@prefix agrovoc: <http://aims.fao.org/aos/agrovoc/> .
@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix ns0: <http://art.uniroma2.it/ontologies/vocbench#> .
@prefix dc: <http://purl.org/dc/terms/> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .

agrovoc:xDef_ad9ed4db
  rdf:value "Lixisols 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. Lixisols have low-activity clays in the argic horizon and a high base saturation in the 50–100 cm depth. Many Lixisols are included in Red yellow podzolic soils (e.g. Indonesia), Chromosols (Australia), Argissolos (Brazil), Sols ferralitiques faiblement desaturés appauvris (France) and Alfisols with low-activity clays (United States of America)."@en ;
  ns0:hasSource "IUSS Working Group WRB. 2015. World Reference Base for Soil Resources 2014, update 2015 International soil classification system for naming soils and creating legends for soil maps. World Soil Resources Reports No. 106. FAO, Rome." ;
  dc:created "2020-01-20T14:28:19.466+01:00"^^xsd:dateTime .

agrovoc:c_7283bd0a skos:definition agrovoc:xDef_ad9ed4db .