Electric vehicle energy model
The project is a simple electric vehicle energy model. It uses the fundamental principle of dynamics to determine the power profile seen by a battery cell for a given mission. The input data are GPX files of the actual path considered. They can also be replaced by a speed and slope profile. In the ...
Physico-chemical parameters and isotopic signatures of the waters of the Forbonnet peatland
pH, electrical conductivity, temperature, redox potential, major elements concentration, and isotope analyses (87Sr/86Sr ratio, 13C of the dissolved inorganic carbon, 18O and 2H of the water molecule) of waters sampled at the Forbonnet peatland. All the methods of acquisition and laboratory ...
Model energetic macroscopic representation (EMR) of the Fuel Cell and leads to a so-called maximal control structure (MCS)
This modeling presents the control part of a proton exchange membrane fuel cell (PEMFC). The objective of the model is to represent the voltage control chain of the PEMFC. This model is based on an energetic macroscopic representation (EMR) of the fuel cell and then leads to a so-called maximum ...
Data on genes expression in Pseudomonas aeruginosa
Pseudomonas aeruginosa is a Gram-negative Human opportunistic pathogen, responsible for nosocomial infections with high mortality for immunocompromised patients. The pathogenesis is based on the production of many structural or secreted virulence factors. P. aeruginosa is also able to produce ...
Glaciological data Austre Lovén Svalbard
These data are measured in High Arctic over an observatory basin, located at 79°N on the W coast of Svalbard. Austre Lovén is a small 4.5 km² polythermal glacier in constant decline since the end of the LIA. The surrounding catchment is no more than 10 km² and exhibits a significant periglacial area ...
Numerical modelling of the impact of the structural anisotropy on the thermal diffusivity
Numerical modelling of the impact of the structural anisotropy on the thermal diffusivity using 1D and 2D codes.
Raman spectrometry on Carbonaceous Material (RSCM) thermometry - Aiguilles Rouges massif
RSCM analyses on metamorphic rocks from the Servoz syncline.
Structural data - Aiguilles Rouges - Mont-Blanc massifs
Field-work structural data (foliations, schistosities and lineations).
Geochemical data - Aiguilles Rouges - Mont-Blanc massifs
Contents of major and trace elements and of Rare Earth elements from whole rocks and minerals.
Geochronological data - Aiguilles Rouges - Mont-Blanc massifs
LA-ICPMS U-Th-Pb analyses on zircon and monazite from the Aiguilles Rouges - Mont-Blanc massifs.
Geochronological data - Agly massif
LA-ICPMS U-Th-Pb analyses on zircon and monazite from the Agly massif.
Structural data - Agly massif
Structural database of foliations, schistosities and lineations of variscan ductile structures of the Agly massif.
Physicochemical characteristics of water and sediment - floodplains of the Ain, Doubs and Loue Rivers - 2015-2016
19 sites (16 wetlands and 3 rivers) with different physicochemical characteristics and distributed along three rivers (Ain, Doubs, and Loue) were sampled. The physicochemical characteristics of the wetlands were measured in situ or after laboratory analysis.
Physicochemical characteristics of water and sediment - Ain River floodplain - 2019-2020
34 sites (16 wetland sites, 15 river sites, and 3 groundwaters) distributed along the Ain River with different physicochemical characteristics were sampled. The physicochemical characteristics of the wetlands were measured in situ or after laboratory analysis.
Abondances and genotypic characteristics of gram-negative bacteria in the environment - Ain River floodplain - 2019-2020
34 sites (16 wetland sites, 15 river sites, and 3 groundwaters) distributed along the Ain River with different physicochemical characteristics were sampled. The abundances of some gram-negative bacteria (Escherichia coli, extended-spectrum beta-lactamase (ESBL)-producing E. coli, Klebsiella ...
Phytomanagement - Tavaux (F-39)
The site is located in Western Europe along a major river and surrounded by several urban aggregates. Production at the chlor- alkali facility began in 1950 with wastewater discharged directly to a stream. In 1964 a dam was constructed downstream of the discharge. A 12-ha area with dikes 5-m high ...
Phytomanagement - Thann (F-68)
The experimental site of Thann is located in the valley of the Thur in Alsace (France) near the border with Germany and Switzerland, on a 15 ha-chemistry-based industrial complex. The Thann plant owned by the TRONOX company is one of the most important sites for TiO2 production in Europe and is the ...
EBSD mapping of shear zones strain gradient - deformation mechanisms
Objective : characterize the deformation mechanisms and the crystallographic fabrics within homogeneously deformed granitic samples.
EBSD mapping of brittle shear zones precursors
Objective : microtextural characterization within a shear zone brittle precursor
EBSD mapping of shear zones strain gradient - seismic anisotropy
Objective : calculate the crystallographic preferred orientation (CPO) of each mineral phase in order to rebuild the elastic properties of the polyminéralic aggregates.
Microprobe analysis on a brittle shear zone precursor
Objective : compare the chemical compositions of minerals within the brittle precursor and in the host rock.
Quantitative X-ray mapping of brittle shear zones precursors
Objective : characterize the chemical zonings in plagioclase and garnet related to fluid-rock interactions within a shear zone precursor
Satellite images of cloud types products in West Africa from March to August in 2017
It is products developped by Meteo France through the SAF application, showing the types of clouds in function of their elevation.
Jurassic Karst
Hydrogeochemical monitoring of karst springs in the Jura mountains
Majors, traces elements and strontium isotopes (87Sr/86Sr) of Cretaceous limestone and Quaternary marl - Jura Mountains
Majors, traces elements and 87Sr/86Sr ratio of Cretaceous limestone (Hauterivien) and Quaternary marls (two samples). The limestone was sampled in the Frasne-Bouverans syncline at proximity of the Forbonnet pealtand (Complexe tourbeux de Frasne-Bouverans). The marl was sampled in the underlying ...
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