Search results for "Geology"

showing 10 items of 6012 documents

Enhanced Skin Permeation of Estradiol by Dimethyl Sulfoxide Containing Transdermal Patches.

2021

Dimethyl sulfoxide is a well-known and widely used dermal penetration enhancer. Its incorporation in transdermal patches would be highly desirable

chemistry.chemical_classificationRecrystallization (geology)Stability testintegumentary systemDimethyl sulfoxideTransdermal patchdimethyl sulfoxidelcsh:RS1-441Pharmaceutical SciencePolymerPermeationtransdermal patchestradiol permeationenhanced skin permeationArticlelcsh:Pharmacy and materia medicaSolventchemistry.chemical_compoundchemistryrecrystallization inhibitionTransdermalNuclear chemistryPharmaceutics
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1985

Proposition d'une methode qui utilise l'information contenue dans la relation entre la vitesse de cisaillement et la viscosite. Solutions de polystyrene dans la trans-decaline

chemistry.chemical_classificationSolvent systemShear (geology)chemistryChemical engineeringPolymer chemistryPolymerDissolutionDie Makromolekulare Chemie, Rapid Communications
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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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Environmental impact of mining activities on the Hermioni area, Greece

1993

Publisher Summary This chapter investigates the environmental impact of mining activities in the Hermioni area, Greece, including the offshore area. A chemical analysis of sediments associated with diabase lavas in the Hermioni mine area has shown significant enrichments in Fe, Mn, Zn, Cu, and As relative to normal pelagic clays. Marked geographic compositional variations within the Hermioni area have been observed, the highest metal enrichments found at Baroutospelia. Mineralogically the Fe–Mn sediments contain hematite, quartz, and minor amounts of illite, smectites, and feldspars. A chemical analysis of sulfide ore samples showed that the Hermioni ores are Cu-rich pyrites, always contain…

chemistry.chemical_classificationSulfideMineralogyHematiteengineering.materialHydrothermal circulationchemistrySeafloor massive sulfide depositsvisual_artIllitevisual_art.visual_art_mediumengineeringQuartzChemical compositionGeologyEnvironmental impact of mining
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A green route to synthesize poly(lactic acid)-based macromonomers in scCO2 for biodegradable nanoparticle production

2014

Poly(lactic acid)-based macromonomers, aimed at biomedical applications and with well-defined average chain length, are produced through catalytic ring-opening polymerization of L,L-lactide co-initiated by a co-monomer bearing a double bond. Reactions have been carried out in supercritical carbon dioxide (scCO2) at different temperatures, ranging from 90 to 130 °C. The resulting oligomers have been characterized by different techniques (1H-NMR, 13CNMR, MALDI-TOF, ESI, GPC, FT-IR, TGA), which show that oligomers with narrower molecular weight distribution are produced at the lowest temperature. In addition, a significant reduction of the impact of the secondary reactions has been found at th…

chemistry.chemical_classificationSupercritical carbon dioxideDouble bondGeneral Chemical EngineeringGeneral ChemistryMacromonomerCatalysisLactic acidchemistry.chemical_compoundchemistryChemical engineeringPolymerizationPolymer chemistryMolar mass distributionDegradation (geology)
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Shear and nonisothermal elongational characterization of a liquid crystalline polymer

1989

A commercial liquid crystalline polymer (LCP) sample was characterized both in shear and in nonisothermal elongational flow over a wide range of temperatures (240–350°C). The LCP sample employed was a copolyesteramide of 2,6 hydroxynaphthoic acid, terephthalic acid, and aminophenol manufactured by Celanese and commercially known as Vectra B950. The viscosity decreases dramatically at temperatures above the crystal-nematic transition of the polymer. At lower temperatures, the extrusion of the sample is mainly due to plastic flow. Die-swell values are very small and contraction of the extrudate is also revealed, but the sample shows high elasticity. The polymer is not spinnable at very low te…

chemistry.chemical_classificationTerephthalic acidMaterials sciencePolymers and PlasticsLiquid crystallineGeneral ChemistryPolymerDie swellPlasticitychemistry.chemical_compoundShear (geology)chemistryMaterials ChemistryExtrusionComposite materialPolymer Engineering and Science
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Influence of inheritance and pedogenesis on heavy metal distribution in soils of Sicily, Italy

