Search results for "Silicate"

showing 10 items of 413 documents

Influence of humic acid on neptunium(V) sorption and diffusion in Opalinus Clay

2013

SummaryThe influence of14C-labeled M42 humic acid (HA) on the interaction between neptunium(V) and natural clay rock (Opalinus Clay (OPA), Switzerland) has been investigated in batch sorption and diffusion experiments under ambient air conditions. The effect of 10 mg/L HA on the diffusion of 8 μM Np(V) in OPA has been investigated in synthetic OPA pore water (pH 7.6, I = 0.4M) for the first time. Batch sorption experiments as a function of solid-to-liquid ratio (4-20 g/L) were performed under same experimental conditions to compare distribution coefficients obtained from both diffusion and sorption experiments. These experiments showed only a slight influence of HA on Np(V) uptake by OPA in…

Calcitechemistry.chemical_classificationLight nucleuschemistry.chemical_compoundchemistrySilicate mineralsNeptuniumchemistry.chemical_elementHumic acidSorptionPhysical and Theoretical ChemistryWaste disposalNuclear chemistryract
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Experimental study of Si–Al substitution in calcium-silicate-hydrate (C-S-H) prepared under equilibrium conditions.

2009

International audience; C-A-S-H of varying Al/Si and Ca/(Al+Si) ratios have been prepared introducing C-S-H (Ca/Si=0.66 and 0.95) at different weight concentrations in a solution coming from the hydration of tricalcium aluminate (Ca3Al2O6) in water. XRD and EDX (TEM) analyses show that using this typical synthesise procedure, pure C-A-S-H is obtained only for calcium hydroxide concentrations below 4.5 mmol L−1. Otherwise, calcium carboaluminate or strätlingite is also present beside C-A-S-H. The tobermorite-like structure is maintained for C-A-S-H. A kinetic study has shown that the formation of C-A-S-H is a fast reaction, typically less than a few hours. The Ca/(Al+Si) ratio of C-A-S-H mat…

Calcium hydroxideCalcium-silicate-hydrate (C-S-H)Aluminium hydroxide0211 other engineering and technologiesAnalytical chemistryMineralogychemistry.chemical_elementIonic bonding02 engineering and technologyBuilding and ConstructionCalcium021001 nanoscience & nanotechnologyKinetic energychemistry.chemical_compoundChemistrychemistryAluminium021105 building & constructionAluminiumThermodynamic equilibriaGeneral Materials ScienceTricalcium aluminateCalcium silicate hydrate0210 nano-technology
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Experimental conditions for respiration and growth studies of F0 and F1 larval and juvenile European seabass Dicentrarchus labrax

2022

Water parameters in the 2 years before spawning of F0 (08.02.2016-06.03.2018) and during larval and juvenile phase of F1: Larval period until 17.05.2018 (48 dph, 900 dd) and 01.06.2018 (63 dph, ~900 dd) for warm and cold life condition respectively, for the juveniles until 28.09.2018 (180 dph, ~4000 dd) and 12.02.2019 (319 dph, ~5100 dd) for warm and cold conditioned fish respectively. Means ± s.e. over all replicate tanks per condition. Temperature (Temp.), pH (free scale), salinity, oxygen and total alkalinity (TA) were measured weekly in F1 and monthly in F0; sea water (SW) measurements were conducted in 2017 and 2018. Water parameters during larval and early juvenile phase of F0: Larval…

