugènia; Mendoza‐Lera, Clara; Milner, Alexander; Packman, Aaron; Pinay, Gilles; Ward, Adam S.; Zarnetzke, Jay P.

doi:10.1029/2021wr029771

Title: Organizational Principles of Hyporheic Exchange Flow and Biogeochemical Cycling in River Networks Across Scales

Journal Article · Fri Feb 11 00:00:00 EST 2022 · Water Resources Research

DOI:https://doi.org/10.1029/2021wr029771· OSTI ID:1854461

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^[8]; Kurz, Marie ^[9];

^[10]; Martí, Eugènia ^[11];

^[12]; Milner, Alexander ^[1];

^[13]; Pinay, Gilles ^[14];

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Univ. of Birmingham (United Kingdom)
Brigham Young Univ., Provo, UT (United States)
Ludwig Maximillian Univ., Munich (Germany)
Center for Advanced Studies of Blanes (Spain)
National Research Institute for Agriculture, Food and the Environment, Paris (France)
Helmholtz Center for Environmental Research, Leipzig (Germany)
Vanderbilt Univ., Nashville, TN (United States)
Durham Univ. (United Kingdom)
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
Leibniz‐Institute of Freshwater Ecology and Inland Fisheries, Berlin (Germany)
Center for Advanced Studies of Blanes Blanes Spain
Univ. of Koblenz‐Landau, Mainz (Germany)
Northwestern Univ., Evanston, IL (United States)
National Centre for Scientific Research, Paris (France)
Indiana Univ., Bloomington, IN (United States)
Michigan State Univ., East Lansing, MI (United States)

Hyporheic zones increase freshwater ecosystem resilience to hydrological extremes and global environmental change. However, current conceptualizations of hyporheic exchange, residence time distributions, and the associated biogeochemical cycling in streambed sediments do not always accurately explain the hydrological and biogeochemical complexity observed in streams and rivers. Specifically, existing conceptual models insufficiently represent the coupled transport and reactivity along groundwater and surface water flow paths, the role of autochthonous organic matter in streambed biogeochemical functioning, and the feedbacks between surface-subsurface ecological processes, both within and across spatial and temporal scales. While simplified approaches to these issues are justifiable and necessary for transferability, the exclusion of important hyporheic processes from our conceptualizations can lead to erroneous conclusions and inadequate understanding and management of interconnected surface water and groundwater environments. This is particularly true at the landscape scale, where the organizational principles of spatio-temporal dynamics of hyporheic exchange flow (HEF) and biogeochemical processes remain largely uncharacterized. This article seeks to identify the most important drivers and controls of HEF and biogeochemical cycling based on a comprehensive synthesis of findings from a wide range of river systems. We use these observations to test current paradigms and conceptual models, discussing the interactions of local-to-regional hydrological, geomorphological, and ecological controls of hyporheic zone functioning. This improved conceptualization of the landscape organizational principles of drivers of HEF and biogeochemical processes from reach to catchment scales will inform future river research directions and watershed management strategies.

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Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER); Leverhulme Trust International Network; HORIZON 2020-PEOPLE-2016-RISE; National Science Foundation (NSF)

