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"\u0627\u0644\u062A\u0631\u0628\u0629 \u0627\u0644\u062C\u0627\u0641\u0629 \u0623\u0648 \u062A\u0631\u0628\u0629 \u0627\u0644\u0635\u062D\u0631\u0627\u0621 \u0623\u0648 \u0623\u0631\u064A\u062F\u0633\u0648\u0644 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Aridisol)\u200F\u060C \u0647\u0648 \u0623\u062D\u062F \u0623\u0646\u0638\u0645\u0629 \u062A\u0635\u0646\u064A\u0641 \u0627\u0644\u062A\u0631\u0628\u0629 \u0627\u0644\u0623\u0645\u0631\u064A\u0643\u064A \u0644\u0648\u0643\u0627\u0644\u0629 \u062D\u0641\u0638 \u0627\u0644\u0645\u0648\u0627\u0631\u062F \u0627\u0644\u0637\u0628\u064A\u0639\u064A\u0629 \u0628\u0627\u0644\u0648\u0644\u0627\u064A\u0627\u062A \u0627\u0644\u0645\u062A\u062D\u062F\u0629. \u0633\u0628\u0628 \u062A\u0633\u0645\u064A\u062A\u0647\u0627 \u0628\u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u062C\u0627\u0641\u0629 \u062A\u0646\u062E\u0641\u0636 \u0628\u0647\u0627 \u0646\u0633\u0628\u0629 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0639\u0636\u0648\u064A\u0629 \u0648\u063A\u0646\u064A\u0629 \u0628\u0627\u0644\u0623\u0645\u0644\u0627\u062D \u0627\u0644\u0645\u062A\u0631\u0633\u0628\u0629\u060C \u0628\u0647\u0627 \u0634\u062D \u0645\u064A\u0627\u0647 \u0648\u0628\u0627\u0644\u062A\u0627\u0644\u064A \u0636\u0639\u0641 \u0625\u0644\u0649 \u0627\u0646\u0639\u062F\u0627\u0645 \u0627\u0644\u0625\u0646\u062A\u0627\u062C \u0627\u0644\u0646\u0628\u0627\u062A\u064A." , "lang" : "ar" } , { "type" : "literal", "value" : "Een aridisol is een van de 12 bodemtypes in de Amerikaanse bodemclassficatie (USDA Soil Taxonomy). Het zijn bodems die zijn gevormd in een aride of semi-aride klimaat. Watertekort en een hoge concentratie zouten zijn in deze bodems belangrijke factoren. Door de beperkte uitspoeling in het profiel komen er horizonten voor met een accumulatie van onder andere SiO2, natriumzouten, CaCO3 en gips. Deze horizonten kunnen ook irreversibel zijn verhard tot een hardpan. Aridisolen komen voor in woestijnen en droge gebieden met een spaarzame droogte-resistente vegetatie." , "lang" : "nl" } , { "type" : "literal", "value" : "L'ordine degli Aridisol \u00E8 uno dei dodici ordini della tassonomia del suolo secondo USDA, contraddistinto ai fini della nomenclatura con il suffisso id." , "lang" : "it" } , { "type" : "literal", "value" : "Als Aridisol bezeichnet man gem\u00E4\u00DF der USDA Soil Taxonomy kalkhaltige W\u00FCsten-B\u00F6den aus den Tropen und gem\u00E4\u00DFigten Breiten, die sich in Regionen trockenen Klimas ausbilden. Zu den Aridisolen geh\u00F6ren im Einzelnen: \n* \n* \n* Solontschake (Wei\u00DFalkalib\u00F6den) \n* Solonetze (Schwarzalkalib\u00F6den) \n* Rohb\u00F6den Weltweit sind etwa 15,7 Millionen Quadratkilometer oder 12 Prozent der eisfreien Landfl\u00E4che von Aridisolen bedeckt." , "lang" : "de" } , { "type" : "literal", "value" : "Arid soils (or desert soils) are a soil order in USDA soil taxonomy. Aridisols (from the Latin aridus, for \"dry\", and solum) form in an arid or semi-arid climate. Aridisols dominate the deserts and xeric shrublands, which occupy about one third of the Earth's land surface. Aridisols have a very low concentration of organic matter, reflecting the paucity of vegetative production on these dry soils. Water deficiency is