N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic...
Transcript of N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic...
![Page 1: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/1.jpg)
Slide 1
Redox gradients in natural & technical systems: Population structure and
physiological properties (H4)
Integral modelling approach for flow and reactive transport at surface
water-groundwater interfaces (N7+H2)
Retention of trace organics in urban hyporheic bioreactors (H1)
Abiotic transformation of organic trace compounds (H3)
Schaper et al. (2018), Water Research 140, 158-166
Broecker et al. (2018), Limnologia 68, 46-68
El-Athman et al. (2018), Environmental Science & Technology, submitted
oxygen freereducedspezies e.g. deiodinated compoundsreduced
e-shuttle
oxidizedspezies
e.g. iodinated compouds
splitting off I
I I
R
R RFe Mn S
corrinoids,humic-, fulvic acids quinones, porhyrins
oxidizede-shuttle
Common topic: Interface urban hyporheic zones
![Page 2: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/2.jpg)
Slide 2
• Attenuation of trace organics (TrOCs) is more efficient in hyporheic zone than surface water
• DOM composition and c(TrOCs) correlate in hyporheic zone, not in surface water
• Lower c(TrOCs) and removal efficiency in summer than in winter
H1: BirgitField sampling campaigns at River Erpe
Results so far:
Overall aim: Keeping/restoring intact hyporheic zone important for attenuation of TrOCs
Seasonality needs to be considered for analyzing whole year removal of TrOCs
![Page 3: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/3.jpg)
Slide 3
H2 + N7: Vahid and TabeaIntegral model for groundwater-surface water interactions
Overall aim: To better understand prevailing flow and transport processes in the interface domain including the exchange processes between the compartments using high resolution simulation
To further develop an integral solver and apply it to cases where interfacial exchanges are crucial (e.g. HZ, coastal engineering) after careful validation using experimental data
To provide new modelling capabilities for questions with combined free and porous media flow as an alternative to coupling of models
![Page 4: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/4.jpg)
Slide 4
• Flow processes in and around chironomid burrow (H2) collaboration with Lewandowski (H1), Nützmann (N6)
H2: VahidIntegral model for groundwater-surface water interactions
Research:
![Page 5: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/5.jpg)
Slide 5
• Flow and transport processes at rippled streambeds (N7) collaboration with Nützmann (N6), Lewandowski (H1)
N7: TabeaIntegral model for groundwater-surface water interactions
Research:
![Page 6: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/6.jpg)
Slide 6
• deiodination under anoxic/anaerobic conditions• the number of cleaved iodine atoms defines the
further behaviour of the TPs e.g. different aerobic biological transformation pathways and sorption to soil, which is also effected by the soil composition (%C-Org, %Clay content)
H3: YukiTransformation and behaviour of iodinated compounds during bank filtration
Results so far:
Overall aim: prediction of contaminant and TPs fate during infiltration (e.g. bank filtration, HZ)
TPs characterization concerning adsorption by soil and during subsequent drinking water treatment
Hypothetical further IOP TP pathway
![Page 7: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/7.jpg)
Slide 7
• Bacterial community in lab-based bioreactors with sediment from hyporheic zone able to transform iopromide under controlled conditions
• Mono-, di- and tri- deiodinated transformation products of the tri-iodinated Iopromide have been detected in outflow suggesting anaerobic microbial transformations
• The transformation of iopromide was shown to be dependent on concentration of organic carbon source suggesting a co-metabolic process
H4: NiranjanRedox gradients in urban water systems: population structure and physiological properties
Results so far:
Overall aim: Exploring the microbial transformation of iopromide by gradient biofilms in lab-scale sediment reactors
![Page 8: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/8.jpg)
Slide 8
Which measurements are conducted where and when?
Surface and pore water (25 cm depth or profiles): Vast sampling campaigns in Sept-Oct 2018, Jan-Feb 2019
and Jul-Aug 2019 19 TrOCs, DOM composition, major cations & anions,
oxygen, temperature, water level, discharge, electric conductivity
Birgit @ Erpe side channel
Yuki @ Lake Tegel & Treatment plant RuhlebenCore samples of 30-40 m depth (Oct 2018): Adsorption tests with ICM Organic content, CNS, XRD, grain size distribution, pHFilter sand of waterworks Tegel (Nov 2019): Batch and column tests with ICMActivated sludge (Apr 2019) Zahn-Wellens-test with ICM
Niranjan @ Erpe side channelSediment samples from the hyporheic zone, 30-40cm (Mar&Apr 2019): Column tests with iopromide
![Page 9: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/9.jpg)
Slide 9
KEY PROCESSESWATER BALANCE
COMPONENT
WHO USED MODEL
Surface runoff H2+N7 OpenFOAM
Infiltration H2+N7 OpenFOAM
Groundwater recharge H2+N7 OpenFOAM
Contaminations H2+N7 OpenFOAM
Which models are used to represent which water balance component?
