Maximum respiration rates in hyporheic zone sediments are primarily constrained by organic carbon concentration and secondarily by organic matter chemistry

<p>River corridors are fundamental components of the Earth system, and their biogeochemistry can be heavily influenced by processes in subsurface zones immediately below the riverbed, referred to as the hyporheic zone. Within the hyporheic zone, organic matter (OM) fuels microbial respiration,...

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Bibliographic Details
Main Authors: J. C. Stegen, V. A. Garayburu-Caruso, R. E. Danczak, A. E. Goldman, L. Renteria, J. M. Torgeson, J. Hager
Format: Article
Language:English
Published: Copernicus Publications 2023-07-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/20/2857/2023/bg-20-2857-2023.pdf