Search results for " Mineralogy"

showing 9 items of 69 documents

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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Die chemische molekulargewichtsbestimmung von polystyrol mit hilfe colorimetrisch bestimmbarer endgruppen. III. Mitt.

1964

Ein mit dem Diacylperoxyd der 3-Benzolazo-benzoesare hergestelltes Polystyrol enthalt Endgruppen, die durch Extinktionsmessungen bei 442, 319 und 262,5 mμ bestimmt wurden. Es wurde eine Extinktionszahl-Molekulargewichts-Beziehung aufgestellt, die dem bekannten VAN'T HOFFschen Gesetz entspricht. Falls die Zahl der charakteristisch absorbierenden Endgruppen je Makromolekul unbekannt ist, wurden fur die experimentelle Bestimmung eines Mindestmolekulargewichts mehrere voneinander unabhangige Gleichungen gefunden. Viskosimetrisch und uber Extinktionsmessungen bestimmte Molekulargewichte wurden verglichen. Polystyrene, prepared by means of a diacylperoxide of the 3-benzeneazobenzoic acid, contain…

chemistry.chemical_compoundChemistryExtinction (optical mineralogy)Polymer chemistryAnalytical chemistryOsmotic pressurePolystyreneDie Makromolekulare Chemie
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Hafnium-neodymium isotope evidence for enhanced weathering and tectonic-climate interactions during the Late Cretaceous

2022

<p>Over million-year timescale the carbon cycle evolution is driven by mantle CO<sub>2</sub> degassing (source) and by continental weathering that drawdowns atmospheric CO<sub>2</sub> through silicate weathering reactions (sink). Based on a novel geochemical proxy of chemical weathering intensity (i.e. using measurements of Hf and Nd isotope ratios in clay-size fractions of sediments) and clay mineralogy, we discuss the links between tectonic, continental weathering and climate evolution during the late Cretaceous. That period records the very first step of the last greenhouse to icehouse transition and is concomitant to …

clay mineralogy[SDU] Sciences of the Universe [physics]Hflate CretaceousupliftpaleoclimateweatheringNd isotope
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Quantitative identification, distribution and source apportionment of anthropogenic trace metals in marine sediment of Milazzo gulf (N-E Sicily): pre…

2009

coastal sea sedimentbulk mineralogybenthic foraminiferapollutiontrace metalgranulometry
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Geomorphological, chemical and physical study of “calanchi” landforms in NW Sicily (southern Italy)

2012

Abstract This work deals with an integrated geomorphological and chemical–physical study of “calanchi” landforms in two sites (Ottosalme and Catalfimo) of NW Sicily (southern Italy), developed on dominant silty-clay deposits. The calanchi fronts are characterized by different morphological features and dominant geomorphic processes. Sharp knife-edged ridges and concentrated water runoff dominate at Ottosalme, and smoother landforms affected by mass movements (mud flows and translational slides) prevail at Catalfimo. We focused on some geochemical and physical parameters such as pH , total dissolved salts, sodium adsorption ratio ( SAR ), porosity, plastic and liquid limits as possible cause…

geographyAbsorption of watergeography.geographical_feature_categoryLandformSettore GEO/04 - Geografia Fisica E GeomorfologiaCrustLandslideCalanchi fronts Chemical and physical properties SAR Microforms MineralogySodium adsorption ratioPorositySurface runoffSaturation (chemistry)GeomorphologyGeologyEarth-Surface ProcessesGeomorphology
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Kalcīts un tā veidošanās apstākļi Franas stāva smilšakmeņos un dolomītos Latvijā

2019

Maģistra darbā “Kalcīts un tā veidošanās apstākļi Franas stāva smilšakmeņos un dolomītos Latvijā” raksturotas kalcīta fizikālās īpašības, ķīmiskais sastāvs un veidošanās apstākļi. Pētījumi veikti 16 Amatas, Pļaviņu, Daugavas un Stipinu svītas atradnēs un atsegumos. Dokumentēti ģeoloģiskie griezumi, pētītas kalcīta fluorescences izpausmes un citas fizikālās īpašības, attiecības ar smilšakmens un dolomīta komponentiem plānslīpējumos, noteikts kalcīta ķīmiskais sastāvs un oglekļa stabilo izotopu attiecības. Secināts, ka kalcīts Amatas svītas smilšakmeņos un Pļaviņu, Daugavas un Stipinu svītas dolomītos kristalizējies līdzīgos apstākļos – no atmosfēras izcelsmes pazemes ūdeņiem sauszemes apstāk…

