Search results for "Deposit"

showing 10 items of 1447 documents

In-situ observations and modeling of small nitric acid-containing ice crystals

2007

Measurements in nascent ice forming regions are very rare and help understand cirrus cloud formation and the interactions of trace gases with ice crystals. A tenuous cirrus cloud has been probed with in-situ and remote sensing instruments onboard the high altitude research aircraft Geophysica M55 in the tropical upper troposphere. Besides microphysical and optical particle properties, water (H<sub>2</sub>O) and reactive nitrogen species (NO<sub>y</sub>) have been measured. In slightly ice supersaturated air between 14.2 and 14.9 km altitude, an unusually low ice water content of 0.031 mg m<sup>−3</sup> and small ice crystals with mean radii of 5…

Atmospheric Science010504 meteorology & atmospheric sciencesiceAnalytical chemistrycirrus010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesTropospherelcsh:Chemistryddc:5500105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereSupersaturationIce crystalsChemistryAtmosphärische Spurenstoffelcsh:QC1-999Trace gasAerosolJnitric acidDeposition (aerosol physics)lcsh:QD1-99913. Climate actionCirrustrace gas uptakeWater vaporlcsh:Physics
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Validation of a novel automatic deposition of bacteria and yeasts on MALDI target for MALDI-TOF MS-based identification using MALDI Colonyst robot

2017

Matrix-assisted laser desorption/ionization time-of-flight mass spectrometry (MALDI-TOF MS) -based identification of bacteria and fungi significantly changed the diagnostic process in clinical microbiology. We describe here a novel technique for bacterial and yeast deposition on MALDI target using an automated workflow resulting in an increase of the microbes' score of MALDI identification. We also provide a comparison of four different sample preparation methods. In the first step of the study, 100 Gram-negative bacteria, 100 Gram-positive bacteria, 20 anaerobic bacteria and 20 yeasts were spotted on the MALDI target using manual deposition, semi-extraction, wet deposition onto 70% formic …

Atmospheric ScienceCarboxylic Acidslcsh:MedicineAnaerobic BacteriaResearch and Analysis MethodsMicrobiologyMass SpectrometryAnalytical ChemistryAutomationSpectrum Analysis TechniquesYeastsEnvironmental Chemistrylcsh:ScienceMatrix-Assisted Laser Desorption Ionization Time-of-Flight Mass SpectrometryGram Negative BacteriaBacteriaOrganic Compoundslcsh:REcology and Environmental SciencesGram Positive BacteriaFormic AcidOrganic ChemistryOrganismsFungiChemical CompoundsBiology and Life SciencesEukaryotaBacteriologyRoboticsYeastChemistryAtmospheric ChemistrySpectrometry Mass Matrix-Assisted Laser Desorption-IonizationPhysical SciencesEarth Scienceslcsh:QAcid DepositionAcidsResearch ArticlePLoS ONE
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A Theoretical Study of the Wet Removal of Atmospheric Pollutants. Part V: The Uptake, Redistribution, and Deposition of (NM4)4SO4by a Convective Clou…

1995

Abstract The effects of an ice phase on the wet deposition of aerosol particles was studied by means of the authors’ 2D cloud dynamics model with spectral microphysics applied to the Cooperative Convective Precipitation Experiment in Miles City, Montana, on 19 July 1981. The cloud macrostructure as well as the cloud microstructure simulated by the model was found to agree well with observations. Although no on-site observations were available with respect to the chemical composition of the cloud and rain water, the values predicted by the model compared well with typical nearby measurements. The following conclusions can be derived from the model computations: (1) In confirmation of the aut…

Atmospheric ScienceDeposition (aerosol physics)MicrophysicsMeteorologyLiquid water contentbusiness.industryCloud physicsEnvironmental scienceCloud computingbusinessScavengingChemical compositionAerosolJournal of the Atmospheric Sciences
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Anthropogenic Perturbations to the Atmospheric Molybdenum Cycle

2021

Molybdenum (Mo) is a key cofactor in enzymes used for nitrogen (N) fixation and nitrate reduction, and the low availability of Mo can constrain N inputs, affecting ecosystem productivity. Natural atmospheric Mo aerosolization and deposition from sources such as desert dust, sea‐salt spray, and volcanoes can affect ecosystem function across long timescales, but anthropogenic activities such as combustion, motor vehicles, and agricultural dust have accelerated the natural Mo cycle. Here we combined a synthesis of global atmospheric concentration observations and modeling to identify and estimate anthropogenic sources of atmospheric Mo. To project the impact of atmospheric Mo on terrestrial ec…

Atmospheric ScienceGlobal and Planetary ChangeNitrogenasechemistry.chemical_elementParticulatesAerosol depositionchemistryNitrogen fixationMolybdenumEnvironmental chemistryNutrient limitationNitrogenaseNitrogen fixationEnvironmental ChemistryEnvironmental scienceAerosol depositionParticulate matterGeneral Environmental Science
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Environmental scanning electron microscopy (ESEM) as a new technique to determine the ice nucleation capability of individual atmospheric aerosol par…

2007

Abstract Heterogeneous ice nucleation on synthetic silver iodide, natural kaolinite and montmorillonite particles via condensation, freezing and deposition modes was studied by environmental scanning electron microscopy (ESEM) in the temperature range of 250–270 K. By increasing the H2O pressure in the sample chamber at constant temperature, ice formation can be studied in situ and can be related to the chemical composition of the particles that can be determined simultaneously. For silver iodide and kaolinite, supersaturation values of first ice formation are in good agreement (1–2% absolute) with diffusion chamber experiments. For both substances, threshold temperatures for the condensati…

