enigma itn coordination presentation · this project has received funding from european...
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ENIGMA ITNCoordination presentation
Damien Jougnot (Deputy Coordinator)
Coordination team: Philippe Davy (Coordinator), Tanguy Le Borgne, and Patricia Gautier
Cluster event « Clean Water »
Girona, 22.10.2019
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Why ENIGMA ITN ?
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Policy making in hydrology has crucial needs for information to constrainhydrological models of the critical zone.
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Why ENIGMA ITN ?
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Policy making in hydrology has crucial needs for information to constrainhydrological models of the critical zone.
Hydrologists usually have sparse and punctual information (boreholes, sensors)…
…and sometimes none !
Hydrogeophysics: “use of advanced geophysical methods to understand the interaction between geology and fluid flow in the subsurface”
Hubbard and Rubbin (2002)
Measured geophysical
property
Hydrological parameter or
structure/contrasts
Petrophysics – Inversion
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This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Hydrosystems are multi-scalesystems
Why ENIGMA ?
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This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
A tool for each scale of interest:we focus on the cm km scales…
Geophysical tools:• non-intrusive• fast and « cheap »• sensitive to parameters of interests• …but indirect measurement and
decreasing resolution with distance
Why ENIGMA ?
Hydrosystems are multi-scalesystems
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Why ENIGMA ?
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
« Picture » of static properties(porosity, water content, permeability…)
Classically (2D – 3D)
Map
2D or 3D Imaging
How to adapt subsurface imaging strategies to the processes of interest ?
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Why ENIGMA ?
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
« Picture » of static properties(porosity, water content, permeability…)
« Movie » of dynamic processes(flux, biogeochemical reactions…)
Classically (2D – 3D) In development (4D)
Map
2D or 3D Imaging
Time-lapse cross-hole
The critical zone is very dynamic !
How to adapt subsurface imaging strategies to the processes of interest ?
Originality of the project: fostering a shift from staticstructure characterizationto dynamic process imaging
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Why ENIGMA ?
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
ENIGMA ITN (from 2017 to 2021)
European training Network for In situ imaGing of dynaMic processes in heterogeneous subsurfAce environments
..from the lab to the field
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This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
The Consortium
11Beneficiaries
10Partners
15ESR
8Countries
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This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Field InfrastructuresField infrastructures Unique attributes
TERENO- Krauthausen (FZJ),Hermalle (ULG),Lauswiesen (TU),H+ Poitiers (CNRS)
Hydrogeophysical test siteswith high borehole densityand large hydrogeophysicaldatabases
H+ Ploemeur (CNRS)H+ Hyderabad (BRGM)Aspo Hard Rock Laboratory
(SKB)
Fractured rockobservatories for long termmonitoring and in situexperiments
TERENO- Selke (UFZ)HOBE obs. (UCPH)Emme (UNINE)
Nested observatories inhighly instrumentedcatchments
Llobregat-Argentona (CSIC)H+ Mallorca (CNRS)
Salt water intrusionmonitoring andexperimentation
H+ Larzac (UM)H+ Low Noise Lab. (CNRS)
Unsaturated zoneobservatories for long termmonitoring and in situexperiments
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ESR7 : Joel Tirado Conde
ESR2 : Guilherme Nogueira
ESR13 : Veronika Rieckh
ESR10 : Peleg HaruziESR12 : Satoshi Izumoto
ESR11: Richard Hoffmann
ESR15: Jorge Lopez Alvis
ESR5 : Lara Blazevic
ESR6 : Behzad Pouladi
ESR8 : Anne-Karin Cooke
ESR3 : Alvaro Pardo Alvarez
ESR9 : Alejandro Fernandez Visentini
ESR4 : Justine Molron
ESR1 : Kevin De VriendtESR14: Andrea Palacios
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
The Early Stage Reseachers
15 ESRs:5 women & 10 men
Surname
NamePosition Start Nationality
Richard
HoffmannESR11 02/05/2017 German
Joel Tirado
CondeESR07 01/05/2017 Spanish
Jorge Lopez
AlvisESR15 01/06/2017 Mexican
Veronika
RieckhESR13 01/07/2017 Austrian
Satoshi
IzumotoESR12 01/07/2017 Japanese
Peleg Haruzi ESR10 01/08/2017 Israeli
Anne-Karin
CookeESR08 28/08/2017 German/ British
Alejandro
Fernandez
Visentini
ESR09 01/09/2017Argentinian/
Spanish
Justine Molron ESR04 04/09/2017 Belgian
Álvaro Pardo
ÁlvarezESR3 01/10/2017 Spanish
Guilherme
NogueiraESR02 03/11/2017 Brazilian
Andrea
PalaciosESR14 01/10/2017 Venezuelian
Lara Blazevic ESR05 01/09/2017Croatian/
Venezuelan
Behzad
PouladiESR6 01/12/2017 Irani
Kevin de
Vriendt ESR01 16/12/2017 Belgium
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WP2: Explore coupled dynamic processes in targeted highly instrumented sites
ESR1 Kevin De Vriendt
Mixing and chemical reaction hotspots in saline-freshwater mixing zones
ESR2 : Guilherme Nogueira
Flow and reactions in stream-riparian zone systems”.
