This HTML5 document contains 21 embedded RDF statements represented using HTML+Microdata notation.

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Namespace Prefixes

PrefixIRI
n15http://vocab.nerc.ac.uk/collection/P07/current/IJWJWK1A/1/
dctermshttp://purl.org/dc/terms/
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owlhttp://www.w3.org/2002/07/owl#
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n8http://purl.org/pav/
n6http://mmisw.org/ont/cf/parameter/
n4http://vocab.nerc.ac.uk/standard_name/tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_turbulent_deposition/

Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
3
owl:sameAs
n4: n6:tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_turbulent_deposition
skos:prefLabel
tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_turbulent_deposition
dcterms:identifier
SDN:P07::IJWJWK1A
dc:identifier
SDN:P07::IJWJWK1A
dcterms:date
2017-07-24 14:37:00.0
skos:definition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. The mass is the total mass of the molecules. "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol particles" means aerosol particles without any water uptake. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The sum of turbulent deposition and gravitational settling is dry deposition. "tendency_of_X" means derivative of X with respect to time. Chemically, "elemental carbon" is the carbonaceous fraction of particulate matter that is thermally stable in an inert atmosphere to high temperatures near 4000K and can only be gasified by oxidation starting at temperatures above 340 C. It is assumed to be inert and non-volatile under atmospheric conditions and insoluble in any solvent (Ogren and Charlson, 1983).
skos:notation
SDN:P07::IJWJWK1A
skos:altLabel
owl:deprecated
false
skos:note
accepted
void:inDataset
n11:void
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n7:
dcterms:replaces
n14:
n8:authoredOn
2017-07-24 14:37:00.0
n8:hasCurrentVersion
n16:
n8:hasVersion
n12: n15:
n8:version
3