Search results for "petrology"

showing 10 items of 1516 documents

Functionalized halloysite nanotubes for enhanced removal of lead(II) ions from aqueous solutions

2018

In this study, environmental friendly halloysite nanotubes and their amino derivatives were used as adsorbent materials for lead(II) ions. The adsorption ability of both nanomaterials towards Pb2+ ions has been studied in NaClaq, at I = 0.1 mol L−1, in the pH range 3–6. Moreover, the effect of ionic strength on the adsorption process was evaluated at the pH of maximum efficiency of the adsorbent materials. Kinetic and equilibrium experiments were carried out by using the Differential Pulse Anodic Stripping Voltammetry (DP-ASV) technique to check the metal ion concentration in solution after contact with the two adsorbents. Different isotherm and kinetic equations were used to fit the experi…

Halloysite Grafting Lead(II) Adsorption Ionic strengthGeochemistry and PetrologySettore CHIM/01 - Chimica AnaliticaGeologySettore CHIM/06 - Chimica Organica02 engineering and technology010402 general chemistry021001 nanoscience & nanotechnology0210 nano-technology01 natural sciencesSettore CHIM/02 - Chimica Fisica0104 chemical sciencesApplied Clay Science
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Atmospheric turbidity and its spectral extinction

1955

The indices of the wavelength dependency of the haze extinction which were currently determined from measurements of solar radiation and visibility at Mainz, show pronounced seasonal variations. The summer values are in general definitely higher than in winter. There is no connection with the scatter light types of the sky-light or with the meteorological situation.

HazeSpectral extinctionRadiationSeasonalityAtmospheric sciencesmedicine.diseaseWavelengthGeophysicsGeochemistry and PetrologyExtinction (optical mineralogy)ClimatologymedicineEnvironmental scienceAstrophysics::Earth and Planetary AstrophysicsTurbidityVisibilityPhysics::Atmospheric and Oceanic PhysicsGeofisica Pura e Applicata
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Thermo‐Hydro‐Mechanical Model and Caprock Deformation Explain the Onset of an Ongoing Seismo‐Volcanic Unrest

2021

Acknowledgments The authors are grateful to the Editor, Prof. Ben‐Zion Yehuda, and the reviewers: Prof. Micol Todesco and an anonymous reviewer, whose comments and recommendations have significantly improved the quality of this work. The authors acknowledge the financial support of the Petroleum Technology Development Fund (PTDF) Nigeria for this research. The comparison of our models with monitoring data was made possible by the outstanding efforts of the staff at the INGV‐Osservatorio Vesuviano, who provide weekly information about geophysical parameters at the Campanian volcanoes (http://www.ov.ingv.it/ov/en/bollettini/272-campi-flegrei-bollettini-settimanali.html). The authors are parti…

History010504 meteorology & atmospheric sciencesInduced seismicityTechnology developmentSoftware license01 natural sciencesGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyMonitoring dataCaprockEarth and Planetary Sciences (miscellaneous)Forensic engineeringVolcanic unrest0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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A year in the life of an aluminous metapelite xenolith—The role of heating rates, reaction overstep, H2O retention and melt loss

2011

Abstract Xenoliths of aluminous metapelite within the Platreef magmatic rocks of the Bushveld Complex, South Africa, are mineralogically and texturally zoned, with coarse-grained margins rich in acicular corundum, spinel and feldspar and cores rich in finer-grained aluminosilicate and cordierite. Xenoliths exhibiting remarkably similar features occur within other intrusions, suggesting a common origin. Using a single 3 m wide xenolith as a case study, a model is proposed to explain their petrogenesis. Mineral equilibria calculations in the NCKFMASHTO system show that the thermal stability of the solid phases, in particular corundum, is highly sensitive to the quantity of H 2 O retained in t…

HornfelsPartial meltingGeochemistryMetamorphismGeologyCordieriteengineering.materialGeochemistry and PetrologyUltramafic rockengineeringXenolithMaficProtolithGeologyLithos
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A model for Ischia hydrothermal system: Evidences from the chemistry of thermal groundwaters.

