Search results for "MINERALS"

showing 10 items of 247 documents

Evaluation of the Bioaccessibility of Antioxidant Bioactive Compounds and Minerals of Four Genotypes of

2019

Microgreens constitute an emerging class of fresh, healthy foods due to their nutritional composition. In this study the content of minerals and antioxidant bioactive compounds, and for the first time bioaccessibility, were evaluated in broccoli (Brassica oleracea L. var. italica Plenck), green curly kale (Brassica oleracea var. sabellica L.), red mustard (Brassica juncea (L.) Czern.) and radish (Raphanus sativus L.) hydroponic microgreens. Macro- (K, Ca, Mg) and oligo-elements (Fe, Zn), ascorbic acid, total soluble polyphenols, total carotenoids, total anthocyanins, total isothiocyanates and total antioxidant capacity (Trolox Equivalent Antioxidant Capacity and Oxygen Radical Absorbance Ca…

bioactive compoundsantioxidantsmicrogreensBrassicaceaefood and beveragesmineralsArticlebioaccessibilityFoods (Basel, Switzerland)
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The geochemistry of Tl and its isotopes during magmatic and hydrothermal processes: The peralkaline Ilimaussaq complex, southwest Greenland

2014

Abstract We use thallium (Tl) concentrations, K/Rb, K/Tl and Rb/Tl ratios and Tl isotopes in minerals from the alkaline to peralkaline Ilimaussaq complex (South Greenland) to trace magmatic differentiation, crustal assimilation, magmatic degassing, ore precipitation and hydrothermal metasomatism. Closed-system magmatic differentiation is marked by a coherent decrease of K/Tl- and K/Rb-ratios, whereas crustal assimilation results in a strong Tl-enrichment, causing low K/Tl-ratios compared to K/Rb-ratios. Thallium isotopes show only slight changes during orthomagmatic differentiation and the assimilation of crustal material cannot be traced, since the isotopic composition of the average crust…

biologyGeochemistryMineralogyGeologyengineering.materialbiology.organism_classificationPeralkaline rockHydrothermal circulationMagmatic waterAstrophylliteGeochemistry and PetrologySilicate mineralsengineeringIgneous differentiationMetasomatismLileGeologyChemical Geology
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Electrical treeing in EVA-bohemite and EVA-montmorillonite nanocomposites

2009

The present experimental work focuses on the growth of electrical treeing inside different Ethylene-vinyl acetate (EVA) nanocomposites containing Bohemite (an aluminum oxide hydroxide) and Montmorillonite (a phyllosilicate clay mineral) nanoparticles. Bohemite and Montmorillonite particles have different aspect ratios: the first one has a nanometric cube-like symmetry, while the latter has a typical layered structure. The results evidence that the growth of the electrical treeing inside the original polymer can be altered significantly by the dispersion of inorganic nanoparticles.

chemistry.chemical_classificationBoehmiteMaterials scienceNanocompositeNanoparticlePolymerElectrical treeing.chemistry.chemical_compoundMontmorillonitechemistryChemical engineeringClay mineralsDispersion (chemistry)
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Sulfide mineral identification using laser-induced plasma spectroscopy

2003

Sulfide minerals in rock samples were identified with laser-induced plasma spectroscopy (LIPS) in the near vacuum ultraviolet spectral region. Reference spectra of pyrite, pyrrhotite, chalcopyrite, sphalerite, barite, calcite and dolomite were applied to classification of minerals in sulfur-bearing drill core samples. On the basis of the results mineral distributions in the sample were estimated. The potential of the LIPS method for in situ analysis is discussed.

chemistry.chemical_classificationCalciteMaterials scienceMineralSulfideChalcopyriteMechanical EngineeringMineralogyGeneral Chemistryengineering.materialGeotechnical Engineering and Engineering GeologySulfide mineralschemistry.chemical_compoundSphaleritechemistryControl and Systems Engineeringvisual_artengineeringvisual_art.visual_art_mediumPyritePyrrhotiteMinerals Engineering
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Peptide-metal complexes: obtention and role in increasing bioavailability and decreasing the pro-oxidant effect of minerals.

2020

Bioactive peptides derived from food protein sources have been widely studied in the last years, and scientific researchers have been proving their role in human health, beyond their nutritional value. Several bioactivities have been attributed to these peptides, such as immunomodulatory, antimicrobial, antioxidant, antihypertensive, and opioid. Among them, metal-binding capacity has gained prominence. Mineral chelating peptides have shown potential to be applied in food products so as to decrease mineral deficiencies since peptide-metal complexes could enhance their bioavailability. Furthermore, many studies have been investigating their potential to decrease the Fe pro-oxidant effect by f…

chemistry.chemical_classificationGastrointestinal tractMineralsAntioxidantmedicine.medical_treatmentMineral deficiencyBiological AvailabilityPeptideGeneral MedicinePro-oxidantmedicine.diseaseIndustrial and Manufacturing EngineeringHydrolysateBioavailabilitychemistryBiochemistryCoordination ComplexesmedicineHumansChelationPeptidesReactive Oxygen SpeciesFood ScienceCritical reviews in food science and nutrition
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Structural studies of adsorbed protein (betalactoglobulin) on natural clay (montmorillonite)

