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Jacques Pironon

Researcher at University of Lorraine

Publications -  153
Citations -  3370

Jacques Pironon is an academic researcher from University of Lorraine. The author has contributed to research in topics: Fluid inclusions & Inclusion (mineral). The author has an hindex of 32, co-authored 145 publications receiving 2978 citations. Previous affiliations of Jacques Pironon include Nancy-Université & Centre national de la recherche scientifique.

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Oil–water two‐phase flow in microchannels: Flow patterns and pressure drop measurements

TL;DR: In this article, the authors investigated oil-water two-phase flows in microchannels of 793 and 667 µm hydraulic diameters made of quartz and glass, respectively, by injecting one fluid at a constant flow rate and the second at variable flow rate.
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Calcite precipitation from CO2–H2O–Ca(OH)2 slurry under high pressure of CO2

TL;DR: In this paper, the formation of solid calcium carbonate (CaCO3) from aqueous solutions or slurries containing calcium and carbon dioxide (CO2) is a complex process of considerable importance in the ecological, geochemical and biological areas.
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Methane-bearing aqueous fluid inclusions: Raman analysis, thermodynamic modelling and application to petroleum basins

TL;DR: In this article, Duan et al. used Raman spectroscopy to calculate the composition of the aqueous liquid phase coexisting with the vapour phase in the synthetic fluid inclusions.
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PIT (Petroleum Inclusion Thermodynamic): a new modeling tool for the characterization of hydrocarbon fluid inclusions from volumetric and microthermometric measurements

TL;DR: Pironon et al. as discussed by the authors proposed a new modeling tool, called Petroleum Inclusion Thermodynamic (PIT), based on applied thermodynamics of natural oils, for interpreting volumetric (Fv) and micro-thermometric (Th) measurements obtained on hydrocarbon fluid inclusions.
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Characterization of smectite and illite by FTIR spectroscopy of interlayer NH+4 cations

TL;DR: In this paper, the authors applied FTIR spectroscopy to NH +-exchanged dioctahedral clay minerals to determine the molecular environment of NH+ and to quantify N concentration.