Search results for "Kaolinite"

showing 10 items of 65 documents

X-ray diffraction Warren–Averbach mullite analysis in whiteware porcelains: influence of kaolin raw material

2018

ABSTRACTCompositional and microstructural analysis of mullites in porcelain whitewares obtained by the firing of two blends of identical triaxial composition using a kaolin B consisting of ‘higher-crystallinity’ kaolinite or a finer halloysitic kaolin M of lower crystal order was performed. No significant changes in the average Al2O3 contents (near the stoichiometric composition 3:2) of the mullites were observed. Fast and slow firing at the same temperature using B or M kaolin yielded different mullite contents. The Warren–Averbach method showed increase of the D110 mullite crystallite size and crystallite size distributions with small shifts to greater values with increasing firing temper…

010302 applied physicsMaterials scienceStoichiometric compositionMullite02 engineering and technologyRaw material021001 nanoscience & nanotechnology01 natural sciencesCrystalGeochemistry and Petrology0103 physical sciencesX-ray crystallographyKaoliniteCrystalliteThickeningComposite material0210 nano-technologyClay Minerals
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Soil development on sediments and evaporites of the Messinian crisis

2020

Abstract Vast areas in the Mediterranean are characterised by evaporite deposits of the Messinian crises (c. 6–5.3 Ma BP). During this period, large deposits were built up in shallow lagoon-like systems and are now found in southern Italy, Albania, Cyprus and Turkey. So far, soil formation on evaporites has been studied predominantly in subarid to arid environments. Although the formation of soils has received new significance, little is known about the evolutional trajectories on evaporites of the Mediterranean. We therefore studied soil formation in the Caltanissetta basin (Sicily) where evaporites are most widespread. The lithologies included the sequence: marine clay deposits, laminated…

010504 meteorology & atmospheric sciencesEvaporite1904 Earth-Surface ProcessesGeochemistryEarthWeathering04 agricultural and veterinary sciences01 natural sciencesDiagenesis10122 Institute of GeographyPedogenesisSurface ProcessesSettore AGR/14 - PedologiaSoil formation Evaporites Clay mineralogy Weathering Diatomite Stable isotopes CarbonatesLeaching (pedology)Marl040103 agronomy & agriculture0401 agriculture forestry and fisheriesKaoliniteAridisol910 Geography & travelGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in th…

2017

Mineral dust and secondary organic aerosols (SOA) account for a major fraction of atmospheric particulate matter, affecting climate, air quality and public health. How mineral dust interacts with SOA to influence cloud chemistry and public health, however, is not well understood. Here, we investigated the formation of reactive oxygen species (ROS), which are key species of atmospheric and physiological chemistry, in aqueous mixtures of SOA and mineral dust by applying electron paramagnetic resonance (EPR) spectrometry in combination with a spin-trapping technique, liquid chromatography-tandem mass spectrometry (LC-MS/MS), and a kinetic model. We found that substantial amounts of ROS includi…

010504 meteorology & atmospheric sciencesRadicalInorganic chemistry010501 environmental sciencesMineral dustbehavioral disciplines and activities01 natural scienceschemistry.chemical_compoundKaolinitePhysical and Theoretical ChemistryIsoprene0105 earth and related environmental sciencesAerosolsAir PollutantsMineralsAqueous solutionAtmosphereWaterParticulatesDecompositionDeposition (aerosol physics)chemistryEnvironmental chemistryParticulate MatterPublic HealthReactive Oxygen SpeciesFaraday Discussions
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Environmental and climatic controls of the clay mineralogy of Albian deposits in the Paris and Vocontian basins (France)

2020

18 pages; International audience; High-resolution clay mineral analyses were performed on lower and middle Albian deposits from the Paris and Vocontian basins in order to specify the weathering conditions that prevailed at that time. The clay mineral assemblages are composed of small proportions of chlorite and vermiculitic clays associated with abundant illite, R0 type illite-smectite mixed-layers (smectite) and kaolinite. Clay minerals originated from the physical alteration and chemical weathering of rocks and soils outcropping on the Variscan massifs bordering the studied areas. In the Paris Basin, the covariation of illite and kaolinite suggests the reworking of these latter minerals f…