2014

International audience; In this work, the adsorption of a small globular protein (betalactoglobulin, BLG), on a natural montmorillonite clay (Mt) was investigated in acidic buffer (pH = 3). The combination of different characterization techniques such as zetametry, X-ray diffraction, transmission electronic microscopy, fluorescence and solid state nuclear magnetic resonance spectroscopies shed light on the interaction mechanism between the clay mineral and the proteins. For low BLG concentration, a slight increase of the interlayer spacing of the clay mineral was noticed as well as structural changes of the protein. In contrast, as the concentration of BLG increased, the adsorption led to a…

chemistry.chemical_classificationGlobular proteinGeneral Chemical EngineeringMineralogyGeneral ChemistryExfoliation jointFluorescencechemistry.chemical_compoundAdsorptionMontmorillonitechemistryChemical engineeringSolid-state nuclear magnetic resonance[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyClay mineralsHybrid materialRSC Adv.
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Synthesis and Characterization of the Hybrid Clay-Based Material Montmorillonite-Melanoidin: A Potential Soil Model

2010

The study of the interactions among metals, minerals, and humic substances is essential in understanding the migration of inorganic pollutants in the geosphere. A considerable amount of organic matter in the environment is associated with clay minerals. To understand the role of organic matter in the environment and its association with clay minerals, a hybrid clay-based material (HCM), montmorillonite (STx-1)-melanoidin, was prepared from L-tyrosine and L-glutamic acid by the Maillard reaction. The HCM was characterized by elemental analysis, nuclear magnetic resonance, x-ray photoelectron spectroscopy (XPS), scanning transmission x-ray microscopy (STXM), and thermal analysis. The presence…

chemistry.chemical_classificationMelanoidinSoil Sciencecomplex mixturesSilicatechemistry.chemical_compoundMontmorillonitechemistryX-ray photoelectron spectroscopyChemical engineeringElemental analysisOrganic chemistryOrganic matterThermal analysisClay mineralsSoil Science Society of America Journal
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Chemical evolution of ore-forming brines – Basement leaching, metal provenance, and the redox link between barren and ore-bearing hydrothermal veins.…

2019

Abstract Six mineralogically exemplary barren and mineralized hydrothermal veins (with Pb and Zn ores) of Jurassic-Cretaceous and Cenozoic age in the Schwarzwald mining district, SW Germany were chosen to shed light on the origin of their mineralogical diversity. The selection of the veins was guided by the fact that they represent the largest number of veins in the region, are very well known mineralogically and geochemically, and they provide nice examples of barren and mineralized veins of similar age. Fluid inclusion data from the individual veins overlap implying their diverse mineralogy is not caused by different fluid compositions participating during fluid mixing. LA-ICPMS data of s…

chemistry.chemical_classificationProvenanceMineralization (geology)010504 meteorology & atmospheric sciencesSulfideGeochemistryTrace elementGeology010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationchemistryGeochemistry and PetrologyFluid inclusionsClay mineralsBase metalGeology0105 earth and related environmental sciencesChemical Geology
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Sulfide ore facies, fluid inclusion and sulfur isotope characteristics of the Tappehsorkh Zn-Pb ( ± Ag-Ba) deposit, South Esfahan, Iran

2020

International audience; The stratiform, stratabound Tappehsorkh Zn-Pb (± Ag-Ba) deposit, located in the southeastern part of the Malayer-Esfahan Metallogenic Belt of Iran, formed during Lower Cretaceous back-arc extension. Sulfide mi-neralization occurs within dolostone, black siltstone, and crystal lithic tuff and andesite associated with the Gushfil-Baghabrisham synsedimentary normal fault. Three sulfide ore facies (massive, bedded, and stockwork) occur in the deposit. Sulfide minerals are sphalerite, galena, tetrahedrite and pyrite with minor chalcopyrite and bornite, and gangue minerals are barite, dolomite and quartz. Sulfide mineralization textures are massive, replacement , vein-vein…

chemistry.chemical_classificationStockworkMineralization (geology)SulfideChalcopyriteGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesSulfide mineralsGeophysicsSphaleritechemistryGeochemistry and PetrologyGalenavisual_artengineeringvisual_art.visual_art_mediumBorniteGeology0105 earth and related environmental sciences[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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The influence of weathering processes on labile and stable organic matter in Mediterranean volcanic soils

2008

The relationship and mechanisms among weathering processes, cation fluxes, clay mineralogy, organic matter composition and stability were studied in soils developing on basaltic material in southern Italy (Sicily). The soils were transitions between Phaeozems and Vertisols. Intense losses of the elements Na, Ca and Mg were measured indicating that weathering has occurred over a long period of time. The main weathering processes followed the sequence: amphibole, mica, volcanic glass or if ash was the primary source→smectite→interstratified smectite–kaolinite→kaolinite. Kaolinite formation was strongly related to high Al, Mg and Na losses. The good correlation between oxyhydroxides and kaolin…

chemistry.chemical_classificationWeatheringGeochemistrySoil ScienceWeatheringVertisolMass balanceClay mineralogyVolcanic glass10122 Institute of GeographyFTOrganic matter stabilitychemistryMediterranean soilsIR spectroscopyEnvironmental chemistrySoil waterKaoliniteOrganic matter910 Geography & travelClay minerals1111 Soil ScienceAmphiboleGeology
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