ESR3 : Álvaro Pardo-Álvarez
Closing the conceptual gap between the hyporheic zone and the river corridor
ESR4 : Justine Molron
Flow and transport in fracture networks
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WP3: Quantify temporal changes in subsurface water content and fluxes distributions
ESR5 : Lara Blazevic
Monitoring spatio-temporal water redistribution in the subsurface
ESR6 : Behzad Pouladi
Active Fiber-Optic DTS methods to monitor subsurface flow dynamics
ESR7 : Joel Tirado Conde
Multi-scale thermal imaging of groundwater upwelling in stream valleys
ESR8 : Anne-Karin Cooke
Monitoring water storage changes with a new portable absolute quantum gravimeter
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WP4: Create new methods for tracking the transport and reactivity of chemical species in subsurface
ESR9 : Alejandro Fernandez Visentini
Geophysical signatures of spreading and mixing.
ESR10 : Peleg Haruzi
High resolution imaging of transport processes with GPR full-waveform inversion
ESR11 : Richard Hoffmann
Joint heat and solute tracer test inversion for imaging preferential pathways
ESR12 : Satoshi Izumoto
Spectral induced polarization monitoring for in-situ quantification of biochemical reactions
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WP4: Design inverse modelling strategies for dynamic processes in complex subsurface structures
ESR13 : Veronika Rieckh
Fully coupled hydrogeophysical inversion of 3D tracer tomography using temporal moments and Ensemble KalmanFiltering
ESR14 : Andrea Palacios
Geologically constrained joint inversion of hydraulic, tracer and ERT data for process visualization
ESR15 : Jorge Lopez Alvis
Integration of dynamical hydrogeophysicaldata in a multiple-point geostatisticalframework
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This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Networking
• Personal Career DevelopmentPlan for each ESR
• 5 meetings• 5 workshops• 1 Summer School
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This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Training
Field & methods Theory and modeling Communication skills
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Objectives
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
Transfer of these innovations to the economic sector
(Final conference @Copenhagen)
Training of 15 ESR
Development of innovative methods for imaging process dynamics in subsurface
hydrosystems
Enhancing the understanding and predictive modelling capacities
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Achieved Results
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
- Most of training program completed (1 more workshop to go), particularsuccess of the Cargèse Summer School 2018
- Fruitful joint site experiments by ESRs (tracer tests in India and France)- Booklets preparation on state-of-the-art hydrogeophysics techniques- 4 publications so far (more in review) and numerous (60+) communications
in international conferences- Youtube channel of Cargèse Summer School classes (here)
- April 2020: ENIGMA Final Conference in Copenhagen (Denmark), organization led by ESRs
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Policy Feedback
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
- We want to provide tools to characterize and monitor the groundwater(instrument prototypes, state-of-the-art techniques, best practice, numerical models, inversion approaches)
- We think that european policies could rely on these developments for decision making concerning water management• monitoring available water quantity• risk estimation for water quality
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Thank you for your attention!
This project has received funding from European Union’s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie Grant Agreement n °722028.
More about ENIGMA ITN on https://enigma-itn.euRegister for the ENIGMA final conference on https://enigma-itn.sciencesconf.org/
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