Abstract
The study, aimed to determine the properties of peat soil (Pachiterric Histosol, HSs-ph) as influenced by different land use, was carried out in two sites – in Varėna (South Lithuania, 53°57′11.98′′ N, 24°19′02.07′′ E) and Radviliskis (Central Lithuania, 55°49′43.19′′ N, 23°28′36.34′′ E) districts. During the renaturalization of drained Pachiterric Histosol, an intensive mineralization in the 0–30 cm soil is taking place; therefore the concentrations of organic carbon and labile organic carbon are unfavourable for the soil. The distribution of total N and P in profile of Pachiterric Histosol is directly related to the vertical gradient of mineralization intensity; higher contents of N and P accumulated where mineralization was more intensive. The distribution of total K is related to land use of Pachiterric Histosol, whereas the highest quantity of total K was established in arable land which had been fertilised with mineral fertilizers.
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