Postes et offres d'emploi

L'Ecole Doctorale EGAAL propose des sujets de thèse https://theses.doctorat-bretagneloire.fr/egaal/campagne-2023

L'offre est ici

We wish to advertise 3 Post-doctoral Fellowships of 2 years in Geomorphology at the University of Rennes (France):  

• From extreme events to landscape building: monitoring and modelling the influence of earthquakes and monsoons on the dynamics of landscapes in the Himalayas of Nepal (Philippe Steer & Marin Clark)
• The impact of a single large storm event on river evolution and sediment transport: combining unique repeated Lidar data with 2D hydro-sedimentary simulations (Philippe Steer, Dimitri Lague, Laure Guerit, Philippe Davy)
• Investigating post-glacial transient phases as hot-moments of landscape dynamics - combining numerical modelling and topographic analysis (Philippe Steer & Pierre Valla)

The positions are part of the FEASIBLe (Finding how Earthquakes And Storms Impact the Building of Landscapes) project, funded by the European Research Council (ERC). Review of applications will start beginning of April 2023 and will be continued until the position is filled (even if we strongly wish to start these fellowships in June)

More infos on these positions and on how to apply here: https://sites.google.com/view/erc-feasible/job-vacancies

Offer description

We are pleased to announce a PhD position at University of Rennes, France on the modelling of heat transport processes in the subsurface. This position is offered in the frame of the recently funded ERC starting grant "CONCRETER" (Groundwater flow CONtrols on CRitical ZonE).
The characterization and predictive modeling of heat transfer processes in geological fractured media is of central interest for hydrogeological studies as well as for numerous industrial applications (radioactive waste disposal, geothermal systems). Traditionally, the integration of hydrothermal processes in (hydro)geological models follows approaches that do not take into account the complex nature of the circulation of fluids in the system (fracture network, fault zones). Only recently, through field experiments and theoretical investigations at the single fracture scale, we have provided evidence that flow channeling has a crucial impact on heat transport [Klepikova et al., 2016, https://doi.org/10.1002/2016WR018789; Klepikova et al., 2021, https://doi.org/10.1016/j.advwatres.2021.104042].
The next challenge is to reveal mechanisms of the coupling between the fracture and network-scale flow and heat transport complexities. This PhD project aims at developing a new generation of heat transport model to explore large-scale thermal behavior in a fractured geological formation. This new model will be based on the DFN.lab software platform that is developed in Rennes and uses the discrete fracture network (DFN) approach. The latter, contrary to widely used continuum modelling approaches, explicitly represents fractures as discrete features that form a network [e.g., Long et al., 1982, https://doi.org/10.1029/WR018i003p00645; Maillot et al., 2016, https://doi.org/10.1002/2016WR018973; Davy et al., 2018, https://onepetro.org/ARMADFNE/proceedings-abstract/DFNE18/1-DFNE18/D013S000R001/122702].
Through direct numerical simulations in synthetic configurations, a direct link between flow and heat transport behavior and the geometric and hydrological characteristics of the structure supporting the flow will be revealed. Based on these results, we will define simplified effective models at large scales in order to develop computationally efficient models enabling joint consideration of relevant heat transfer processes.

Requirements

Research Field - Geosciences or Physics or Environmental science
Education Level - Master Degree or equivalent
Skills/Qualifications
- Experience with computer programming /scripting (Matlab, Python, R)
- Sound and quantitative understanding of geological fluid flow
- Applicants must be proficient in both written and oral English
- Experience in fluid flow modelling in porous media is an advantage
- Experience with either reservoir modelling or hydrodynamic modelling is an advantage.
- Applicants must be able to work independently and in a structured manner and demonstrate good collaborative skills.
Scientific environment

Géosciences Rennes (GR) is a joint research unit (CNRS + UR1) with 60 permanent researchers. It hosts ~10 foreign researchers/year, and publishes ~ 100 papers/year. The Rennes hydrogeology group is composed of 15 permanent staff and is internationally recognized as one of the leading group in this field.
The PhD will be carried out in Geosciences Rennes and supervised by Maria Klepikova and Philippe Davy. The PhD student will also benefit from collaborations with the Fractory - a joint laboratory established in between the CNRS, the Univ. of Rennes and the company ITASCA Consultants SAS in the field of the modeling of environmental systems, fractorylab.org.

