{"@context":{"obo_purl":"http://purl.obolibrary.org/obo/","rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","owl":"http://www.w3.org/2002/07/owl#","rdfs":"http://www.w3.org/2000/01/rdf-schema#","metadata_def":"http://data.bioontology.org/metadata/def/","metadata":"http://data.bioontology.org/metadata/"},"@id":"obo_purl:ENVO_00002248","@type":"owl:Class","rdfs:subClassOf":{"@id":"obo_purl:ENVO_00001998"},"rdfs:label":"luvisol","obo_purl:IAO_0000115":"Luvisols 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. Luvisols have high-activity clays throughout the argic horizon and a high base saturation at certain depths.","metadata:def/prefLabel":"luvisol","metadata:def/mappingLoom":"luvisol","metadata:def/mappingSameURI":{"@id":"obo_purl:ENVO_00002248"},"metadata:prefixIRI":"obo1:ENVO_00002248"}