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International Agrophysics |
wydawca: | Instytut Agrofizyki
im. B. Dobrzańskiego
PAN
w Lublinie |
ISSN: |
0236-8722 |
vol. 9, nr. 3 (1995)
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poprzedni artykuł wróć do listy artykułów następny artykuł |
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The structural state of soils on loesses |
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T. Alekseeva1, A. Alekseev 1, Y. Morgun1, , G. Józefaciuk2 |
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1 Institute of Soil Science and Photosynthesis, Russian Academy of Sciences, Puschino, Moscow Region, 142292 Russia |
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2 Institute of Agrophysics, Polish Academy of Sciences, DoŁwiadczalna 4,20-236 Lublin, Poland |
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vol. 9 (1995), nr. 3,
pp. 171-178
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streszczenie
Amount and mineralogy of clay material separated from four geochemically linked loessial soil samples of various genesis due to a sequential dissolution of aggregating agents were studied by X-ray dif-fractometry, Mossbauer spectroscopy and magnetic measurements. Some regularities in the distribution of mineral (crystalline and amorphous) and organic soil compounds as related to pedoenvironmental conditions, were observed.
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słowa kluczowe
loessial soil, aggregation structure, sequential disruption
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