Search results for "Sediment"

showing 10 items of 1648 documents

Nature and origin of fault-controlled fluid seepage across the Maltese Islands

2018

The Maltese Islands are intersected by two major fault systems associated with two diverse rifting episodes affect the islands. The first and most widespread system is Early Miocene to mid-Pliocene in age, and consists of faults that are orientated ENE-WSW. The most distinct of these faults is the Great Fault (known also as the Victoria Lines Fault). The younger system of faults (Late Miocene-Early Pliocene) is still active and consists of faults striking NW to SE that often cross-cut the first generation of faults. The most extensive of these faults is the Maghlaq Fault, located along the southern coastline of the Maltese Islands.

Environmental managementSettore GEO/02 - Geologia Stratigrafica E SedimentologicaHydrology -- MaltaGeotechnical engineering -- MaltaSeepage faultHydrogeology -- Malta
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Fractionation of mercury in sediments during draining of Augusta (Italy) coastal area by modified Tessier method

2013

Abstract A modified Tessier method was applied to sediments dredged from Augusta (Italy) coastal area with the purpose of establishing the amount and the forms in which mercury is present in the different sediment fractions. The mercury fractionation was made by measuring the concentration of the metal ion on the solutions and directly on the sediment fractions obtained by sequential extraction. The measurements on the solutions as well as that on the solid fractions were carried out by using a Direct Mercury Analyser, DMA 80. This new instrument does not require sample preparation, and gives results comparable to those obtained with CV-AAS and ICP-MS and few minutes are necessary for each …

Environmental remediationAugustaAnalyserRemediationSedimentchemistry.chemical_elementFractionationSettore CHIM/12 - Chimica Dell'Ambiente E Dei Beni CulturaliAnalytical ChemistryMercury (element)SedimentsCertified reference materialschemistryMercury(II) ionEnvironmental chemistryEnvironmental scienceSettore CHIM/01 - Chimica AnaliticaSample preparationFractionationSpectroscopyMicrochemical Journal
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Dynamic evaluation of aggregation and agglutination of red blood cells.

1984

Viscoelastic evaluation of aggregation and agglutination of red blood cells was attempted. A concentric double cylinder viscoelastometer was used for determining the dynamic rigidity modulus and loss modulus of blood sample. The dynamic rigidity modulus of horse blood were measured over a wide range of hematocrit. The relation between the viscoelastic behavior and the erythrocyte sedimentation was examined. The change in the amount of surface charge of enzyme treated red blood cells was qualitatively estimated from the measurements of dynamic viscoelasticity of red blood cells suspension with added poly-L-lysine. The dynamic rigidity modulus of red blood cells agglutinated by adding lectin …

Erythrocyte AggregationErythrocytesPhysiologyModulusNeuraminidaseRigidity (psychology)Blood SedimentationHematocritViscoelasticityPhysiology (medical)Dynamic modulusmedicineConcanavalin AAnimalsHumansPolylysineTrypsinSurface chargeHorsesmedicine.diagnostic_testbiologyChemistryBlood ViscosityElasticityAgglutination (biology)Concanavalin Abiology.proteinBiophysicsCattleRheologyBiorheology. Supplement : the official journal of the International Society of Biorheology
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Hunting for valuables from landfills and assessing their market opportunities A case study with Kudjape landfill in Estonia

2017

Landfill mining is an alternative technology that merges the ideas of material recycling and sustainable waste management. This paper reports a case study to estimate the value of landfilled materials and their respective market opportunities, based on a full-scale landfill mining project in Estonia. During the project, a dump site (Kudjape, Estonia) was excavated with the main objectives of extracting soil-like final cover material with the function of methane degradation. In total, about 57,777 m3 of waste was processed, particularly the uppermost 10-year layer of waste. Manual sorting was performed in four test pits to determine the detailed composition of wastes. 11,610 kg of waste was…

EstoniaEnvironmental EngineeringWaste management020209 energySorting (sediment)Extraction (chemistry)Environmental engineeringFraction (chemistry)02 engineering and technology010501 environmental sciences01 natural sciencesPollutionMiningWaste Disposal FacilitiesWaste Management0202 electrical engineering electronic engineering information engineeringEnvironmental scienceRecyclingLandfill miningChemical compositionRefuse-derived fuelFinal cover0105 earth and related environmental sciencesAlternative technologyWaste Management & Research: The Journal for a Sustainable Circular Economy
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Sample details on OSL data for aeolian sediments in north-eastern part of European Sand Belt

2019

A compilation of previously published and unpublished absolute age (OSL and TL) determinations of aeolian sediments from the north-eastern part of European Sand Belt. Contains age, error, sampling depth, location etc. and a reference to data source. Coordinates of sampling locations for contemporary publications are taken from field observations (GPS), but older ones - published schematic maps. Data set is created according to schema of DATED-1 database (https://doi.org/10.1594/PANGAEA.848117).

