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Soils of the European Union - European Soil Portal - Europa

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4.6 CalcisolsGeographical distributionCalcisols cover less than 10,000 km 2 , only 0.22% <strong>of</strong> <strong>the</strong> land surface <strong>of</strong> <strong>the</strong> <strong>European</strong> <strong>Union</strong>. Calcisols occur in twocountries, being dominant on <strong>the</strong> islands <strong>of</strong> Malta and covering about 1.7% <strong>of</strong> total land area <strong>of</strong> Spain. The Reference <strong>Soil</strong>Group <strong>of</strong> Calcisol appears 34 times as dominant and 38 cases as associated (with ra<strong>the</strong>r high share <strong>of</strong> 30-50%) within <strong>the</strong>irpolygons.Two soil units are represented in <strong>the</strong> <strong>European</strong> <strong>Union</strong> from <strong>the</strong> Calcisol Reference <strong>Soil</strong> Group, dominated (>95%) byAridic Calcisol. (Table 4.6, Figure 4.6)Table 4.6 Area <strong>of</strong> <strong>the</strong> second level units <strong>of</strong> CalcisolsUnits in <strong>the</strong> Reference <strong>Soil</strong> Groupin <strong>the</strong> EUCodes <strong>of</strong>soil unitsArea in <strong>the</strong> EUkm 2Aridic Calcisol CLad 8972Haplic Calcisol CLha 317Among <strong>the</strong> two soil units <strong>of</strong> <strong>the</strong> Calcisol Reference <strong>Soil</strong> Group Aridic Calcisols can be found in Spain, while <strong>the</strong> Maltesesoils are fall into <strong>the</strong> Haplic category.3.41%CLadCLha96.59%Global referenceFigure 4.6 Share <strong>of</strong> <strong>the</strong> second level soil units in <strong>the</strong> area <strong>of</strong> CalcisolsCalcisols are soil with significant accumulation <strong>of</strong> secondary calcium carbonates, generally developed in dry areas. <strong><strong>Soil</strong>s</strong>belonging to this Reference <strong>Soil</strong> Group are common on calcareous parent material in regions with distinct dry seasons, aswell as in dry areas where carbonate-rich groundwater comes near <strong>the</strong> surface. The total Calcisol area amounts to some 10million km 2 , nearly all <strong>of</strong> it in <strong>the</strong> arid and semi-arid (sub)tropics <strong>of</strong> both hemispheres.Many Calcisols are old soils if counted in years but <strong>the</strong>ir development was slowed down by recurrent periods <strong>of</strong> drought inwhich such important soil forming processes as chemical wea<strong>the</strong>ring, accumulation <strong>of</strong> organic matter and translocation <strong>of</strong>clay came to a virtual standstill. However, most Calcisols have substantial movement and accumulation <strong>of</strong> calciumcarbonatewithin <strong>the</strong> soil pr<strong>of</strong>ile. The precipitation may occur as pseudomycelium (root channels filled with fine calcite),nodules or even in continuous layers <strong>of</strong> s<strong>of</strong>t or hard lime (calcrete).Most Calcisols have a thin (=

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