{ "items" : [
    { "id" : "http://purl.obolibrary.org/obo/ENVO_00002249"
      "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" : [ "phaeozem" ] ,
        "http://www.w3.org/2000/01/rdf-schema#subClassOf" : [ "http://purl.obolibrary.org/obo/ENVO_00001998" ] ,
        "http://purl.obolibrary.org/obo/IAO_0000115" : [ "Phaeozems accommodate soils of relatively wet grassland and forest regions in moderately continental climates. Phaeozems are much like Chernozems and Kastanozems but are leached more intensively. Consequently, they have dark, humus rich surface horizons that, in comparison with Chernozems and Kastanozems, are less rich in bases. Phaeozems may or may not have secondary carbonates but have a high base saturation in the upper metre of the soil." ] ,
        "http://www.geneontology.org/formats/oboInOwl#hasOBONamespace" : [ "ENVO" ] ,
        "http://www.geneontology.org/formats/oboInOwl#id" : [ "ENVO:00002249"] } } }
