@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_d74e6fc2
  rdf:value "Alisols 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. Alisols have high-activity clays throughout the argic horizon and a low base saturation in the 50–100 cm depth. They occur predominantly in humid tropical, humid subtropical and humid temperate regions. Many Alisols correlate with Parabraunerden (Germany), Argissolos (Brazil), Ultisols with high-activity clays (United States of America), Kurosols (Australia), and Fersialsols and Sols fersiallitiques très lessivés (France)."@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 "2020-01-20T14:30:12.359+01:00"^^xsd:dateTime ;
  dc:modified "2025-01-31T11:45:27"^^xsd:dateTime .

agrovoc:c_479c499a skos:definition agrovoc:xDef_d74e6fc2 .