2009

Abstract Ischia volcano, in Central Italy, has long been known for its copious surface hydrothermal manifestations, signs of a pervasive circulation of hot fluids in the subsurface. Because of the significant chemical heterogeneity of fumarolic gas discharges and hot spring discharges, evidences of a complex hydrothermal setting, a definite model of fluid circulation at depth is currently unavailable, in spite of the several previous efforts. Here, we report on the chemical and isotopic composition of 120 groundwater samples, collected during several sampling surveys from 2002 to 2007. The acquired data suggest that the composition of surface manifestations reflect contributions from meteor…

Hot springgeographygeography.geographical_feature_categoryischia volcano hydrothermal systemsGeochemistryTrachyteHydrothermal circulationGeophysicsOceanographyVolcanoGeochemistry and PetrologyMagmaMeteoric waterSeawaterGeologyThermal fluids
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2020

Abstract. Fluid flow on different scales is of interest for several Earth science disciplines like petrophysics, hydrogeology and volcanology. To parameterize fluid flow in large-scale numerical simulations (e.g. groundwater and volcanic systems), flow properties on the microscale need to be considered. For this purpose experimental and numerical investigations of flow through porous media over a wide range of porosities are necessary. In the present study we sinter glass bead media with various porosities and measure the permeability experimentally. The microstructure, namely effective porosity and effective specific surface, is investigated using image processing. We determine flow proper…

HydrogeologyMaterials science010504 meteorology & atmospheric sciencesStratigraphyPetrophysicsPaleontologySoil ScienceGeologyMechanics010502 geochemistry & geophysics01 natural sciencesTortuosityEffective porosityPermeability (earth sciences)GeophysicsGeochemistry and PetrologyFluid dynamicsPorosityPorous medium0105 earth and related environmental sciencesEarth-Surface ProcessesSolid Earth
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Evaluation and reformulation of the maximum peak height algorithm (MPH) and application in a hypertrophic lagoon

2017

Hydrology010504 meteorology & atmospheric sciences0208 environmental biotechnology02 engineering and technologyOceanography01 natural sciences020801 environmental engineeringGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceEutrophication0105 earth and related environmental sciencesJournal of Geophysical Research: Oceans
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A new windstorm proxy from lake sediments: A comparison of geological and meteorological data from western Germany for the period 1965–2001

2009

[1] The feasibility of detecting windstorm layers in lake sediments is explored by comparing quartz grain size data from a freeze core obtained from the Schalkenmehrener Maar (Eifel region, western Germany) to recent meteorological wind data. The Schalkenmehrener Maar is appropriate for such a calibration study because the morphological settings of the lake allow the conservation of windstorm layers (in particular, there is no fluvial sediment inflow) and long-term wind measurements are available from nearby stations. The age model for the uppermost 30 cm of the sediment core is based on measurements of 137Cs and 210Pb concentrations. An ultra-high-resolution grain size analysis is performe…

HydrologyAtmospheric ScienceEcologyPaleontologySoil ScienceSedimentForestryStormInflowAquatic ScienceSiltOceanographyProxy (climate)Grain sizeMaarGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyGranulometryEarth and Planetary Sciences (miscellaneous)Physical geographyGeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Modelling fractionation of stable isotopes in stalagmites

2009

Abstract High resolution δ13C and δ18O profiles recorded in precisely dated speleothems are widely used proxies for the climate of the past. Both δ13C and δ18O depend on several climate related effects including meteorological processes, processes occurring in the soil zone above the cave and isotope fractionation processes occurring in the solution layer on the stalagmite surface. Here we model the latter using a stalagmite isotope and growth model and determine the relationship between the stable isotope values in speleothem calcite and cave parameters, such as temperature, drip interval, water p CO 2 and a mixing coefficient describing mixing processes between the solution layer and the …

HydrologyCalcitegeographygeography.geographical_feature_categoryIsotopeStable isotope ratioδ18OSpeleothemMineralogyStalagmiteFractionationchemistry.chemical_compoundIsotope fractionationchemistryGeochemistry and PetrologyGeologyGeochimica et Cosmochimica Acta
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Assessment of nitrate contamination risk: The Italian experience

2009

16 páginas, 19 figuras, 10 tablas.-- El PDF es el manuscrito aceptado para su publicación.-- et al.

HydrologyDenitrificationbusiness.industryContaminationNitrateSoil qualityHazardGroundwater contaminationGroundwater vulnerabilitychemistry.chemical_compoundNitratechemistryItalyGeochemistry and PetrologyAgricultureEnvironmental scienceEconomic GeologyWater resource managementRisk assessmentbusinessGroundwaterRisk assessment
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