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Porosity and water useful for plants in Luvisols created from sandy silt and silt

机译:沙质淤泥和淤泥产生的Luvisols中植物有用的孔隙度和水

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摘要

The results of the studies concerning the total and the differential porosity in Luvisols profiles created from sandy-sift and loess were presented. It has been stated that the total porosity of the soils created from sandy-silt formations was smallerthan in the soils of loess origin and the differences were the most evident in the upper parts of the profiles of the forest soils. The amount of macropores in the forest soils, created from both parent materials was considerably higher than in the arable soils, while the soils created from sandy-silt formations were characterized by generally lower amount of mesopores and micropores than in the soils created from loess. The amount of water easily available for plants was considerably lower in the soils created from sandy-silt formations than in the soils of loess origin - it was especially well seen for the forest soils. The amount of water difficult available for plants was generally considerably higher than the amount of water easily available, inall the investigated soil profiles and it practically did not depend on the kind of parent material.
机译:提出了有关由沙滤和黄土形成的Luvisols剖面中总孔隙度和微分孔隙度的研究结果。有人说,由沙质粉尘形成的土壤的总孔隙度比黄土来源的土壤小,而且差异最大的是在森林土壤剖面的上部。由两种母体材料产生的森林土壤中的大孔数量要比可耕种土壤中的高得多,而由沙粉砂岩层形成的土壤的中孔和微孔的数量通常比由黄土形成的土壤要少。在沙质粉尘形成的土壤中,植物容易获得的水量比黄土来源的土壤要低得多-在森林土壤中尤为明显。在所有调查的土壤剖面中,植物难获取的水量通常比易获取的水量高得多,并且实际上不取决于母体材料的种类。

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