Analytical equipments

Louvain-La-Neuve

Main equipment

The main equipment of the platform are listed below, with the applications for which they are used.

Equipment
Principle
Applications
δ18O and δD Analyzer
The Picarro L2130-i analyser is an essential tool for research requiring highly accurate and reliable isotopic analysis of water (δD and δ18O).
It contributes to a better understanding and management of water resources, from the study of hydrological cycles to the traceability of water resources.
Thanks to this advanced technology, isotopic analysis of water can be carried out with great precision and reliability, allowing to conduct innovative research and provide high-quality scientific solutions.
Isotope analysis of water
Determination of water isotope ratios: H216O, H218O and HD16O molecules
C,N,S Elemental Analyser system
The elementary analyzer works on the principle of catalytic combustion and separation of the gases released during it.
At the time of this combustion, the elements C, N, S are oxidized to CO2, H2O, NOx, SO2 and SO3.
The NOx released during this oxidation are reduced to N2 and directly sent to the thermo-conductive detector (TCD).

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Food
 - Protein determination
 - Verification of low N content in gluten-free products
Pharmaceutical - Tracking of C content in drugs (eg aspirin, etc.)
Environment
  - C / N ratio in soils and sulfur in volcanic discharges
  - Measuring stages of litter decomposition
Energy - Checking the sulfur content in fuels
Isotope Ratio Mass Spectrometer - IRMS
Coupled with an elementary analyser, the Elementar Isoprime precisION determines the isotopic signatures of solid matrices (soil, sediments, plants, etc.).
Isotopic signature of solid matrices (soil, sediments, plants, etc.)
  - understand process such as the evolution of organic carbon in soils, or sources such as sources of nitrogen in atmospheric deposits : nitrates, ammonia, nitrogen oxides, etc
  - monitor food regimes within trophic networks
  - understand the nitrogen cycle
  - analyse the dynamics of pesticides
Gas Chromatography
Gas Chromatography is a technique for separating a mixture of thermostable and volatile molecules.
This method is often used to check the purity of a given substance, or to separate the components of a mixture to determine the relative amounts of each compound.

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Determination of :
  - volatile fatty acids (from C2 to C6)
  - fatty acids, in the form of methyl ester
  - sugars, in the form of TMS
  - PAHs and PCBs
High Pressure Liquid Chromatography
High Pressure Liquid Chromatography allows the separation or the purification of one or more compounds of a mixture with a view to their identification and their quantification.
This technique makes it possible to carry out a large part of the analyzes made in Gas Chromatography but especially those which are impossible with these techniques such as the analysis of thermosensitive compounds or of molecular masses which are both very large and even polar.

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Determination of :
  - amino acid
  - water-soluble vitamins (Vit. B and Vit. C) and fat-soluble vitamins (Vit. A and Vit. E)
  - the GSH/GSSG ratio (oxidative stress indicator)
  - volatile fatty acids (from C2 to C6)
  - chlorophylls and xanthophylls
  - polyamines
Sugar dosage
Assay of cytotoxics
Identification of lipopeptides by LC-MS
Inductively Coupled Plasma spectrometry
Inductively Coupled Plasma spectrometry (ICP) is a chemical analytical method allowing the determination of almost all the elements simultaneously thanks to the high temperature of the argon plasma (> 8000°C).

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Mineral matrices
  - Chemical analysis of Soils and Waters: major elements (Ca, K, Na, Mg, P, Al, Fe, Mn, S) and ETM - metallic elements in trace form (B, Cd, Cu, Pb, Zn)
  - Determination of S in thermal waters
  - Catalyst tracking
Biological matrices
  - Detection of heavy metals (As, Cd, Hg) in plants,
  - Zn, Cu and Se content in bull semen
  - Al dosage - Eel toxicity study
  - Determination of Cd in cocoa beans
Environment
  - Isotope analysis in various matrices (rock, soil, sediment, selective soil extractions, soil solution, river water, plant tissue): Si isotopes, Mg isotopes, radiogenic Sr isotopes (87Sr/86Sr)
  - Field of applications: thermal waters (anion-rich), polar rivers (low concentration, organic-rich), soil-plant systems
Archeology
  - Tooth: radiogenic Sr isotopes (87Sr/86Sr)
Liquid Phase Ion Chromatography
Liquid Phase Ion Chromatography (IC) allows the identification and simultaneous quantification of various inorganic and organic ions (cations and anions). The principle of this technique is based on the differences in ion affinities for a functionalized substrate (ion exchange resin) in the presence of a carrier liquid phase (eluent).

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Environment
  - Anion measurement: F-, Cl-, SO42-, NO2-, NO3-, PO43-
  - Measurement of cations: Ca2+, Na+, NH4+, K+, Mg2+, Al+, Fe2+/3+
Food
  - Sugar dosage
  - Determination of organic acids
TOC Analyser
The determination of dissolved carbon is an essential analytical prerequisite in many agronomic and environmental problems in aqueous media: detection of organic contaminants in soils, control of the decomposition of organic matter from the soil  surface, etc.
In these various contexts, the use of a carbon analyzer is particularly judicious when organic substances appear at low concentration levels.

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  - in the clay fraction (f <2 µm) of soils and in sediments
  - in solutions extracted from acid forest soils and in the liquid phase of hydromorphic soils downstream of agricultural plots
  - in rainwater, rivers, lysimeters in forest ecosystems
  - in soil and river waters in areas of permafrost thawed in the context of global warming
  - measurement of different forms of carbon in river water, waste water, sea water
UV-VIS Spectrometer
Spectrophotometry is a non-destructive and rapid analysis method which is widely used in the laboratory. This technique makes it possible to determine the absorbance of a chemical substance in solution, that is to say its capacity to absorb the light passing through it.
UV-Visible spectrophotometry makes it possible to provide qualitative information on the nature of the bonds present within the sample (via the order of magnitude of λmax and εmax) but also to quantitatively determine the concentration of species absorbing in this spectral range (via Beer-Lambert law).

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This technique will also make it possible to follow the kinetics of a chemical reaction.
X-Ray Diffractometer
The application of X-Ray Diffraction (DRX) relates to the identification and quantification of crystalline minerals in the soil. Among these, phyllosilicates constitute a privileged object of study given their preferential location in the fine fraction of soils and their colloidal properties: high specific surface, electrical charge, ion exchange, adsorption of metallic elements, pesticides, etc.
This analysis technique makes it possible to characterize the arrangement of atoms and layers of atoms as organized within crystals.
It complements other techniques and is not an exclusive tool for characterizing soil minerals.

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  - Mineralogical identification of soils (Quartz, Mica, Magnetite, Pyroxene…)
  - Identification of clays
  - Identification of cheese residues (Brushite and Giniitte)

 

Various specialized equipment