010506 paleontologyAptianOutcropGeochemistryWeatheringengineering.materialPalaeoclimate010502 geochemistry & geophysics01 natural sciencesParis BasinKaoliniteMortoniceras0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyPaleontologyAlbianMassifbiology.organism_classificationClay mineralsVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringClay mineralsGeologyCretaceous Research
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Conjunctive use of spectral gamma-ray logs and clay mineralogy in defining late Jurassic-early Cretaceous palaeoclimate change (Dorset, U.K.).

2006

Abstract Detrital clay mineralogy is controlled by weathered source rock, climate, transport and deposition that in turn influence the spectral gamma-ray (SGR) response of resultant sediments. Whilst a palaeoclimate signal in clay mineralogy has been established in some ancient successions, the SGR response remains contentious, largely because the data sets have yet to be collected at the same or appropriate vertical scales to allow comparison. In addition, the influence of organic matter on SGR is not always considered. Here, we present clay mineralogical, total organic carbon (TOC) and SGR analyses from the late Jurassic and early Cretaceous of the Wessex Basin, a period of previously doc…

010506 paleontologyJurassic-Cretaceous boundary[SDE.MCG]Environmental Sciences/Global ChangesSpectral gamma raychemistry.chemical_elementStructural basin010502 geochemistry & geophysicsOceanographyPalaeoclimate[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontology[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgDorsetKaoliniteOrganic matter[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/MineralogyEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbonchemistry.chemical_classificationPaleontologyThoriumClay mineralogyCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesSource rockchemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPurbeck facies[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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The Mid-Cenomanian Event in southeastern France: evidence from palaeontological and clay mineralogical data.

2013

16 pages; International audience; Reconstruction of main palaeoenvironmental conditions across the Mid-Cenomanian Event (MCE I) in the hemipelagic Tethyan section of Blieux (Southeast France, Vocontian Basin) is proposed. Quantitative analyses of calcareous nannofossil, ammonoid and clay mineral assemblages have been made and compared with respect to sea level changes and the carbon cycle perturbations. The nannofossil primary productivity, as recorded by nannofossil fluxes and relative abundances of meso-eutrophic taxa, is low just below and during the MCE Ia, then slightly increases in the interval including the MCE Ib. The clay assemblages mainly consist of illite/smectite mixed-layers w…

010506 paleontology[SDE.MCG]Environmental Sciences/Global Changesengineering.material[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesClimatic conditionsPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySchloenbachiaCalcareous nannofossilsKaoliniteRelative species abundanceSea level[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesMiddle CenomanianbiologyAmmonoidsPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.organism_classificationCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringPrimary productivityCenomanianClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Late Jurassic palaeoclimatic change from clay mineralogy and gamma-ray spectrometry of the Kimmeridge Clay, Dorset, UK

2009

Abstract: The Late Jurassic was a time of increasing aridity in NW Europe. Here, a new clay mineral dataset is presented from a 600 m thick composite core through the Kimmeridge Clay Formation, southern England. Clay mineral assemblages comprise mainly illite and kaolinite, with minor randomly interstratified illite–smectite mixed-layer clays. SEM observations indicate that clay minerals are mainly detrital, except in silty strata of late Tithonian age, which contain abundant pore-filling kaolinite aggregates. Th/K ratios determined from gamma-ray spectrometry mirror palaeoclimatically significant variations in kaolinite/illite ratios, with notable exception where diagenetic kaolinite occur…

010506 paleontology[SDE.MCG]Environmental Sciences/Global Changesengineering.material[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontologychemistry.chemical_compound[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryPhanerozoicKaoliniteMesozoic0105 earth and related environmental sciencesGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySilicateDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesKimmeridge Claychemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringClay mineralsGeologyJournal of the Geological Society
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Characterization of the porous structure of Chilean volcanic soils by nitrogen adsorption and mercury porosimetry

