scholarly journals Linkage Between Dissolved Organic Matter Transformation, Bacterial Carbon Production, and Diversity in a Shallow Oligotrophic Aquifer: Results From Flow-Through Sediment Microcosm Experiments

2020 ◽  
Vol 11 ◽  
Author(s):  
Roland Hofmann ◽  
Jenny Uhl ◽  
Norbert Hertkorn ◽  
Christian Griebler
2017 ◽  
Vol 137 (1-2) ◽  
pp. 93-104 ◽  
Author(s):  
Eero Asmala ◽  
Lumi Haraguchi ◽  
Hans H. Jakobsen ◽  
Philippe Massicotte ◽  
Jacob Carstensen

Author(s):  
Piotr Zieliński ◽  
Elżbieta Jekatierynczuk-Rudczyk

Dissolved organic matter transformation in the hyporheic zone of a small lowland riverThe objective of this study was to examine dissolved organic carbon (DOC) concentration and specific ultraviolet absorbance (SUVA) changes in porewaters that occur over a small scale (cm) in the hyporheic zone (HZ) of a lowland stream in the Knyszynska Forest in northeast Poland. Hyporheic zone porewaters were sampled at different depths of 10, 30, 50, 70 cm at two study sites with different sediment material. The results showed significant differences in DOC concentrations between the upper and lower stream HZ. The current results indicate that small lowland sediments provide both a source and a sink of DOC for stream water, depending on the river course. The higher DOC level observed in the hyporheic zone suggests that porewater can be an autonomic site of biogeochemical changes of dissolved organic matter, which is very clear in the SUVA fluctuations.


2013 ◽  
Vol 32 (3) ◽  
pp. 821-836 ◽  
Author(s):  
Ryan M. Burrows ◽  
Jason B. Fellman ◽  
Regina H. Magierowski ◽  
Leon A. Barmuta

2017 ◽  
Vol 51 (8) ◽  
pp. 4328-4337 ◽  
Author(s):  
Runa Antony ◽  
Amanda S. Willoughby ◽  
Amanda M. Grannas ◽  
Victoria Catanzano ◽  
Rachel L. Sleighter ◽  
...  

2018 ◽  
Vol 4 (6) ◽  
pp. 806-819 ◽  
Author(s):  
Céline Jacquin ◽  
Mathias Monnot ◽  
Razina Hamza ◽  
Yahaut Kouadio ◽  
François Zaviska ◽  
...  

MBR instabilities during urinary nitrogen stabilization could be identified and explained using 3DEEM.


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