Calculated by CO2sys_xls_program Lewis and WallaceSalinityAlkalinityLife stageType of studyTemperature waterGermanyCalculatedAlkalinity totalSalinity standard errortotallarval growthteleostexperiment2006pH2007 with purified m cresol purpleOcean acidificationMeasured spectrophotometrically Dickson et alTemperatureWeilheimPartial pressure of carbon dioxide (water) at sea surface temperature (wet air) standard errorSilicatedissolvedLaboratory experimentSEAL AA3 segmented flow autoanalyzerSilicate standard errorstandard errorMultiprobeEarth System ResearchWTW 340imetabolic rateswaterGenerationOxygen dissolvedMultiprobe WTW 340iPhosphateocean warmingAlkalinity total standard errorjuvenile growthCarbon dioxide (water) partial pressurepH meter (WTW 3110) with electrode (WTW Sentix 41)DATE TIMEWTW Oxi 340i probeTemperature water standard errorCarbon dioxide water partial pressurepH standard errorXylem Analytics GermanySalinometer (WTW LF325 Xylem Analytics Germany Weilheim Germany)Calculated by CO2sys_xls_program (Lewis and Wallace 2006)OxygenTreatmentDATE/TIMEPartial pressure of carbon dioxide water at sea surface temperature wet airSalinometer WTW LF325Oxygen dissolved standard errorMeasured spectrophotometrically (Dickson et al. 2007) with purified m-cresol purplepH meter WTW 3110 with electrode WTW Sentix 41Phosphate standard error
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Origin of clay minerals in soils on pyroclastic deposits in the island of Lipari (Italy)

2005

The island of Lipari (Italy) is characterized by calc-alkaline to potassic volcanism and a Mediterranean-type climate. The mineralogical and chemical features of two different soil profiles with ages of 92,000 and 10,000–40,000 y, respectively, have been investigated. There were no Andisols, but Vitric and Vertic Cambisols have developed at both sites. Although the morphology of the soils was similar, remarkable differences in the clay mineralogy between the two sites were observed. The site with the Vitric Cambisol was associated with the weathering sequence: glass → halloysite → kaolinite or interstratified kaolinite-2:1 clay minerals. Both sites had smectite in the clay fraction and, to …

CambisolGeochemistrySoil ScienceMineralogyWeatheringAndisols geochemistry montmorillonite glasses kaolinite sheet silicates Italy Cambisols clay mineralogy Europe silicates soils halloysite Lipari Islands clay minerals igneous rocks Lipari Island smectite metasomatism weathering Sicily Italy volcanic rocks Southern Europeengineering.materialHalloysitechemistry.chemical_compoundMontmorillonitechemistrySettore AGR/14 - PedologiaGeochemistry and PetrologySoil waterEarth and Planetary Sciences (miscellaneous)engineeringSoil horizonKaoliniteClay mineralsGeologyWater Science and Technologyclays and clay minerals
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The growth of charged platelets.

2014

Growth models of charged nanoplatelets are investigated with Monte Carlo simulations and simple theory. In a first model, 2-dimensional simulations in the canonical ensemble are used to demonstrate that the growth of a single weakly charged platelet could be limited by its own internal repulsion. The short range attractive interaction in the crystal is modeled with a square well potential while the electrostatic interactions are described with a screened Coulomb potential. The qualitative behavior of this case can also be described by simply balancing the attractive crystal energy with the screened Coulomb repulsion between the crystal sites. This repulsion is a free energy term dominated b…

Canonical ensembleChemistryNucleationGeneral Physics and AstronomyCharge densityElectrostaticschemistry.chemical_compoundChemical physicsComputational chemistryFinite potential wellCoulombElectric potentialPhysical and Theoretical ChemistryCalcium silicate hydratePhysical chemistry chemical physics : PCCP
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Microtomographic Quantification of Hydraulic Clay Mineral Displacement Effects During a CO2 Sequestration Experiment with Saline Aquifer Sandstone

2013

We combined a noninvasive tomographic imaging technique with an invasive open-system core-flooding experiment and compared the results of the pre- and postflooded states of an experimental sandstone core sample from an ongoing field trial for carbon dioxide geosequestration. For the experiment, a rock core sample of 80 mL volume was taken from the 629 m Stuttgart Formation storage domain of a saline sandstone aquifer at the CCS research pilot plant Ketzin, Germany. Supercritical carbon dioxide and synthetical brine were injected under in situ reservoir p/T-conditions at an average flow rate of 0.1 mL/min for 256 h. X-ray computed microtomographic imaging was carried out before and after the…

Carbon SequestrationGeological PhenomenaSalinitySupercritical carbon dioxideTomographic reconstructionMineralogyCore sample550 - Earth sciencesX-Ray MicrotomographyGeneral ChemistryCarbon DioxideCarbon sequestrationPermeabilitySedimentary depositional environmentBriningClayEnvironmental ChemistryAluminum SilicatesSaltsClay mineralsPorosityGroundwaterPorosityGeologyEnvironmental Science & Technology
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Application of a MTT Assay for Screening Nutritional Factors in Growth Media of Primary Sponge Cell Culture

