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首页> 外文期刊>Moscow University Soil Science Bulletin >Biomorph silica in meadow soils of the Mid-Amur lowland.
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Biomorph silica in meadow soils of the Mid-Amur lowland.

机译:中阿穆尔低地草甸土壤中的生物形态二氧化硅。

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摘要

On the basis of an analysis of the gross composition and morphology of the particles of soil samples from the Mid-Amur lowlands, it is shown that the biomorph silica of the meadow soils with bleached horizons is represented by meadow forms of phytoliths (mainly true grasses). In the upper profile part of the AUg horizon, frustules of diatom algae are found, while no spicules of sponges are registered. The upper part of the profile is characterized by the highest degree of weathering of the phytolith silica. In the lower part, they are better preserved. In this part of the profile, diatoms are represented by small-celled species around 2 micro m in size (supposedly, spores of Cyclotella sp.). The presence of such algae in the water-peptized silt is associated with the process of migration down the profile.Notes Translated from Vestnik Moskovskogo Universiteta. Pochvovedenie (2013) (1), 37-45 (Ru).
机译:在对中阿穆尔河低地土壤样品的总组成和颗粒形态进行分析的基础上,研究表明,具有漂白层位的草甸土壤的生物形态二氧化硅以草甸形式的植硅石(主要是真草)为代表。 )。在AUg地层的上剖面部分,发现了硅藻藻类的结节,而没有海绵状的针状结节。轮廓的上部的特征在于植硅石二氧化硅的风化程度最高。在下部,它们保存得更好。在此部分的剖面图中,硅藻由大小约为2微米的小细胞物种(据说是Cyclotella sp。的孢子)代表。在水溶淤泥中这种藻类的存在与沿剖面向下迁移的过程有关。注释译自Vestnik Moskovskogo Universiteta。 Pochvovedenie(2013)(1),37-45(Ru)。

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