Grant/Contract Number:: AC05-00OR22725; EAR-1734300; EAR-1652293; SC0019377

OSTI ID:: 1854461

Journal Information:: Water Resources Research, Vol. 58, Issue 3; ISSN 0043-1397

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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Linking in-stream nutrient uptake to hydrologic retention in two headwater streams Drummond, Jennifer D.; Bernal, Susana; von Schiller, Daniel Freshwater Science, Vol. 35, Issue 4 https://doi.org/10.1086/688599	journal	December 2016
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Development of Layered Sediment Structure and its Effects on Pore Water Transport and Hyporheic Exchange Packman, Aaron I.; Marion, Andrea; Zaramella, Mattia Water, Air, & Soil Pollution: Focus, Vol. 6, Issue 5-6 https://doi.org/10.1007/s11267-006-9057-y	journal	November 2006
Colmation and Depth Filtration within Streambeds: Retention of Particles in Hyporheic Interstices Brunke, Matthias International Review of Hydrobiology, Vol. 84, Issue 2 https://doi.org/10.1002/iroh.199900014	journal	January 1999
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Impact of Bed Form Celerity on Oxygen Dynamics in the Hyporheic Zone Wolke, Philipp; Teitelbaum, Yoni; Deng, Chao Water, Vol. 12, Issue 1 https://doi.org/10.3390/w12010062	journal	December 2019
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Less Fine Particle Retention in a Restored Versus Unrestored Urban Stream: Balance Between Hyporheic Exchange, Resuspension, and Immobilization Drummond, J. D.; Larsen, L. G.; González‐Pinzón, R. Journal of Geophysical Research: Biogeosciences, Vol. 123, Issue 4 https://doi.org/10.1029/2017JG004212	journal	April 2018
Physical Controls on Salmon Redd Site Selection in Restored Reaches of a Regulated, Gravel‐Bed River Harrison, Lee R.; Bray, Erin; Overstreet, Brandon Water Resources Research, Vol. 55, Issue 11 https://doi.org/10.1029/2018WR024428	journal	November 2019
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Trends and seasonality of river nutrients in agricultural catchments: 18 years of weekly citizen science in France Abbott, Benjamin W.; Moatar, Florentina; Gauthier, Olivier Science of The Total Environment, Vol. 624 https://doi.org/10.1016/j.scitotenv.2017.12.176	journal	May 2018
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In-stream geomorphic structures as drivers of hyporheic exchange: IN-STREAM STRUCTURES AND HYPORHEIC EXCHANGE Hester, Erich T.; Doyle, Martin W. Water Resources Research, Vol. 44, Issue 3 https://doi.org/10.1029/2006WR005810	journal	March 2008
The interplay between transport and reaction rates as controls on nitrate attenuation in permeable, streambed sediments: NITRATE REMOVAL IN PERMEABLE SEDIMENTS Lansdown, K.; Heppell, C. M.; Trimmer, M. Journal of Geophysical Research: Biogeosciences, Vol. 120, Issue 6 https://doi.org/10.1002/2014JG002874	journal	June 2015
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Natural attenuation of chlorinated ethenes in hyporheic zones: A review of key biogeochemical processes and in-situ transformation potential Weatherill, John J.; Atashgahi, Siavash; Schneidewind, Uwe Water Research, Vol. 128 https://doi.org/10.1016/j.watres.2017.10.059	journal	January 2018
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The functional significance of bioturbation and biodeposition on biogeochemical processes at the water–sediment interface in freshwater and marine ecosystems Mermillod-Blondin, Florian Journal of the North American Benthological Society, Vol. 30, Issue 3 https://doi.org/10.1899/10-121.1	journal	September 2011
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Effects of benthic and hyporheic reactive transport on breakthrough curves Aubeneau, Antoine F.; Drummond, Jennifer D.; Schumer, Rina Freshwater Science, Vol. 34, Issue 1 https://doi.org/10.1086/680037	journal	March 2015
Coupled 3-D stream flow and hyporheic flow model under varying stream and ambient groundwater flow conditions in a pool-riffle system: Coupled 3-D Stream Flow and Hyporheic Flow Model Trauth, Nico; Schmidt, Christian; Maier, Uli Water Resources Research, Vol. 49, Issue 9 https://doi.org/10.1002/wrcr.20442	journal	September 2013
Modeling hyporheic exchange with unsteady stream discharge and bedform dynamics: Unsteady Hyporheic Exchange with Moving Bed Forms Boano, Fulvio; Revelli, Roberto; Ridolfi, Luca Water Resources Research, Vol. 49, Issue 7 https://doi.org/10.1002/wrcr.20322	journal	July 2013

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