{ "items" : [
    { "id" : "http://purl.obolibrary.org/obo/ENVO_00002231"
      "properties" : {
        "http://www.w3.org/1999/02/22-rdf-syntax-ns#type" : [ "http://www.w3.org/2002/07/owl#Class" ] ,
        "http://www.w3.org/2000/01/rdf-schema#label" : [ "alisol" ] ,
        "http://www.w3.org/2000/01/rdf-schema#subClassOf" : [ "http://purl.obolibrary.org/obo/ENVO_00001998" ] ,
        "http://purl.obolibrary.org/obo/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." ] ,
        "http://www.geneontology.org/formats/oboInOwl#hasOBONamespace" : [ "ENVO" ] ,
        "http://www.geneontology.org/formats/oboInOwl#id" : [ "ENVO:00002231"] } } }
