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This article discusses the use of X-ray diffraction (XRD) as a tool for material characterization and mineral quantification in applied geology and mineralogy. It covers the principles of XRD, the equipment used, and the challenges and disadvantages of traditional sample preparation methods. It also presents a standardized procedure for sample preparation and introduces the Rietveld method for accurate quantification and structure analysis. Practical information and support for XRD measurements are provided.
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ClaylabAppliedGeology & Mineralogy X-raydiffraction A tool formaterialcharacterization and mineralquantification Rieko Adriaens rieko.adriaens@ees.kuleuven.be 23/01/2013
X-ray diffraction on mineral powders Mono- chromator Antiscatter- slit Divergence slit Detector- slit Tube Sample
θ 2 Diffractionpattern Detector Tube θ Sample focusing-circle measurement circle
Unique fingerprintforanorganicsubstances a = b = c o 90 = = = c a b
crystalline Amorphous
Errors in XRD – analysis: Vendor competition Sample preparation Measurement Identification Quantification
Sample preparation: Classicalapproach • Manualgrindingusingmortar & pestle • Back/top loading of holderapplyingpressure
Classicalapproach: disadvantages • Presence of coarseparticles and bad loadingcauseseveralnegativeeffects: • Extreme preferredorientation • Patternshifts • Verypoorreproducibility • Complex identification & wrong quantification
Classicalapproach: disadvantages • Preferredorientation & patternshifts XRD pattern: Ideal case
Classicalapproach: disadvantages • Preferredorientation: Cleavageplanes & prominent crystalfaces Halite Quartz Gypsum Mica
Classicalapproach: disadvantages • Preferredorientation & patternshifts • Verypoorreproducibility !!!
Bulk XRD – analysis • Disadvantagesimpede accurate Q-XRD • Neccessity of standardizedpreparation procedures We need a procedure whichmakessurethat: • Particlesshouldbefinerthan <50µm • Wet grindinginstead of dry grinding • Particles are randomlyoriented in the measurementholder • Sample surfaceshouldbesmooth and perfectly flat • Reproducible & representativemeasurements
Standardized procedure afterSrodon, 2001 • Powder mixed withinternalstandard (ZnO, Al2O3, TiO2 ) • Grinding media (Al2O3, Yttriastabilized Zr) • Grinding agent: methanol/ ethanol • McCronemicronizingmill (5min.) • Side loadfilling / nopressure top load
Standardized procedure afterSrodon, 2001 • Good random orientation of crystallitesobtained BUT canbeimprovedby the making of sphericalgranules: use of Vertrel XF treatment, spray dryingequipment, elvacitetreatment,… Kaolinite Portland cement
Standardized procedure: Validation Classic methodology Renewedmethodology
Standardized procedure: Validation Muchlesspreferredorientation Classic methodology Renewedmethodology
Standardized procedure afterSrodon, 2001 • Allows accurate Q-XRD analysis
[The Rietveld Method] • Most powerfulmethodforcombinedquantification and structureanalysis • Relieson the refinement of basictheoreticalstructures • Minimizedifferencebetweencalculated XRD pattern and measured XRD pattern
Rietveld refinement: procedure • Measure the diffractionpattern of the sample • Comparebothpatterns • Refine parameters and recalculatepattern • Draw info from the refined data (crystallitesizes / quantitativephaseinformation / …) • Introducereasonablestarting models / values to calculate a diffractionpattern
Whatcanbeevaluatedwith a Rietveld refinement ? • Example: Cement Fullyamorphousblastfurnace slag ZnO as internalstandard
Whatcanbeevaluatedwith a Rietveld refinement ? <10nm crystallites • CrystalliteSizes / Strain • Absolute Crystallitesizes Usefulfor: • Processoptimisation • Product characterisation • Product qualityassesment Finercrystallites are prone to reactfaster (or to reactbetter as catalysts, etc.) • Assessment of crystalliteshape (in case of anisotropicpeaksizebroadening)
Whatcanbeevaluatedwith a Rietveld refinement ? • SolidSolution • Example: Fe-richDolomite (CaMg(CO3)2) – Ankerite (CaFe(CO3)2) • Change in lattice parameters as a function of the Fe-content With a Rietveld refinement; Lattice parameters and henceFe-contentscanbeaccuratelydetermined Example: Fe-richDolomite/Ankerite in Sedimentary rock: Exact average formula: Ca(Fe0,46Mg0,54)(CO3)2 Fe-Dolomite
Practical information 1st floor Software computers XRD rooms Groundfloor 1st floor
Practical information Reservationshttps://ees.kuleuven.be/reservations/xrd/calendar/index.html
Practical information Measurementsoverview list
Practical information Technical support: Dirk Steeno dirk.steeno@ees.kuleuven.be 200C – 00.89 General support: Rieko Adriaens rieko.adriaens@ees.kuleuven.be 200E – 03.217 Responsible professor: Jan Elsen jan.elsen@ees.kuleuven.be 200E – 02.207
Questions / more information Contact rieko.adriaens@ees.kuleuven.be