the major defining characteristic of Aridisols. Also required is sufficient age to exhibit subsoil weathering and development. Limited leaching in aridisols often results in one or more subsurface soil horizons in which suspended or dissolved minerals have been deposited: silicate clays, sodium, calcium carbonate, gypsum or soluble salts. These subsoil horizons can also be cem" , "lang" : "en" } , { "type" : "literal", "value" : "Aridisol adalah kondisi tanah, lingkungan, atau daerah yang kering. Tanah aridisol memiliki kandungan organik rendah. Aridisol mengandung lempung, kalsium karbonat, silika, garam, dan/atau gipsum yang telah terakumulasi. Kutub dingin, gurun beriklim sejuk, dan gurun hangat termasuk ke dalam daerah aridisol. Ketiga hal tersebut jika dikualifikasikan berdasarkan iklim yakni menempati 36% permukaan tanah dan jika dikualifikasikan berdasarkan vegetasi yakni menempati 35%. Aridisol juga dapat terjadi di daerah semi-kering. Berdasarkan klasifikasi kelembaban tanah, tanah yang kering atau aridisol di semua bagian mencapai >50% dari waktu di sebagian besar tahun." , "lang" : "in" } , { "type" : "literal", "value" : "Aridis\u00F2ls (o s\u00F2ls del desert) s\u00F3n un ordre de s\u00F2l (Aridisol) de la USA soil taxonomy. Aridisols (del llat\u00ED aridus, per a \u201Csec\u201D, i solum per a s\u00F2l) es formen en climes \u00E0rids o semi\u00E0rids. Els aridis\u00F2ls dominen els cosistemes de desert i arbusts x\u00E8rics els quals ocupen un ter\u00E7 de la superf\u00EDcie emergida de la Terra. Els aridis\u00F2ls tenen una concentraci\u00F3 de mat\u00E8ria org\u00E0nica molt baixa que reflecteix que s\u00F3n s\u00F2ls molt poc productius." , "lang" : "ca" } ] , "http://xmlns.com/foaf/0.1/depiction" : [ { "type" : "uri", "value" : "http://commons.wikimedia.org/wiki/Special:FilePath/Aridisol_profile.jpg" } ] , "http://purl.org/dc/terms/subject" : [ { "type" : "uri", "value" : "http://dbpedia.org/resource/Category:Types_of_soil" } , { "type" : "uri", "value" : "http://dbpedia.org/resource/Category:Pedology" } ] , "http://dbpedia.org/ontology/abstract" : [ { "type" : "literal", "value" : "L'ordine degli Aridisol \u00E8 uno dei dodici ordini della tassonomia del suolo secondo USDA, contraddistinto ai fini della nomenclatura con il suffisso id." , "lang" : "it" } , { "type" : "literal", "value" : "Aridis\u00F2ls (o s\u00F2ls del desert) s\u00F3n un ordre de s\u00F2l (Aridisol) de la USA soil taxonomy. Aridisols (del llat\u00ED aridus, per a \u201Csec\u201D, i solum per a s\u00F2l) es formen en climes \u00E0rids o semi\u00E0rids. Els aridis\u00F2ls dominen els cosistemes de desert i arbusts x\u00E8rics els quals ocupen un ter\u00E7 de la superf\u00EDcie emergida de la Terra. Els aridis\u00F2ls tenen una concentraci\u00F3 de mat\u00E8ria org\u00E0nica molt baixa que reflecteix que s\u00F3n s\u00F2ls molt poc productius. La defici\u00E8ncia d'aigua \u00E9s la caracter\u00EDstica definit\u00F2ria d'aquests s\u00F2ls. La lixiviaci\u00F3 hi \u00E9s molt limitada i sovint en el perfil del s\u00F2l apareixen dip\u00F2sits minerals i/o cimentaci\u00F3 per carbonats, guix o s\u00EDlice. Poden donar lloc a la salinitzaci\u00F3." , "lang" : "ca" } , { "type" : "literal", "value" : "Een aridisol is een van de 12 bodemtypes in de Amerikaanse bodemclassficatie (USDA Soil Taxonomy). Het zijn bodems die zijn gevormd in een aride of semi-aride klimaat. Watertekort en een hoge concentratie zouten zijn in deze bodems belangrijke factoren. Door de beperkte uitspoeling in het profiel komen er horizonten voor met een accumulatie van onder andere SiO2, natriumzouten, CaCO3 en gips. Deze horizonten kunnen ook irreversibel zijn verhard tot een hardpan. Aridisolen komen voor in woestijnen en droge gebieden met een spaarzame droogte-resistente vegetatie. De Aridisolen bestaan uit de volgende suborders: \n* Cryids - aridisols met een gemiddelde jaarlijkse bodemtemperatuur tussen 0 \u00B0C en 8 \u00B0C, en geen permafrost \n* Salids - aridisols met binnen 100 cm diepte een >15 cm dikke horizont met een sterke accumulatie van zouten \n* Durids - aridisols met een (een harde, door silicium gecementeerde horizont) binnen 100 cm diepte \n* Gypsids - aridisols met al dan niet verharde gipshoudende horizont (gypsic) binnen 100 cm diepte \n* Argids - aridisols met een kleiinspoelingshorizont (argillic), al dan niet met een hoog natriumgehalte binnen 100 cm diepte \n* Calcids - aridosols met een al dan niet verharde horizont met een aanrijking van CaCO3 binnen 100 cm \n* Cambids - overige aridisols In de World Reference Base for Soil Resources (WRB) komen de Aridisolen overeen met onder meer Solonchaks, Durisolen en Gypsisolen." , "lang" : "nl" } , { "type" : "literal", "value" : "Arid soils (or desert soils) are a soil order in USDA soil taxonomy. Aridisols (from the Latin aridus, for \"dry\", and solum) form in an arid or semi-arid climate. Aridisols dominate the deserts and xeric shrublands, which occupy about one third of the Earth's land surface. Aridisols have a very low concentration of organic matter, reflecting the paucity of vegetative production on these dry soils. Water deficiency is the major defining characteristic of Aridisols. Also required is sufficient age to exhibit subsoil weathering and development. Limited leaching in aridisols often results in one or more subsurface soil horizons in which suspended or dissolved minerals have been deposited: silicate clays, sodium, calcium carbonate, gypsum or soluble salts. These subsoil horizons can also be cemented by carbonates, gypsum or silica. Accumulation of salts on the surface can result in salinization. In the World Reference Base for Soil Resources (WRB), most Aridisols belong to the Calcisols, Gypsisols, Durisols and Solonchaks." , "lang" : "en" } , { "type" : "literal", "value" : "Als Aridisol bezeichnet man gem\u00E4\u00DF der USDA Soil Taxonomy kalkhaltige W\u00FCsten-B\u00F6den aus den Tropen und gem\u00E4\u00DFigten Breiten, die sich in Regionen trockenen Klimas ausbilden. Zu den Aridisolen geh\u00F6ren im Einzelnen: \n* \n* \n* Solontschake (Wei\u00DFalkalib\u00F6den) \n* Solonetze (Schwarzalkalib\u00F6den) \n* Rohb\u00F6den Sie finden sich insbesondere im westlichen S\u00FCdamerika entlang der Andenkette, in den westlichen USA landeinw\u00E4rts der Rocky Mountains, in S\u00FCdwestafrika und den n\u00F6rdlichen K\u00FCstenregionen dieses Kontinents, im Nahen Osten inklusive Arabiens und am Horn von Afrika, im Iran, in Afghanistan und gro\u00DFen Teilen Zentralasiens bis in die Volksrepublik China hinein sowie in Australien. Die leicht alkalischen bis