Oxic and suboxic zones along hyporheic flow paths contribute to the attenuation of trace organic contaminants, as revealed by suspect screening - Data repository Data storage for the publication "Oxic and suboxic zones along hyporheic flow paths contribute to the attenuation of trace organic contaminants, as revealed by suspect screening". Data obtained in the side channel of the River Erpe (Neuenhagener Mühlenfließ): location 52.476437 N, 13.625765 E

 

CSV stored here contains the intensities of 130 trace organic contaminants that fulfil the quality criteria (as described in manuscript: detection in at least 8 of 10 quality control samples, small signal drift in quality control samples, modi with less signal drift if detected in both ionization modi). CSV contains pore water (flow paths 1-3) and surface water (SW) measurements. Intensities are blank corrected and corrected by isotope-labelled internal standard (if available). 0 = below LOQ (peak area < standard deviation of QC samples), NA = not detected.

 

For experimental setup, see 

- publication: Reith, C. J., Spahr, S., Putschew, A., & Lewandowski, J. (2023). Attenuation of trace organic compounds along hyporheic flow paths in a lowland sandbed stream. Journal of Hydrology, 624, 129905. https://doi.org/10.1016/j.jhydrol.2023.129905

- data repository to Reith et al. (2023): Attenuation of trace organic compounds along hyporheic flow paths in a lowland sandbed stream - data from "Rechter Randgraben". IGB Leibniz-Institute of Freshwater Ecology and Inland Fisheries. dataset. https://doi.org/10.18728/igb-fred-902.2

]]> Rechter Randgraben 13.625 52.476 Christoph J. Reith 0009-0000-6865-026X Jörg Lewandowski