@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_27617f37
  rdf:value "Acrisols 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. Acrisols have low-activity clays in the argic horizon and a low base saturation in the 50–100 cm depth. Many Acrisols correlate with Red yellow podzolic soils (e.g. Indonesia), Argissolos (Brazil), Kurosols (Australia), Sols ferralitiques fortement ou moyennement désaturés (France) and Ultisols 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 "2020-01-20T14:18:35.492+01:00"^^xsd:dateTime ;
  dc:modified "2025-01-31T12:27:17"^^xsd:dateTime .

agrovoc:c_101 skos:definition agrovoc:xDef_27617f37 .