Search results for " FT-IR"

showing 10 items of 18 documents

Differences of stabilized organic carbon fractions and microbiological activity along Mediterranean Vertisols and Alfisols profiles

2010

This study examined the chemical and structural properties of humic substances and microbiological activity in order to verify differences in carbon dynamics along soil profiles in two Vertisols (Typic Haploxerert and Xeric Epiaquert) and two Alfisols (Mollic Haploxeralf and Ultic Haploxeralf) developed under Mediterranean climate in Italy. Humification parameters, thermal methods, including differential scanning calorimetry (DSC) and thermogravimetry (TG), together with Fourier transform infrared (FT-IR) and fluorescence spectroscopies were used to characterize humic acids (HA). Microbiological activity of soils was assessed by basal respiration, metabolic quotient (qCO2) and Cmic:Corg rat…

Total organic carbonChemistrySoil ScienceMineralogyVertisolHumusThermogravimetrySettore AGR/14 - PedologiaSoil pHEnvironmental chemistrySoil waterAlfisolSoil horizonVertisols Alfisols Microbial indices DSC TG FT-IR Fluorescence spectra Humic acidsGeoderma
researchProduct

Preparation and XAFS studies of organotin(IV) complexes with adenosine and related compounds and calf thymus DNA

2007

Complexes of adenosine and related compounds (adenosine-5’-monophosphate, adenosine-5’-triphosphate and pyridoxal-5-phosphate) with Bu2SnO and/or BuSnCl2 were prepared in the solid state. The compositions of the complexes were determined by standard analytical methods. It was found that the complexes contain the organotin(IV) moiety and the ligand in a ratio of 1:1. The FT-IR spectra demonstrated that Bu2SnO reacts with the D-ribose moiety of the ligands, while Bu2SnCl2 is coordinated to the deprotonated phosphate group. The basic part of the ligands does not participate directly in complex formation. Comparison of the experimental Mossbauer Δ (quadrupole splitting) values with those calcul…

XAFS organotin(IV) DNA Mossbauer FT-IRExtended X-ray absorption fine structureChemistryLigandStereochemistryHealth Toxicology and MutagenesisPublic Health Environmental and Occupational HealthQuadrupole splittingPollutionMedicinal chemistryAnalytical ChemistryX-ray absorption fine structureBond lengthDeprotonationNuclear Energy and EngineeringSettore CHIM/03 - Chimica Generale E InorganicaMössbauer spectroscopyMoietyRadiology Nuclear Medicine and imagingSpectroscopyJournal of Radioanalytical and Nuclear Chemistry
researchProduct

Spectroscopic and Structural Investigation of the Confinement of D and L Dimethyl Tartrate in Lecithin Reverse Micelles

2009

The confinement of D and L dimethyl tartrate in lecithin reverse micelles dispersed in cyclohexane has been investigated by FT-IR, polarimetry, electronic and vibrational circular dichroism (ECD and VCD), 1H NMR, and small-angle X-ray scattering (SAXS). Measurements have been performed at room temperature as a function of the solubilizate-to-surfactant molar ratio (R) at fixed lecithin concentration. The analysis of experimental data indicates that the dimethyl tartrate molecules are solubilized within reverse micelles in proximity to the surfactant head groups in the same way for the D and L forms. The encapsulation of dimethyl tatrate within lecithin reverse micelles involves changes in i…

lecithin dimethyl tartrate FT-IR polarimetry circular dichroism NMR SAXSfood.ingredientCyclohexanemicellesTartrateLecithinMicellePolyethylene Glycolschemistry.chemical_compoundfoodLecithinsMaterials ChemistryOrganic chemistryPhysical and Theoretical ChemistryTartratesModels StatisticalDose-Response Relationship DrugChemistry PhysicalViscosityChemistrySmall-angle X-ray scatteringTemperaturetechnology industry and agricultureElasticitySurfaces Coatings and FilmslecithinModels ChemicalSpectrophotometryVibrational circular dichroismMicellar solutionsPhosphatidylcholinesProton NMRPhysical chemistrylipids (amino acids peptides and proteins)Rheologydimethyl tartrate
researchProduct

Caratterizzazione di sostanza organica disciolta mediante rilassometria NMR in modalità fast field cycling

2009

Settore AGR/13 - Chimica AgrariaNMR NMRD FT-IR DOM
researchProduct

Il cammino del sole, gli spazi del giorno. Piano urbanistico del comune di Grammichele (CT) su lastra di ardesia dipinta

2008

Metodi di pulitura gelFluorescenza ultraviolettaSpettroscopia FT-IR
researchProduct

MULTIDISCIPLINARY STUDY FOR THE DATING AND THE RESTORATION OF THE SAN VITO WOODEN PULPIT OF MUSEO DIOCESANO OF PALERMO

2017

The aim of the present research is to investigate the execution techniques of San Vito wooden pulpit in the Museo Diocesano of Palermo and to provide helpful information to dating it in addition to technical, historical and artistic evaluations. In particular, this paper describes the application of analytical techniques (imaging diagnostics techniques, Scanning Electron Microscopy coupled with X-ray Energy Dispersive spectroscopy Scanning Electron Microscopy-Energy Dispersive X-ray Spectroscopy and Fourier Transform Infrared Spectroscopy) to better understand the pulpit characteristics, both support and decoration, useful to plan and perform the correct restoration.

