_:b1217730	<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> .
_:b1217730	<http://www.w3.org/2002/07/owl#annotatedSource>	<http://purl.obolibrary.org/obo/ENVO_00002248> .
_:b1217730	<http://www.w3.org/1999/02/22-rdf-syntax-ns#type>	<http://www.w3.org/2002/07/owl#Axiom> .
_:b1217730	<http://www.w3.org/2002/07/owl#annotatedProperty>	<http://purl.obolibrary.org/obo/IAO_0000115> .
_:b1217730	<http://www.w3.org/2002/07/owl#annotatedTarget>	"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."^^<http://www.w3.org/2001/XMLSchema#string> .