_:b1217732	<http://www.geneontology.org/formats/oboInOwl#hasDbXref>	"FAO:http://fao.org/ag/agl/agll/wrb/doc/wrb2006final.pdf"^^<http://www.w3.org/2001/XMLSchema#string> .
_:b1217732	<http://www.w3.org/2002/07/owl#annotatedSource>	<http://purl.obolibrary.org/obo/ENVO_00002250> .
_:b1217732	<http://www.w3.org/2002/07/owl#annotatedTarget>	"Plinthosols are soils with plinthite, petroplinthite or pisoliths. Plinthite is an Fe-rich (in some cases also Mn-rich), humus-poor mixture of kaolinitic clay (and other products of strong weathering such as gibbsite) with quartz and other constituents that changes irreversibly to a layer with hard nodules, a hardpan or irregular aggregates on exposure to repeated wetting and drying. Petroplinthite is a continuous, fractured or broken sheet of connected, strongly cemented to indurated nodules or mottles. Pisoliths are discrete strongly cemented to indurated nodules. Both petroplinthite and pisoliths develop from plinthite by hardening."^^<http://www.w3.org/2001/XMLSchema#string> .
_:b1217732	<http://www.w3.org/2002/07/owl#annotatedProperty>	<http://purl.obolibrary.org/obo/IAO_0000115> .
_:b1217732	<http://www.w3.org/1999/02/22-rdf-syntax-ns#type>	<http://www.w3.org/2002/07/owl#Axiom> .