PRACA ORYGINALNA
The dynamics of mobile iron compounds and redox potential of Albic Pantostagnic Luvisol depending on long-term various fertilisation
1
Department of Agrochemistry and Soil Science, Institute of Agriculture of Carpathian region National Academy of Agrarian Sciences, Ukraine
2
Department of Agrochemistry and Soil Science, Lviv National Environmental University, Ukraine
Data nadesłania: 08-07-2024
Data ostatniej rewizji: 16-10-2024
Data akceptacji: 14-11-2024
Data publikacji online: 14-11-2024
Data publikacji: 14-11-2024
Autor do korespondencji
Yurii Olifir
Department of Agrochemistry and Soil Science, Institute of Agriculture of Carpathian region National Academy of Agrarian Sciences, Hrushevskoho str., 5, 81115, Obroshyne, Ukraine
Department of Agrochemistry and Soil Science, Institute of Agriculture of Carpathian region National Academy of Agrarian Sciences, Hrushevskoho str., 5, 81115, Obroshyne, Ukraine
Soil Sci. Ann., 2024, 75(4)195939
SŁOWA KLUCZOWE
STRESZCZENIE
Iron is one of the most important trace elements in plant nutrition. The content of ferric iron and ferrous oxide in the soil and their dynamics during the vegetation period can be used to assess not only the course of oxidation-reduction processes but also the supply of plants with this available trace element. Therefore, the main objective of the research was to find out the effect of long-term fertilisation and liming on the dynamics of the redox potential and mobile iron compounds in the Albic Pantostagnic Luvisol of the forest-steppe of Western Ukraine. The research was conducted under the conditions of a long-term experiment established in 1965 with different doses of mineral fertilisers, manure, and lime on the Albic Pantostagnic Luvisol. It was found that the gross content of iron compounds and the content of their mobile forms in the Albic Pantostagnic Luvisol are within the optimal range for the plant's growth and development. Only in the case of long-term use of this soil without fertilisation or in the conditions of long-term mineral fertilisation, which contributes to the increase of the acidity of the soil solution and to the creation of restoring conditions during the periods of overwetting, iron can turn into a toxic substance.
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