![Page 10: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/10.jpg)
Slide 10
Collaborations within HZ group (without first supervisors)
Field workLab analysisShared dataModellingPublication
123
123 123
123
123123
123
123
![Page 11: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/11.jpg)
Slide 11
What we offer!• Help with sample analysis (major cations & anions, trace organic contaminants,
DOC, SAK)• Microbial community analysis (sequencing, photometry, flow cytometry, light-,
fluorescence- and confocal laser scanning microscopy, fluorescence in-situhybridisation, quantitative real time polymerase chain reaction (qPCR))
• Oxygen, temperature, electric conductivity measurement • OpenFOAM introduction, Integral flow and transport model for ground- and
surface water (high resolutions results for pressure distributions, flow paths, tracer concentrations)
• Field work devices and advice
![Page 12: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/12.jpg)
Slide 12
What we need!• Field data for model validation: Flow and transport processes at the
groundwater-surface water interface (including porosities, grain sizes, velocities, tracer concentrations, water levels)
• Iodide/iodine species detection in the range of ng/L to lower µg/L• Heavy/Transition Metal Analysis• Dissolved Oxygen Measurements• Anion analysis DOC measurements
![Page 13: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/13.jpg)
Slide 13
Where can we cooperate better?
• Share more data and publish together• Sharing results
• H3 and H4 collaborate on overlapping points
![Page 14: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/14.jpg)
Slide 14
Common Publications, ConferencesRealized publications:• Broecker, T., Teuber, K., Sobhi Gollo, V., Nützmann, G., Lewandowski, J. & Hinkelmann, R. (2019).
Integral Flow Modelling Approach for Surface Water-Groundwater Interactions along a RippledStreambed. Water, 11(7), 1517.
• Lewandowski, J., Arnon, S., Banks, E., Batelaan, O., Betterle, A., Broecker, T., Coll, C., Drummond, J.D., Gaona Garcia, J., Galloway, J., Gomez-Velez, J., Grabowski, R.C., Herzog, S.P., Hinkelmann, R., Höhne, A., Hollender, J., Horn, M.A., Jaeger, A., Krause, S., Löchner Prats, A., Magliozzi, C., Meinikmann, K., Mojarrad, B.B., Mueller, B.M., Peralta-Maraver, I., Popp, A.L., Posselt, M., Putschew, A., Radke, M., Raza, M., Riml, J., Robertson, A., Rutere, C., Schaper, J.L., Schirmer, M., Schulz, H., Shanafield, M., Singh, T., Ward, A.S., Wolke, P., Wörman, A. & Wu, L. (2019). Is theHyporheic Zone Relevant beyond the Scientific Community? Water, 11(11), 2230
• Sobhi Gollo, V., Broecker, T., Lewandowski, J., Nützmann, G. & Hinkelmann, R. (2019). Comparisonof an integral solver to coupled modelling approach for hydraulic exchange at surface water-groundwater interface along rippled streambed, EGU General Assembly, Vienna, Austria.
![Page 15: N7+H2 H4 ( ) · N7+H2) Retention of trace organics in urban hyporheic bioreactors (H1) Abiotic transformation of organic trace compounds (H3) Schaper et al. (2018), Water Research](https://reader033.fdocuments.net/reader033/viewer/2022052021/603573df4fc018719c4c639a/html5/thumbnails/15.jpg)
Slide 15
Planned publications:• Augustyniak, A., Sikora, P., Grygorcewicz, B., Despot, D., Braun, B., Szewzyk, U.,
Barjenbruch, M., Stephan, D. (in preparation, planned submission July 2020). Biofilms in the gravity sewer interfaces – making a friend from a foe.
• Broecker, T., Sobhi Gollo, V., Fox, A., Lewandowski, J., Nützmann, G. & Hinkelmann, R. Integral, high resolution transport modelling approach for surface water-groundwater interaction (planned submission to Water Resources Research 2020).
• Mueller, B. M., Schulz, H., Putschew A., Danczak, R. E., Lewandowski, J. (planned for 2020). Attenuation of trace organic compounds and dissolved organic matter in the surface water and the hyporheic zone of a lowland river.
• Sobhi Gollo, V., Broecker, T., Lewandowski, J., Nützmann, G. & Hinkelmann, R. Integral modeling of flow in and around a ventilated U-shaped chironomid burrow (planned submission to Water Resources Research 2020).
• Sorgler, Y., Schaper, J., Kerl, C., Putschew, A., Planer-Friedrich, B. (in preparation, planned submission August 2020). Fate and transformation of iodinated compounds in the hyporheic zone.
• UWI conference