Search results for "Cronstedtite"

showing 2 items of 2 documents

A multi-technique characterisation of cronstedtite synthetized by iron-clay interaction in a step by step cooling procedure

2013

International audience; The cooling of steel containers in radioactive-waste storage was simulated in a step-by-step experiment from 90 to 40 degrees C. Among newly formed clay minerals observed in run products, cronstedtite was identified by a number of analytical techniques (powder X-ray diffraction, transmission electron microscopy, and scanning electron microscopy). Cronstedtite has not previously been recognized to be so abundant and so well crystallized in an iron-clay interaction experiment. The supersaturation of experimental solutions with respect to cronstedtite was due to the availability of Fe and Si in solution, as a result of the dissolution of iron metal powder, quartz, and m…

Materials scienceBase (chemistry)Analytical chemistry[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSoil Science020101 civil engineering02 engineering and technology010502 geochemistry & geophysics01 natural sciencesCronstedtite; Experimental iron-clay interaction; MDO polytypes; Radioactive waste storage0201 civil engineeringDiffraction tomographyGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryradioactive waste storageEarth and Planetary Sciences (miscellaneous)experimental iron-clay interactionDissolutionQuartz[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geologyMDO polytypes0105 earth and related environmental sciencesWater Science and Technologychemistry.chemical_classificationSupersaturationAtmospheric temperature rangeCronstedtiteCrystallographychemistrySelected area diffractionClay minerals[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Iron-clay interactions: Detailed study of the mineralogical transformation of claystone with emphasis on the formation of iron-rich T-O phyllosilicat…

2014

International audience; Iron-minerals-water interactions are of primary importance in the contexts of underground structure engineering (e.g. reactive barriers or deep geological storage) and for the understanding of secondary alteration processes in primitive meteorites. To improve our understanding of these systems, we determine the mineralogical transformations induced by the association of iron and silicates during a cooling through an experimental simulation of iron-clay interactions with a step-by-step procedure in the range of 90 degrees C to 40 degrees C. The run products and solutions are well characterised, by means of different techniques (X-ray diffraction, scanning and transmis…

Mineralogy[SDU.STU]Sciences of the Universe [physics]/Earth Sciences020101 civil engineering02 engineering and technologyengineering.materialGreenalite010502 geochemistry & geophysics01 natural sciences0201 civil engineeringMagnetitechemistry.chemical_compoundGeochemistry and PetrologyKaoliniteDissolutionChloriteQuartz0105 earth and related environmental sciencesMagnetiteIron-claystone interaction; Cronstedtite; Greenalite; Magnetite; Cooling experimentGeologyGreenaliteCronstedtiteIron-claystone interactionCooling experimentMeteoritechemistry13. Climate actionIlliteengineeringGeology
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