EstoniaIdentificationReference sourceLocationStratigraphySiteDEPTH sediment/rockAge commentAnalytical methodduneAGETypeELEVATIONLONGITUDESample code/labelSediment typeMultiple investigationsEvent labelCommentSample code labelLithuaniaAge errorerrorLatviasediment rockBalticsDEPTHEarth System ResearchLATITUDEabsolute ageReference/source
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Petrography and decay of a marly limestone in the cloister of a medieval cathedral in Sicily

2004

This paper deals with a significant process of decohesion of a marly limestone, taking place in the cloister of the medieval Cathedral of Cefalu, a pleasant town on the northern coast of Sicily. After desalination with deionised water and consolidation with ethyl silicate, the decay of the stone became faster. The aim of our study is to characterise the stony material and investigate the observed decay phenomena. The stone, that is a poor building material indeed, is characterised by means of petrographical, chemical and physical analyses on samples taken from the monument. Furthermore, experimental tests are performed in the laboratory in order to highlight the causes of incompatibility be…

Ethyl silicateCloisterGeneral EngineeringWeatheringDecayArchaeologyPetrographyMining engineeringEarth and Planetary Sciences (miscellaneous)CefalùGeneral Earth and Planetary SciencesEnvironmental ChemistryCarbonate rockSedimentary rockMarly limestoneSicilyGeologyGeneral Environmental ScienceWater Science and TechnologyEnvironmental Geology
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Depositional environment and biofacies characterisation of the Triassic (Carnian to Rhaetian) carbonate succession of Punta Bassano (Marettimo Island…

2007

AThe aims of this study are to reconstruct the geological setting of the Punta Bassano series (Marettimo Island, Egadi Archipelago, western Sicily) and its palaeogeographic evolution. The reference section for the Upper Triassic of Marettimo shows an alternation of marl and limestone beds together with brecciated levels. The limestones are both homogeneous mudstones with evaporite pseudomorphs and laminated with fenestrae. Foraminiferal, palynomorph, and ostracod associations constrain the Punta Bassano sequence to the Carnian-Rhaetian interval. The Punta Bassano succession represents a shallow inner ramp, ranging from open-marine environment with good water circulation to lagoonal and peri…

EvaporiteStratigraphySedimentary depositional environmentPaleontologyForaminifersOstracodMarlddc:550SedimentologyUpper Triassic Sedimentology Foraminifers Ostracods Palynomorphs Palaeogeography Sicily Marettimo IslandSicilygeographygeography.geographical_feature_categorybiologyOstracodsPaleontologyMarettimo IslandGeologyPalynomorphsSedimentologybiology.organism_classificationTectonicsFaciesArchipelagoUpper TriassicPalaeogeographyGeology
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The architecture and Neogene to Recent evolution of the W Calabrian continental margin: an upper plate perspective to the Ionian subduction system (C…

2010

The western Calabria continental margin forms the transition between the Pliocene to Recent Marsili spreading center and continental Calabria, all parts of the upper plate of the Ionian subduction zone. Integrating high-resolution and crustal seismic images constrained by gravity modeling, we provide a detailed reconstruction of the architecture of the margin and develop a new scheme for its Miocene to present evolution. This time span encompasses the continent-continent collision between Africa and Eurasia, subsequent orogenic collapse and rifting apart between the two continental masses, and the Pliocene to Recent emplacement of oceanic crust in the Vavilov and Marsili basins. The crust o…

Extensional faultSubductionSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleCrustW Calabria continental marginNeogeneGeophysicsContinental marginGeochemistry and PetrologyOceanic crustThrust faultTyrrhenian BasinSynclineIonian subduction zoneSeismologyGeology
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Evolution of depositional settings in the Torrey area during the Smithian (Early Triassic, Utah, USA) and their significance for the biotic recovery

2015

This work focuses on well-exposed Lower Triassic sedimentary rocks in the area of Torrey (south-central Utah, USA). The studied Smithian deposits record a large-scale third-order sea-level cycle, which permits a detailed reconstruction of the evolution of depositional settings. During the middle Smithian, peritidal microbial limestones associated with a rather low-diversity benthic fauna were deposited seaward of the tidal flat siliciclastic red beds. Associated with siliceous sponges, microbial limestones formed small m-scale patch reefs. During the late middle to late Smithian interval, the sedimentary system is characterized by tidal flat dolostones of an interior platform, ooid-bioclast…

Extinction event010506 paleontologyRed bedsgeographygeography.geographical_feature_categoryEarly TriassicGeology010502 geochemistry & geophysics01 natural sciencesSedimentary depositional environmentPaleontologyFaciesSedimentary rockSiliciclastic14. Life underwaterReefGeology0105 earth and related environmental sciencesGeological Journal
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Facies stacking and extinctions across the Triassic–Jurassic boundary in a peritidal succession from western Sicily

2017

An uppermost Triassic–lowermost Jurassic carbonate platform succession, which is 430 m thick, in northwestern Sicily is described with the aim to provide new data on the sedimentological and biological variations across the Triassic–Jurassic boundary in peritidal environments. The studied succession belonged to the rimmed carbonate shelf that developed during the upper Triassic along the margins of the Ionian Tethys. The peritidal sediments consist of metre-scale shallowing-upward cycles formed by subtidal, intertidal and supratidal facies. Three main informal units are differentiated along the section on the basis of the variations recorded by the subtidal facies. The lower and middle unit…

Extinction event010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyFaunaPaleontologyGeologyEcological succession010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundPaleontologychemistryTriassic-Jurassic boundary mass extinction foraminiferal biostratigraphy peritidal carbonates facies analysis SicilyBenthic zoneFaciesCarbonateSedimentologyGeology0105 earth and related environmental sciencesFacies
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