schluff – Traduction – Dictionnaire Keybot

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  Zusammenfassung Heft 13...  
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Die natürlichen Böden bestehen im Oberboden in der Feinerdefraktion etwa zu 70 Gew. % aus Sand (davon rund 70 % Mittelsand),rund 20 Gew. % Schluff und 10 Gew. % Ton. Die Rohböden (Typ I) und die IIC -Horizonte (Unterböden) der Zweischichtböden (Typ
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While the humus contents of the top soil of the natural soils and of the deposited layer of Type II soils average around 1% by weight, humus is generally lacking in the raw soils (Type I) and the raw subsoils (Type II). The total nitrogen contents of 1 g/kg in the developed soils compare to only traces of nitrogen in the raw material (Type I and subsoil of Type II). The supply of nitrogen increases with the amount of deposited material.
  Zusammenfassung Heft 13...  
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Auf ursprünglich stärker carbonathaltigern Substrat fand Tonverlagerung statt, die zum typischen Profilbild einer Parabraunerde mit einer Anreicherung von Ton (und Schluff), von Sesquioxiden und Nährelementen im Illuvialhorizont führte.
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The topsoils of the natural soils contain about 70% by weight sand within the fine earth fraction (of this ca. 70% by weight is medium sand fraction), about 20% by weight silt, and 10? by weight clay. In contrast the raw soils (Type I) and the IlCn horizons (subsoils) of the two-layered soils (Type II) are characterized by proportions of sand in part up to 98% by wei ght.
  Zusammenfassung Heft 42...  
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Die Böden sind stets skelettfrei. Die häufigsten Bodenarten sind sandiger Schluff (Us) und Schluff (U). Die Trockenraumdichte (TRD) liegt im gesamten Bodenprofil relativ homogen bei Werten zwischen 0,40 und 0,60 g/cm3.
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The soils from young and middle aged volcanic ash generally have high available soil moisture levels. Due to rapid litter decomposition in the upper soil, L-Mull (2-4 cm) is the predominant humus form. Underneath the organic layer an Ah-horizon has formed, which is normally underlain by two transition horizons (AB,BA), a B-horizon and a C-horizon. The B-horizon has already completed the process of brunification. In general, volcanic soils are developed deep to very deep (100 - 140 cm). The soils have no skeleton content. The dominating textures are sandy silt (Us) and typical silt (U). The bulk density is relatively homogenious throughout the entire soil profile with values between 0.40 and 0.60 g/cm3. The water storage capacity lies between 200 - 250 mm per 1 m soil depth.
  Zusammenfassung Heft 42...  
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Die Böden sind stets skelettfrei. Die häufigsten Bodenarten sind sandiger Schluff (Us) und Schluff (U). Die Trockenraumdichte (TRD) liegt im gesamten Bodenprofil relativ homogen bei Werten zwischen 0,40 und 0,60 g/cm3.
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The soils from young and middle aged volcanic ash generally have high available soil moisture levels. Due to rapid litter decomposition in the upper soil, L-Mull (2-4 cm) is the predominant humus form. Underneath the organic layer an Ah-horizon has formed, which is normally underlain by two transition horizons (AB,BA), a B-horizon and a C-horizon. The B-horizon has already completed the process of brunification. In general, volcanic soils are developed deep to very deep (100 - 140 cm). The soils have no skeleton content. The dominating textures are sandy silt (Us) and typical silt (U). The bulk density is relatively homogenious throughout the entire soil profile with values between 0.40 and 0.60 g/cm3. The water storage capacity lies between 200 - 250 mm per 1 m soil depth.