@prefix pp: .
@prefix metadata: .
@prefix eol: .
@prefix owl: .
@prefix cos: .
@prefix skos: .
@prefix lexinfo: .
@prefix vivo-inra: .
@prefix ms2o: .
@prefix xml: .
@prefix dcterms: .
@prefix vann: .
@prefix pan: .
@prefix prism: .
@prefix foaf: .
@prefix ontology: .
@prefix void: .
@prefix pav: .
@prefix inra: .
@prefix snomed: .
@prefix ado: .
@prefix onto: .
@prefix core: .
@prefix wto: .
@prefix status: .
@prefix schema: .
@prefix obol: .
@prefix owl2xml: .
@prefix xsd: .
@prefix rdfs: .
@prefix fp: .
@prefix ncbitaxon: .
@prefix omv: .
@prefix dcat: .
@prefix kg: .
@prefix sp: .
@prefix prov: .
@prefix eng: .
@prefix cc: .
@prefix st: .
@prefix oboInOwl: .
@prefix skosxl: .
@prefix cw: .
@prefix thviande: .
@prefix rdf: .
@prefix insee: .
@prefix plp: .
@prefix bibo: .
@prefix thesaurusINRAE: .
@prefix tp: .
@prefix atol: .
@prefix dc: .
skos:broader .
rdfs:label "RDF description of c2_2574" ;
foaf:primaryTopic .
skos:narrower .
skos:broader .
skos:broader .
skos:broader .
skos:broader .
skos:broader .
skos:broader .
rdf:type skos:Concept ;
status:hasStatus "Published"^^xsd:string ;
dcterms:modified "2020-08-31T16:59:17.719+02:00"^^xsd:dateTime ;
skos:altLabel "teneur en eau du sol"@fr , "soil water content"@en , "soil humidity"@en ;
skos:broader ;
skos:definition , "1) Water stored in soils.\n2) One of the most important elements involved in pedological processes and plant growth. There are three basic forms: a) water adhering in thin films by molecular attraction to the surface of soil particles and not available for plants is termed hygroscopic water. b) Water forming thicker films and occupying the smaller pore spaces is termed capillary water. Since it is held against the force of gravity it is permanently available for plant growth and it is this type of soil water which contains plant nutrients in solution. c) Water in excess of hygroscopic and capillary water is termed gravitational water, which is of a transitory nature because it flows away under the influence of gravity. When the excess has drained away the amount of water retained in the soil is termed its field capacity, when some of its pore spaces are still free of water."@en ;
skos:exactMatch , ;
skos:inScheme ;
skos:narrower , , , , , , , , , , ;
skos:prefLabel "soil moisture"@en , "humidité du sol"@fr .
skos:broader .
skos:broader .
skos:broader .
skos:broader .