2004

Pore volume, specific surface area (SSA), and total intragranular porosity (TIP) of Chilean soils derived from volcanic materials were studied. Soil samples involving the 0-15 and 15-30 cm depth of virgin and cultivated Collipulli (Ultisol) and Diguillin (Andisol) soils at two particle size fractions (<1 mm and <2 µm) were considered. From mercury porosimetry and N2 adsorption, mainly mesopores (pore diameter, dpore, about 10 nm) were determined for <1 mm Collipulli samples. Diguillin <1 mm soil shows macroporosity with dpore from 70 nm to 7000 nm. The clay fraction of Collipulli has macropores (dpore from 2000 nm to 40000 nm) and mesopores (dpore from 3 nm to 23 nm), while for Diguillin cl…

021110 strategic defence & security studiesMaterials scienceMacropore0211 other engineering and technologiesAnalytical chemistryMineralogy02 engineering and technologyGeneral ChemistryPorosimetry15. Life on land021001 nanoscience & nanotechnologyAndisol[SPI]Engineering Sciences [physics]AdsorptionSpecific surface areaKaolinite0210 nano-technologyAllophanePorosityComputingMilieux_MISCELLANEOUS
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Retention of Vanadium(V), Molybdenum(VI) and Tungsten(VI) by Kaolin

1993

Abstract The ability of kaolin (approximately H2Al2Si2O8 · H2O), a well known clay mineral constituent, to retain V(V) andMo(VI) species from 10−5 and 10−4 M solutions, and W(VI) species from 10−4 M solutions was investigated in the pH range 2–7.5 using a solid/liquid ratio 1:100 (w:v). The equilibration time in the adsorption studies was 72 h, and the shaking time in the desorption studies was 17 h. 0.02 M KCl was used as ionic medium and desorbing liquid. V(V), Mo(VI) and W(VI) were all retained by kaolin to some extent, and the amounts of the elements which could be washed away from kaolin with 0.02 M KCl were very small. The pH dependence of the adsorption was considerable: when added a…

AdsorptionChemistryMolybdenumDesorptionInorganic chemistrySoil Sciencechemistry.chemical_elementKaoliniteIonic bondingVanadiumTungstenClay mineralsAgronomy and Crop ScienceActa Agriculturae Scandinavica, Section B - Soil &amp; Plant Science
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Selective adsorption of oppositely charged PNIPAAM on halloysite surfaces: a route to thermo-responsive nanocarriers.

2018

Halloysite nanotubes were functionalized with stimuli-responsive macromolecules to generate smart nanohybrids. Poly(N-isopropylacrylamide)-co-methacrylic acid (PNIPAAM-co-MA) was selectively adsorbed into halloysite lumen by exploiting electrostatic interactions. Amine-terminated PNIPAAM polymer was also investigated that selectively interacts with the outer surface of the nanotubes. The adsorption site has a profound effect on the thermodynamic behavior and therefore temperature responsive features of the hybrid material. The drug release kinetics was investigated by using diclofenac as a non-steroidal anti-inflammatory drug model. The release kinetics depends on the nanoarchitecture of th…

AmideMaterials scienceTechnological applicationBioengineering02 engineering and technologyengineering.material010402 general chemistry01 natural sciencesHalloysiteLower critical solution temperatureAcrylic monomerchemistry.chemical_compoundAdsorptionthermo-responsive materialKaoliniteGeneral Materials ScienceElectrical and Electronic EngineeringNon-steroidal anti-inflammatory drugPoly (n isopropylacrylamide)Hybrid materialTargeted drug deliveryThermodynamic behaviors Controlled drug deliveryMechanical EngineeringHalloysiteGeneral Chemistry021001 nanoscience & nanotechnologyControlled release0104 chemical sciencesNanotubeHydrogelChemical engineeringchemistryMechanics of MaterialsSelective adsorptionSelf-healing hydrogelsengineeringPoly(N-isopropylacrylamide)0210 nano-technologyHybrid materialTemperature-responsivecontrolled releaseYarn Controlled releaseThermo-responsiveNanotechnology
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