Sediment incubation flux data of reservoir sediment cores

DOI
  1. Fred is the total O2 required per area to oxidize all reduced compounds released by the sediment was calculated according to Steinsberger et al. (2017): Steinsberger T, Schmid M, Wüest A, Schwefel R, Wehrli B, Müller B (2017) Organic carbon mass accumulation rate regulates the flux of reduced substances from the sediments of deep lakes. Biogeosciences, 14, 3275-3285.2. LOI and Water content values refer to a weighted mean of 3 sediment layers; 0-1, 1-3, and 3-5 cm.3. pH value refer to mean pH value of the overlying water in the sediment cores during the sediment incubation period.4. na refers to data. (print version)5. TC, TOC, TN and TFe in the sediment was measured once at each site in the upper 5 cm sediment layer.
Identifier
DOI https://doi.pangaea.de/10.1594/PANGAEA.928565
Related Identifier https://doi.pangaea.de/10.1594/PANGAEA.928570
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.928565
Provenance
Creator Dadi, Tallent; Friese, Kurt; Wendt-Potthoff, Katrin; Marcé, Rafael; Koschorreck, Matthias
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 2021
Rights Data access is restricted (moratorium, sensitive data, license constraints)
OpenAccess false
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 3590 data points
Discipline Earth System Research
Spatial Coverage (2.389W, 41.972S, 14.465E, 51.736N); Germany; Saxony-Anhalt, Germany; Catalonia, Spain
Temporal Coverage Begin 2013-04-29T00:00:00Z
Temporal Coverage End 2015-10-13T00:00:00Z