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Impact of alfalfa and NPK fertilization in agricultural reclamation on the transformation of Technosols in an area following lignite mining

Bibliographic Data

ID21648786
AuthorsKrzysztof Otremba (0000-0001-9035-5566, Department of Soil Science and Reclamation Poznań University of Life Sciences Poznań Poland), Michal Kozlowski (0000-0002-0889-928X, Department of Soil Science and Reclamation Poznań University of Life Sciences Poznań Poland), Natalia Tatuśko‐Krygier (0000-0002-6842-2125, Department of Soil Science and Reclamation Poznań University of Life Sciences Poznań Poland), Marek Pająk (0000-0002-6946-8803, Department of Forest Ecology and Reclamation University of Agriculture in Kraków Kraków Poland), Beata Kołodziej (0000-0002-2637-2764, University of Life Sciences in Lublin, corresponding author), Maja Bryk (0000-0002-2291-1492, University of Life Sciences in Lublin)
Year2021
Volume32
Issue3
Pages1179-1191
Publication date2021-02-15
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.3781
OpenAlexW3088739606
LanguageEN
Citations received2
References cited45

Open‐cast mining of lignite leads to considerable degradation of the natural environment, which then must be reclaimed. The aim of this study was to assess the transformation of Technosols in an area after lignite mining which had been under 40‐year cultivation of alfalfa with grass at various NPK fertilization rates. We hypothesized that 40‐year cultivation of plants caused morphological transformation of the parent material and resulted in differentiation of physical and chemical properties in the profile of the Technosols; fertilization had an added advantageous effect on their properties. The surface layer was transformed into an Ap‐horizon. Under alfalfa, with grass and NPK fertilization, Ap‐horizons demonstrated lower bulk density (BD) (7–11%) and particle density (PD) (1–2%), and higher total porosity (TP) (18–35%), drainable porosity (DP) (2–94%), field water capacity (FC) (11–21%), unavailable water (UW) (4–17%), soil organic carbon (SOC) (80–142%), total nitrogen (TN) (261–330%), available P (39–435%), available K (32–89%), cation exchange capacity (CEC) (25–43%), and soil acidity ( H ext ) (42–81%) compared to Cd‐horizons. Fertilized Technosols (1NPK, 2NPK), compared with control (0NPK), showed in the Ap‐horizon an increase in SOC (18–35%), TP (8–15%), DP (81–90%), FC (9–10%), P (110–285%), K (14–71%), and TN (0–18%), and a decrease in BD (4–7%). In contrast, fertilization had no effect on the UW, PD, soil inorganic carbon (SIC), CaCO 3 , available Mg, and pH KCl . The alfalfa and orchard grass played a key role in the reclamation and soil‐forming processes, while fertilization played a supporting role

Agronomy · Biology · Bulk density · Cation-exchange capacity · Fertilizer · Human fertilization · Land reclamation · Soil carbon · Soil horizon · Soil water · Chemistry · Environmental Science · Peatlands and Wetlands Ecology · Soil and Water Nutrient Dynamics · Soil Carbon and Nitrogen Dynamics · Ecology · Environmental Chemistry · Soil Science

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Citations per year0.67
Citation span2023 - 2023 (1)
Highly citedNo

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