mineraloģija; mineralogykristalizācija; crystallisationĢeoloģijaķīmiskais sastāvs; chemical compositionpēcsedimentācijas izmaiņas; diagenesisδ13C analīze; δ13C analysis
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Kalcīts un tā veidošanās apstākļi augšējā devona Daugavas svītas dolomītos Latvijas centrālajā un austrumu daļā

2017

Bakalaura darbā “Kalcīts un tā veidošanās apstākļi augšējā devona Daugavas svītas dolomītos Latvijas centrālajā un austrumu daļā” ir raksturotas minerāla kalcīta fizikālās īpašības, mikroelementu saturs un veidošanās apstākļi. Pētījumi veikti 8 dolomīta atradnēs; ģeoloģiskajā griezumā un atradņu teritorijā salīdzinātas kalcīta īpašības. Testētas kalcīta fluorescences izpausmes, pētīti plānslīpējumi, raksturoti kalcītā sastopamie mikroelementi un oglekļa stabilo izotopu attiecības tajā. Secināts, ka kalcīts kristalizējies no atmosfēras ūdeņiem sauszemes apstākļos. Šis minerāls veidojies paleokarsta procesa beigu stadijā pēc iegruvumu izveidošanās. Atslēgas vārdi: mineraloģija, paleokarsts, f…

mineraloģija; mineralogyĢeoloģijafluorescence; fluorescencepaleokarsts; palaeokarstmikroelementi; minor elementsδ13C analīze; δ13C analysis
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Solar radiative effects of a Saharan dust plume observed during SAMUM assuming spheroidal model particles

2011

The solar optical properties of Saharan mineral dust observed during the Saharan Mineral Dust Experiment (SAMUM) were explored based on measured size-number distributions and chemical composition. The size-resolved complex refractive index of the dust was derived with real parts of 1.51–1.55 and imaginary parts of 0.0008–0.006 at 550 nm wavelength. At this spectral range a single scattering albedo ω o and an asymmetry parameter g of about 0.8 were derived. These values were largely determined by the presence of coarse particles. Backscatter coefficients and lidar ratios calculated with Mie theory (spherical particles) were not found to be in agreement with independently measured lidar data.…

optical propertiesAtmospheric Scienceradiative transfer simulationsMaterials sciencespectral radiative flux densities010504 meteorology & atmospheric sciencesSingle-scattering albedospheroidal aerosol particlesMie scatteringAtmosphärische SpurenstoffeMineralogy010501 environmental sciencesMineral dustAtmosphärenprozessoren01 natural sciencesComputational physicsSaharan mineral dustExtinction (optical mineralogy)Radiative transferParticlescattering databaseParticle sizeAstrophysics::Earth and Planetary AstrophysicsOptical depth0105 earth and related environmental sciencesTellus B
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Italica (Seville, Spain): use of local marble in Augustan age

2010

This study concerns 51 marble finds made of “Cipollino verde” coming from the ancient city of Italica (north of the modern city of Santiponce, 9 km NW of Seville, Spain), the earliest Roman settlement in Spain, founded in 206 B.C. The aim of this work was to determine their provenance from Greek and Italian quarries or from local quarries worked in the Iberian Peninsula. Thin-section optical microscopy, X-ray powder diffraction, bulk rock chemistry and O, C and Sr stable isotope analyses were carried out. Results were compared with literature data on “Cipollino verde” marbles quarried in southern Euboea (Greece), Apuan Alps (Italy), Almería, Extremoz, Seville (Spain) and Évora (Portugal). T…

“Cipollino verde” marble; mineralogy; petrography; geochemistry; stable isotopes; Italica; Spainarchaeometry; cipollino verde marble; mineralogy; stable isotopes; spain; italica; roman age; clay samples; pottery; viminacium; petrography; cipollino verde" marble; geochemistrySpainstable isotope“Cipollino verde” marblemineralogyItalicaSettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.petrographygeochemistry
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