@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> . @prefix obo_purl: <http://purl.obolibrary.org/obo/> . @prefix owl: <http://www.w3.org/2002/07/owl#> . @prefix rdfs: <http://www.w3.org/2000/01/rdf-schema#> . @prefix skos: <http://www.w3.org/2004/02/skos/core#> . @prefix oboinowl_gen: <http://www.geneontology.org/formats/oboInOwl#> . @prefix metadata_def: <http://data.bioontology.org/metadata/def/> . obo_purl:ENVO_00002231 metadata_def:mappingLoom "alisol" ; metadata_def:mappingSameURI obo_purl:ENVO_00002231 ; metadata_def:prefLabel "alisol" ; obo_purl:IAO_0000115 "Alisols are soils that have a higher clay content in the subsoil than in the topsoil as a result of pedogenetic processes (especially clay migration) leading to an argic subsoil horizon. Alisols have a low base saturation at certain depths and high-activity clays throughout the argic horizon. They lack the albeluvic tonguing as in Albeluvisols. They occur predominantly in humid tropical, humid subtropical and warm temperate regions." ; oboinowl_gen:hasOBONamespace "ENVO" ; oboinowl_gen:id "ENVO:00002231" ; a owl:Class ; rdfs:label "alisol" ; rdfs:subClassOf obo_purl:ENVO_00001998 ; skos:notation "ENVO:00002231" .
@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix obo_purl: <http://purl.obolibrary.org/obo/> .
@prefix owl: <http://www.w3.org/2002/07/owl#> .
@prefix rdfs: <http://www.w3.org/2000/01/rdf-schema#> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix oboinowl_gen: <http://www.geneontology.org/formats/oboInOwl#> .
@prefix metadata_def: <http://data.bioontology.org/metadata/def/> .

obo_purl:ENVO_00002231
    metadata_def:mappingLoom "alisol" ;
    metadata_def:mappingSameURI obo_purl:ENVO_00002231 ;
    metadata_def:prefLabel "alisol" ;
    obo_purl:IAO_0000115 "Alisols are soils that have a higher clay content in the subsoil than in the topsoil as a result of pedogenetic processes (especially clay migration) leading to an argic subsoil horizon. Alisols have a low base saturation at certain depths and high-activity clays throughout the argic horizon. They lack the albeluvic tonguing as in Albeluvisols. They occur predominantly in humid tropical, humid subtropical and warm temperate regions." ;
    oboinowl_gen:hasOBONamespace "ENVO" ;
    oboinowl_gen:id "ENVO:00002231" ;
    a owl:Class ;
    rdfs:label "alisol" ;
    rdfs:subClassOf obo_purl:ENVO_00001998 ;
    skos:notation "ENVO:00002231" .