Is the Hyporheic Zone Relevant beyond the Scientific Community?

Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic zone is a ubiquitous, reactive interface between the main channel and its surrounding sediments along the river network. We elaborate on the main physical, biological, and biogeochemical drivers and processes with...

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Main Authors: Jörg Lewandowski, Shai Arnon, Eddie Banks, Okke Batelaan, Andrea Betterle, Tabea Broecker, Claudia Coll, Jennifer D. Drummond, Jaime Gaona Garcia, Jason Galloway, Jesus Gomez-Velez, Robert C. Grabowski, Skuyler P. Herzog, Reinhard Hinkelmann, Anja Höhne, Juliane Hollender, Marcus A. Horn, Anna Jaeger, Stefan Krause, Adrian Löchner Prats, Chiara Magliozzi, Karin Meinikmann, Brian Babak Mojarrad, Birgit Maria Mueller, Ignacio Peralta-Maraver, Andrea L. Popp, Malte Posselt, Anke Putschew, Michael Radke, Muhammad Raza, Joakim Riml, Anne Robertson, Cyrus Rutere, Jonas L. Schaper, Mario Schirmer, Hanna Schulz, Margaret Shanafield, Tanu Singh, Adam S. Ward, Philipp Wolke, Anders Wörman, Liwen Wu
פורמט: Artigo
שפה:Inglês
יצא לאור: MDPI AG 2019-10-01
סדרה:Water
נושאים:
hyporheic zone
hyporheic exchange flow
surface water–groundwater exchange
ecosystem services
nutrient turnover
refuge
hyporheos
removal of trace organic compounds
emerging pollutants
self-purification capacity
גישה מקוונת:https://www.mdpi.com/2073-4441/11/11/2230
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