Please include in your application:

- a brief account of the applicant's research interests and motivation for applying for the position;
- the names and contact information for two referees (one of these should be the main advisor for the master's thesis or equivalent thesis);
- a CV;
- transcripts and diplomas showing completion of the bachelor's and master's degrees (if you have not yet completed your master's degree, please submit a statement from your institution confirming that the master's thesis has been submitted);
- relevant certificates/references;
- a list of any works of a scientific nature (publication list).
The application and appendices with translations into English or French must be sent to maria [dot] klepikovauniv-rennes [dot] fr.

Offer description

We are pleased to announce a PhD position at University of Rennes, France on the modelling of heat transport processes in the subsurface. This position is offered in the frame of the recently funded ERC starting grant "CONCRETER" (Groundwater flow CONtrols on CRitical ZonE).
Understanding heat transport processes in the subsurface is central to many environmental, geological and industrial processes. This includes geothermal applications, near-field thermal effects in radioactive waste disposals, urban heat islands and quantification of surface water‐groundwater interactions. Groundwater flow plays a key role in the distribution of heat at different scales. However, while this key role has been generally recognized, existing modeling frameworks have largely sidestepped the complexities associated with the heterogeneity in groundwater flow present at a wide range of spatial scales. The major scientific obstacle that prevents accurate understanding of the impact of subsurface heterogeneity in hydraulic and thermal properties on heat transport is related to our inability to image the hidden interaction between flow and heat transport processes at the pore/fracture scale [Heinze and Pastore, 2023, https://doi.org/10.1038/s41467-023-36034-w].
Recent studies raise questions regarding the relevance of classical models, i.e., models misrepresenting the structural heterogeneity, for modelling heat transport in the subsurface. Thus, in fractured media, our recent studies questioned the validity of the classical parallel plate fracture conceptualization [Klepikova et al., 2016, https://doi.org/10.1002/2016WR018789; Klepikova et al., 2021, https://doi.org/10.1016/j.advwatres.2021.104042].
This PhD project aims to examine the conditions in natural saturated fractured media under which classical formalisms, i.e., disregarding structural heterogeneity, apply and determine when they are expected to fail, and laboratory experiments are unique assets to tackle this issue. This raises technical challenges as current experimental techniques, based on point (sensor) temperature measurements, do not allow capturing the interplay between temperature gradients and 3D flow topologies. In this project, high resolution optical monitoring of the time-evolving temperature field will be achieved by a phosphor thermometry technique [Stelter et al., 2021, https://doi.org/10.18409/ispiv.v1i1.205]. The method will be applied to image the spatial distribution of temperature in rough geological fractures and to investigate the effects 3-D fracture geometry has on the scaling of heat recovery in both space and time.

Requirements

Research Field - Geosciences or Physics or Environmental science
Education Level - Master Degree or equivalent
Skills/Qualifications
- Sound and quantitative understanding of fluid mechanics
- Experience with computer programming /scripting (Matlab, Python, R) is an advantage
- Applicants must be proficient in both written and oral English
- Experience in fluid flow modelling in geological media is an advantage
- Applicants must be able to work independently and in interdisciplinary teams.
Scientific environment

Géosciences Rennes (GR) is a joint research unit (CNRS + UR1) with 60 permanent researchers. It hosts ~10 foreign researchers/year, and publishes ~ 100 papers/year. The Rennes hydrogeology group is composed of 15 permanent staff and is internationally recognized as one of the leading group in this field.
The PhD will be carried out in Geosciences Rennes and supervised by Maria Klepikova. The expertise on fluid experimentation in porous media systems will be provided by Y. Méheust, T. Le Borgne and J. Heyman, while the expertise in phosphor thermometry technique will be provided by B. Fond (ONERA - The French Aerospace Lab).

Please include in your application:

- a brief account of the applicant's research interests and motivation for applying for the position;
- the names and contact information for two referees (one of these should be the main advisor for the master's thesis or equivalent thesis);
- a CV;
- transcripts and diplomas showing completion of the bachelor's and master's degrees (if you have not yet completed your master's degree, please submit a statement from your institution confirming that the master's thesis has been submitted);
- relevant certificates/references;
- a list of any works of a scientific nature (publication list).
The application and appendices with translations into English or French must be sent to maria [dot] klepikovauniv-rennes1 [dot] fr