Atmospheric ScienceIce cloudSupersaturationIce crystalsChemistryAnalytical chemistrySilver iodideCloud physicsMineralogychemistry.chemical_compoundIce nucleusDeposition (phase transition)Environmental scanning electron microscopeGeneral Environmental ScienceAtmospheric Environment
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The transatlantic dust transport from North Africa to the Americas-Its characteristics and source regions

2015

Transport of Saharan dust over the Atlantic to the Americas is a relevant process since dust is a nutrient for marine and terrestrial ecosystems. It is therefore important to better quantify the frequency and amount of transatlantic dust transport, its preferred altitude and duration, and the regions of dust origin. This study uses a novel combination of Eulerian and Lagrangian diagnostics, applied to a previously validated 5 year simulation of the fifth generation European Centre for Medium Range Weather Forecast-Hamburg-model (ECHAM5)/Modular Earth Submodel System (MEESy) Atmospheric Chemistry model, to quantify these dust transport characteristics and their seasonal variations. Results c…

Atmospheric ScienceIntertropical Convergence ZoneMineral dustAtmospheric sciencesMonsooncomplex mixturesGeophysicsAltitudeDeposition (aerosol physics)BorealSpace and Planetary ScienceAtmospheric chemistryClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceLagrangian analysisJournal of Geophysical Research: Atmospheres
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Hygroscopic properties and extinction of aerosol particles at ambient relative humidity in South-Eastern China

2008

Abstract During the “Program of Regional Integrated Experiments of Air Quality over Pearl River Delta 2004 (PRIDE-PRD2004)” hygroscopic properties of particles in the diameter range 22 nm to 10 μ m were determined. For that purpose, a Humidifying Differential Mobility Particle Sizer (H-DMPS) and a Micro-Orifice Uniform Deposition Impactor (MOUDI) were operated. The derived size-dependent particle hygroscopic growth factors were interpolated to ambient relative humidity (RH) and used to calculate the particle number size distributions (PNSDs) at ambient conditions. A comparison between the modeled particle extinction coefficients ( σ ext , Mie ) and those observed with a Raman lidar was made…

Atmospheric ScienceMaterials scienceDeposition (aerosol physics)Particle numberExtinction (optical mineralogy)Ultrafine particleParticle-size distributionAnalytical chemistryMineralogyParticleRelative humidityGeneral Environmental ScienceAerosolAtmospheric Environment
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2010

Abstract. As a contribution to the Large-Scale Biosphere-Atmosphere Experiment in Amazonia – Cooperative LBA Airborne Regional Experiment (LBA-CLAIRE-2001) field campaign in the heart of the Amazon Basin, we analyzed the temporal and spatial dynamics of the urban plume of Manaus City during the wet-to-dry season transition period in July 2001. During the flights, we performed vertical stacks of crosswind transects in the urban outflow downwind of Manaus City, measuring a comprehensive set of trace constituents including O3, NO, NO2, CO, VOC, CO2, and H2O. Aerosol loads were characterized by concentrations of total aerosol number (CN) and cloud condensation nuclei (CCN), and by light scatter…

Atmospheric ScienceOzone010504 meteorology & atmospheric sciencesParticle number010501 environmental sciences15. Life on landAtmospheric sciences01 natural sciencesPlumeAerosolAtmospherechemistry.chemical_compoundDeposition (aerosol physics)chemistry13. Climate action11. SustainabilityCloud condensation nucleiTropospheric ozone0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Multilayer modelling of ozone fluxes on winter wheat reveals large deposition on wet senescing leaves

2015

Understanding how ozone is deposited on vegetation canopies is needed to perform tropospheric greenhouse gas budgets and evaluate the associated damage on vegetation. In this study, we propose a new multilayer scheme of ozone deposition on vegetation canopies that predicts stomatal, cuticular and soil deposition pathways separately. This mechanistic ozone deposition scheme is based on the multi-layer, multi-leaf mass and energy transfer model MuSICA. This model was chosen because it explicitly simulates the processes of rain interception, through fall and evaporation at different depths within the vegetation canopy, so that ozone deposition on wet leaf cuticles can be explicitly modelled wi…

Atmospheric ScienceOzonesenescence010504 meteorology & atmospheric sciences[SDV]Life Sciences [q-bio]010501 environmental sciencesAtmospheric sciences01 natural scienceswater filmchemistry.chemical_compoundMuSICAozone depositionEvapotranspirationwheat0105 earth and related environmental sciencesHydrologyGlobal and Planetary Change[ SDV ] Life Sciences [q-bio]ForestryVegetation15. Life on landchemistry13. Climate actionGreenhouse gasEnvironmental scienceDewcuticleInterceptionAgronomy and Crop ScienceDeposition (chemistry)Water vapor
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2016

Abstract. We found that ambient and laboratory-generated secondary organic aerosols (SOA) form substantial amounts of OH radicals upon interaction with liquid water, which can be explained by the decomposition of organic hydroperoxides. The molar OH yield from SOA formed by ozonolysis of terpenes (α-pinene, β-pinene, limonene) is  ∼  0.1 % upon extraction with pure water and increases to  ∼  1.5 % in the presence of Fe2+ ions due to Fenton-like reactions. Upon extraction of SOA samples from OH photooxidation of isoprene, we also detected OH yields of around  ∼  0.1 %, which increases upon addition of Fe2+. Our findings imply that the chemical reactivity and aging of SOA particles is strongl…

Atmospheric ScienceOzonolysis010504 meteorology & atmospheric sciencesRadicalInorganic chemistryExtraction (chemistry)010501 environmental sciencesPhotochemistry01 natural sciencesDecompositionAerosolchemistry.chemical_compoundDeposition (aerosol physics)chemistryYield (chemistry)Isoprene0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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