2000

Abstract The recognition of the potential health hazards associated with heavy metals has focused attention on the levels and behaviours of these elements both in natural and contaminated environments. Various soil types developed from different parent materials in Sicily, Italy, have been analysed in order to compare heavy metal distribution under different geopedological conditions. Total metal concentrations, metal partitioning and distribution profiles are discussed in relation to the inheritance factor and pedogenic processes. Parent material composition largely influences the contents of heavy metals in most of the analysed soils, mainly differentiating pedons for their metal concentr…

chemistry.chemical_classificationTopsoilInceptisolSoil ScienceSoil scienceVertisolPedogenesischemistryEnvironmental chemistryCation-exchange capacitySoil horizonOrganic matterEntisolGeologyGeoderma
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Pedogenesis in disturbed alpine soils (NW Italy)

2002

In alpine environments, natural or man-induced disturbances are fairly common and acknowledged as determining factors in pedogenesis and soil distribution. We have selected a representative alpine valley in the Italian Northwestern Alps to evaluate the effects of perturbations of different intensity and frequency on soil development and weathering during the last few centuries. In order of decreasing disturbances, we selected: (i) an active avalanche shoot; (ii) a man-built terrace; (iii) a park-like forest; and (iv) a coniferous forest. In the two most disturbed sites, independently of the intensity and frequency of the disturbances, the active pedogenic processes are restricted to the top…

chemistry.chemical_classificationTopsoilSoil ScienceSoil scienceWeatheringVegetationengineering.materialPodzolPedogenesischemistryIlliteengineeringSoil horizonOrganic matterGeologyGeoderma
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Effect of climate and vegetation on soil organic carbon, humus fractions, allophanes, imogolite, kaolinite, and oxyhydroxides in volcanic soils of Et…

2007

A soil sequence along an elevational gradient ranging from subtropical to subalpine climate zones in the Etna region (Sicily, southern Italy) was investigated with respect to organic C, kaolinite, and crystalline to noncrystalline Al and Fe phases. Special emphasis was given to the stabilization of soil organic carbon (SOC) and its interaction with the inorganic phases. The soils were variations of Vitric Andosols that developed on a trachy-basaltic lava flow with an age of 15,000 years. Two main vegetation systems dominated the sites: at the lower sites, it was mainly maquis vegetation and, at the higher elevated sites, predominantly coniferous forest. The concentration of SOC in the topso…

chemistry.chemical_classificationTopsoilSoil organic matterSoil ScienceSoil scienceSoil carbonHumusAndosolSoil organic matter kaolinite fulvic and humid acidschemistrySoil waterVegetation typeOrganic matterGeology
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Factors influencing carbon decomposition of topsoils from the Brazilian Amazon Basin

1999

The influence of texture and local climate, especially precipitation, on C decomposition was evaluated in topsoils under forest and pastures at different sites located in the western, central, and eastern Brazilian Amazon Basin. Independent of the geographical location and vegetation cover, C decomposition was lower in topsoils of fine texture with a sand/clay ratio of less than 1, compared to topsoils of coarse a texture with a sand/clay ratio ranging from 2 to 8. In the former, the low sand/clay ratio appears to reduce C decomposition. In the latter, besides the effect of the high sand/clay ratio, the local climate, especially the annual precipitation, seems to play an important role in c…

chemistry.chemical_classificationTopsoil[SDV]Life Sciences [q-bio]Soil biologySoil ScienceSoil scienceRainforestMicrobiologyTexture (geology)Soil qualityCarbon cyclechemistry[SDE]Environmental SciencesEnvironmental scienceOrganic matterPrecipitationAgronomy and Crop ScienceBiology and Fertility of Soils
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