Les plasmas induits par laser (PIL) ont depuis leurs apparitions dans les années soixante suscité un très grand intérêt notamment comme source de données spectroscopiques. Ils ont également acquis des nombreuses applications, comme sources des rayons X pour la lithographie, l’allumage plasma, la déposition par laser pulsé, ou sont devenues la base d’une technique d’analyse très populaire – la LIBS (laser induced breakdown spectroscopy). Cette dernière peut s’appliquer in situe à tout type d’échantillon et sans préparation. Toutefois, les mesures faites par cette méthode sont latéralement intégrées nécessitant des techniques d’inversion, mais dépendent également des conditions d’équilibre thermodynamiques local (ETL) dans le plasma. Afin de valider les mesures effectuées par LIBS, la diffusion Thomson qui est une méthode spatialement résolue et indépendante des hypothèses d’équilibre thermodynamique a été appliquée pour caractériser les PIL. Des plasmas d’ablation et de claquage ont donc été caractérisés à la fois par spectroscopie d’émission et par diffusion Thomson. La comparaison des paramètres température et densité électronique obtenues par les deux méthodes d’une part, et le critère de McWhirter ainsi que les temps de relaxation et les longueurs de diffusions des espèces contenues dans le plasma d’autre part, ont permis de statuer sur l’ETL. / Laser induced plasma (LIP) which was first reported in the beginning of sixties, has achieved a great interest as a source of spectroscopic data. It has also many applications like X-ray sources for lithography, plasma igniters, pulsed laser deposition or it has become a basis of a very popular analytical technique – LIBS (laser induced breakdown spectroscopy). The latter is mainly due to its applicability to different kinds of samples, no sample preparation or in-situ and remote sensing capability. However, LIBS measurements are laterally integrated and Abel inversion must be performed. Also the method assumes the plasma to be in local thermodynamic equilibrium (LTE). In order to validate LIBS measurements, Thomson scattering (TS) method which is spatially resolved and free from equilibrium assumption was applied. Thus, ablation and breakdown plasmas were characterized by both two methods. Comparison between plasma parameters (temperature and electron density) obtained by the two methods and McWhirter criterion as well as relaxation times and diffusion lengths of species in the plasma allowed to estimate LTE.

This master’s thesis is focused on the LIBS technique for compositional differentiation and relative hardness quantification of selected geological samples. The experimental part of this thesis was conducted at the National Institute of Laser Enhanced Sciences (NILES) in Cairo, Egypt where a simple LIBS system was constructed. In parallel to the experimental work, the literature review was surveyed with the aim to give a thorough view of the history, fundamentals and all the factors related to LIBS. LIBS is a developing analytical technique, which is used to perform qualitative and semi-quantitative elemental analysis of materials (solid, liquid and gas). The fast data collection and the lack of sample preparation made LIBS be an attractive technique to be used for geological samples. This study was done to improve analytical methods for geochemical analysis of samples during different exploration phases (Mining, filed analysis, etc.), as a real-time analysis method to save money and time spent in labs. For a generation of laser induced plasma, a Q-switched Nd: YAG laser operated at 10 Hz and wavelength of 1064 nm was employed on the surface of the samples. A spectrometer fitted with an intensified charge-coupled device (ICCD) was used to disperse and detect the spectrum; then fed to a computer for recording and further processing of the data. The sample set was compiled from samples collected from different areas (South Africa and Namibia). Using principal component analysis (PCA), it was found that LIBS was able to differentiate between the samples even those of the same area. The results from the LIBS technique were correlated with subsequent analysis of the same samples by Particle-induced X-ray emission (PIXE). The feasibility of relative hardness estimation using LIBS was done by measuring the plasma excitation temperature for different samples. LIBS with its advantages as an elemental analysis technique made it possible to estimate the hardness of geological samples. Based on theory and results, an analytical technique for compositional differentiation and quantification of relative hardness of geological samples is proposed. / National Research Foundation (South Africa) / Physics / M Sc. (Physics)