neutralen B\u00F6den besitzen gew\u00F6hnlich kein gut entwickeltes Bodenprofil, lassen aber eine schwache Horizontbildung erkennen. In gr\u00F6\u00DFeren Tiefen enthaltenes Wasser wird durch Kapillarwirkung mitsamt den darin gel\u00F6sten Salzen an die Oberfl\u00E4che gezogen, wo es verdunstet; als Folge bleibt oft eine d\u00FCnne Salzschicht zur\u00FCck. Daneben findet man h\u00E4ufig auch Gips-, Lehm- oder Kalkbestandteile. Anders als bei Vertisolen, die sich in Regionen mit ausgepr\u00E4gten Trocken- und Regenzeiten finden, bilden Aridisole allerdings keine tiefgehenden Bodenspalten aus. Obwohl Aridisole durch Bew\u00E4sserung zu sehr fruchtbaren B\u00F6den werden k\u00F6nnen, auf denen etwa Weizen angebaut werden kann, wachsen aufgrund des sehr niedrigen Feuchtigkeitsgehaltes normalerweise nur sehr wenige trockenheitsangepasste Pflanzen. Als Folge enthalten diese B\u00F6den nur sehr wenig organisches Material und sind durch den geringen Pflanzenbewuchs auch extrem erosionsgef\u00E4hrdet \u2013 erodierte Aridisole werden wieder zu unentwickelten B\u00F6den, den Entisolen. Weltweit sind etwa 15,7 Millionen Quadratkilometer oder 12 Prozent der eisfreien Landfl\u00E4che von Aridisolen bedeckt." , "lang" : "de" } , { "type" : "literal", "value" : "\u0627\u0644\u062A\u0631\u0628\u0629 \u0627\u0644\u062C\u0627\u0641\u0629 \u0623\u0648 \u062A\u0631\u0628\u0629 \u0627\u0644\u0635\u062D\u0631\u0627\u0621 \u0623\u0648 \u0623\u0631\u064A\u062F\u0633\u0648\u0644 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Aridisol)\u200F\u060C \u0647\u0648 \u0623\u062D\u062F \u0623\u0646\u0638\u0645\u0629 \u062A\u0635\u0646\u064A\u0641 \u0627\u0644\u062A\u0631\u0628\u0629 \u0627\u0644\u0623\u0645\u0631\u064A\u0643\u064A \u0644\u0648\u0643\u0627\u0644\u0629 \u062D\u0641\u0638 \u0627\u0644\u0645\u0648\u0627\u0631\u062F \u0627\u0644\u0637\u0628\u064A\u0639\u064A\u0629 \u0628\u0627\u0644\u0648\u0644\u0627\u064A\u0627\u062A \u0627\u0644\u0645\u062A\u062D\u062F\u0629. \u0633\u0628\u0628 \u062A\u0633\u0645\u064A\u062A\u0647\u0627 \u0628\u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u062C\u0627\u0641\u0629 \u062A\u0646\u062E\u0641\u0636 \u0628\u0647\u0627 \u0646\u0633\u0628\u0629 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0639\u0636\u0648\u064A\u0629 \u0648\u063A\u0646\u064A\u0629 \u0628\u0627\u0644\u0623\u0645\u0644\u0627\u062D \u0627\u0644\u0645\u062A\u0631\u0633\u0628\u0629\u060C \u0628\u0647\u0627 \u0634\u062D \u0645\u064A\u0627\u0647 \u0648\u0628\u0627\u0644\u062A\u0627\u0644\u064A \u0636\u0639\u0641 \u0625\u0644\u0649 \u0627\u0646\u0639\u062F\u0627\u0645 \u0627\u0644\u0625\u0646\u062A\u0627\u062C \u0627\u0644\u0646\u0628\u0627\u062A\u064A." , "lang" : "ar" } , { "type" : "literal", "value" : "Aridisol adalah kondisi tanah, lingkungan, atau daerah yang kering. Tanah aridisol memiliki kandungan organik rendah. Aridisol mengandung lempung, kalsium karbonat, silika, garam, dan/atau gipsum yang telah terakumulasi. Kutub dingin, gurun beriklim sejuk, dan gurun hangat termasuk ke dalam daerah aridisol. Ketiga hal tersebut jika dikualifikasikan berdasarkan iklim yakni menempati 36% permukaan tanah dan jika dikualifikasikan berdasarkan vegetasi yakni menempati 35%. Aridisol juga dapat terjadi di daerah semi-kering. 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