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- W986667609 abstract "The Mg content in individual granulometric fractions of the soils studied was found to be inversely proportional to the fraction diameter. The >0.02 mm diameter fraction separated from soils originating from loess were between 60 and 130%, richer in magnesium than the same fractions separated from Carpathian soils, at 80% on average. It has been found that the lower the content of a given granulometric fraction in the soil, the higher its share in the distribution of the total magnesium pool in the soil. Hence, in light soils with a low content of the <0.02 mm fraction, the share in the accumulation of the total Mg pool in the soil mass is considerably higher than in the case of similar fractions of heavy soils that are richer in the <0.02 mm fraction, and also in the colloidal fraction of <0.002 mm. Magnesium is an indispensable element for the normal functioning of the organisms of both plants and animals. From the quantitative point of view, it is the eighth most common element in the Earth's crust (11), and forms part of a group of minerals found in magma and deposit rocks. In the surface layers, where the lithosphere has been transformed into soils, the magnesium content is exceptionally low, especially in the part accessible to plants. Several studies have shown that the main storage of biogenic components is in the clayey fractions (1-7, 9-10, 12-14). Detailed studies were made into the quantitative distribution of magnesium of groups separated from the soil granulometric fractions. Soils originating from two geological formations with differentiated granulations and typologies were selected for the studies, and these included acidic brown soils originating from P O L I S H J O U R N A L O F S O I L S C I E N C E" @default.
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- W986667609 date "2010-01-01" @default.
- W986667609 modified "2023-09-23" @default.
- W986667609 title "QUANTITATIVE MAGNESIUM DISTRIBUTION IN GRANULOMETRIC FRACTIONS OF SOME SOILS" @default.
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