Wooden pulpit SEM-EDS FT-IR spectroscopy Museo Diocesano of Palermo
researchProduct

Volatiles in pantellerite magmas: A case study of the Green Tuff Plinian eruption (Island of Pantelleria, Italy)

2013

Abstract The Green Tuff (GT) Plinian eruption, the largest in magnitude at Pantelleria, erupted 3 to 7 km3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2O content in the pantellerite melt. Microanalytical methods were used to determine major element, Cl, F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt %, i.e. much higher than the 1.4 wt % of earlier published studies. The…

LavaSettore GEO/07 - Petrologia E PetrografiaGeochemistryTrachyteMagma chamberStrombolian eruptionGeophysicsEffusive eruptionGeochemistry and PetrologyPumiceMagmaThe Green Tuff (GT) Plinian eruption the largest in magnitude at Pantelleria erupted 3 to 7 km 3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2Ocontent in the pantellerite melt. Microanalytical methods were used to determine major element Cl F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt % i.e. much higher than the 1.4 wt % of earlier published studies. The chlorine content is constant at about 1 wt %. Combined Cl and H2O data were used to estimate a confining pressure of about 50 MPa (depth around 2-3 km) for the GT magma chamber. The chamber was characterized by a compositional zoning with a dominant pantellerite overlying a trachyte magma. Soon after the GT eruption intra-caldera volcanism was dominated by the eruption of voluminous trachyte lavaflows while pantellerite melt production resumed after about 20 ka with numerous low-volume mildly explosive (Strombolian) to effusive eruptions. Comparison with data from the literature reveals that despite the differentexplosivity the post-caldera Strombolian eruptions and the GT Plinian eruption were fed by pantelleritic magmas with similar water contents. Chlorine and CO2contents suggest that the young magma reservoirs feeding the Strombolian to effusive activity were deeper (h≥4.5 km) than the much larger (based on erupted volumes) magma chamber which fed the GT eruptionGeologyMelt inclusionsJournal of Volcanology and Geothermal Research
researchProduct

Petrographic and spectroscopic (FT-IR) study of Western Mediterranean obsidians geological sources and of a lithic collection from Ustica Island (Sic…

2019

I n this study we applied petrochemical methods (SEM-EDS; FT-IR) in order to characterize a group of obsidian flakes collected at Ustica island (Sicily). Despite the absence of obsidian geological outcrops, a lot of obsidian fragments still emerging from the lands of Ustica testify that the island was a major import center of obsidian during the prehistory. On this island, there are some prehistoric settlements, dated from the Neolithic to the Middle Bronze Age (6000- 1200 BC), in which the use of obsidian continued until the beginning of metals age. Our study includes: i) Macroscopic and microscopic optical observations, which allowed selecting 18 obsidian flakes (starting from 50 obsidian…

Mediterranean climateObsidian Petrographic study FT-IR Mediterranean obsidians Ustica IslandOutcropFlakeSettore GEO/07 - Petrologia E PetrografiaGeochemistry010502 geochemistry & geophysics01 natural sciencesPrehistoryPetrographyGeophysicsBronze AgeGeology0105 earth and related environmental sciencesAnnals of Geophysics
researchProduct

Interaction of a Recombinant Prion Protein with Organo-Mineral Complexes as Assessed by FT-IR and CPMAS 13C NMR Analysis

2010

Prion proteins are considered as the main agents for the Transmissible Spongiform Encephalopathies (TSE). The misfolded form, PrP Sc , which is also indicated as the etiological agent for TSE, exhibits high resistance to degradation in environmental processes. Soil contamination by prion proteins is a real environmental issue since contaminated soils can become potential reservoir and diffuser for TSE infectivity. In this work, the interaction of prion protein with organo- mineral complexes was studied by using a recombinant non pathogenic prion protein and a model soil system. This latter was represented by a soil manganese mineral coated with polymerized catechol. FT-IR spectra showed ami…

chemistry.chemical_classificationCatecholBirnessiteStereochemistryanimal diseasesSoil Organo-Mineral ComplexeSettore AGR/13 - Chimica Agrariachemistry.chemical_elementNuclear magnetic resonance spectroscopyManganeseCarbon-13 NMRnervous system diseaseslaw.inventionFT-IRTSE diseasechemistry.chemical_compoundPrion proteinchemistryBiochemistryPolymerizationlawCPMAS 13C NMRRecombinant DNAPrion protein TSE diseases Soil Organo-Mineral Complexes FT-IR CPMAS 13C NMRAlkylThe Open Magnetic Resonance Journal
researchProduct

Biostimulant Potential of Humic Acids Extracted From an Amendment Obtained via Combination of Olive Mill Wastewaters (OMW) and a Pre-treated Organic …

2018

Olive mill wastewaters (OMW) detain contain significant levels of phenolic compounds with antimicrobial/phytotoxic activity and high amounts of undecomposed organic matter that may a high pollutant load that exerts negative effects on soil biology because of significant levels in phenolic compounds with antimicrobial/phytotoxic activity and limited biodegradability, and high amounts of undecomposed organic matter. Among OMW detoxification techniques, those focusing on oxidative degradation of phenolic compounds are relevant those focusing on oxidative degradation of phenolic compounds to reduce their toxicity. The composting (bio-oxidation) process in particular, exploits exothermic oxidati…

amendmentsNitrogen assimilationAmendmentPlant Science010501 environmental scienceslcsh:Plant cultureNitrate reductase01 natural sciencesHumic acidOrganic matterlcsh:SB1-1110Original Research0105 earth and related environmental scienceschemistry.chemical_classificationnitrogen assimilation04 agricultural and veterinary sciencesglycolysisBiodegradationbio-oxidationZea Mays L.humic acidsFT-IRbiostimulantsAmendments; Bio-oxidation; Biostimulants; FT-IR; Glycolysis; Humic acids; Nitrogen assimilation; Zea mays L; Plant SciencechemistryEnvironmental chemistry040103 agronomy & agriculture0401 agriculture forestry and fisheriesPhytotoxicityZea mays LPlant nutritionFrontiers in Plant Science
researchProduct