2004

Marine sponges (Porifera) are producers of the largest variety of bioactive compounds among benthic marine organisms. In vitro culture of marine sponge cells has been proposed for the sustainable production of these pharmacologically interesting compounds from marine sponges but with limited success. The development of a suitable growth medium is an essential prerequisite for sponge cells grown in vitro. The MTT (3-(4,5-dimethylthiazol-2-yl)-2,5-diphenyltetrazolium bromide) assay was adapted to screen for potential nutritional factors in formulating a growth medium for primary cell culture of Suberites domuncula. In 96-well plates, the effects of nutritional factors including glutamine, pyr…

Cell SurvivalGlutamineIronCell Culture TechniquesCell CountMicrobiologychemistry.chemical_compoundPyruvic AcidAnimalsNutritional Physiological PhenomenaMTT assayViability assayFood scienceGrowth mediumbiologyCell growthSilicatesbiology.organism_classificationCulture MediaPoriferaSuberites domunculaGlutamineSpongechemistryCell cultureBiotechnologyBiotechnology Progress
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Electrokinetic Properties which Control the Coagulation of Silicate Cement Suspensions during Early Age Hydration

1998

The coagulation of cement particles during early age hydration has been previously identified as the first step of the setting and hardening of cement pastes. By hydrating Ca3SiO5and a silicate-rich clinker under controlled conditions, a correlation between the coagulation of the suspensions and the electrokinetic properties of particles is established. The zeta potential, and hence the surface charge, of particles in suspension depends on the calcium content of the medium. At low concentrations of Ca2+, the zeta potential of Ca3SiO5particles, calcium silicate hydrate (C–S–H), and clinker is negative (<−30 mV) and the suspensions are well dispersed. A strong coagulation occurs at intermedia…

CementChemistryMineralogySurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsBiomaterialschemistry.chemical_compoundElectrokinetic phenomenaColloid and Surface ChemistryChemical engineeringParticle-size distributionHardening (metallurgy)Zeta potentialSilicate CementSurface chargeCalcium silicate hydrateJournal of Colloid and Interface Science
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Prediction of Long-Term Chemical Evolution of a Low-pH Cement Designed for Underground Radioactive Waste Repositories

2012

Low-pH cements, also referred as low-alkalinity cements, are binders with a pore solution pH ≤ 11. They can be designed by replacing significant amounts of Portland cement (OPC) (≥40 %) by silica fume, which can be associated in some cases to low-CaO fly ash and/or ground granulated blast furnace slag to decrease the heat output during hydration by dilution of OPC and improve the mechanical strength of the final material. With the prospect of using these materials in a geological repository, it is of main importance to estimate their long-term properties and the influence of external and internal factors (chemical composition of the binder, storage temperature) on their characteristics. For…

CementEngineeringSilica fumeWaste managementbusiness.industryMetallurgytechnology industry and agricultureengineering.materiallaw.inventionchemistry.chemical_compoundPortland cementchemistryGround granulated blast-furnace slaglawFly ashSlurryCalcium silicate hydratebusinessLime
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Hydration of alite containing aluminium

2011

Abstract The most important phase in Portland cement is tricalcium silicate, which leads during its hydration to the nucleation and growth of calcium silicate hydrate [referred to as C–S–H, (CaO)x–SiO2–(H2O)y]. The development of this hydrate around the cement grains is responsible for the setting and hardening of cement pastes. The general term for designating the tricalcium silicate in cements is alite. This name relates to all polymorphs containing various foreign ions inserted in their structure. These ions may influence the intrinsic reactivity, and once released during the dissolution, they may interact also with C–S–H. One of the most likely species to be inserted in the alite struct…

CementMaterials scienceAliteNucleationMineralogychemistry.chemical_elementIndustrial and Manufacturing Engineeringlaw.inventionPortland cementchemistry.chemical_compoundchemistryChemical engineeringlawAluminiumCeramics and CompositesCalcium silicate hydrateHydrateDissolutionAdvances in Applied Ceramics
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