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ORIGINAL PAPER
Sustainable nitrogen release and changes in soil properties induced by composite biochar-manure pellets with mineral additives
 
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1
Division of Agricultural and Environmental Chemistry, Institute of Agriculture, Warsaw University of Life Sciences – SGGW, Nowoursynowska Str. 159, 02-776 Warsaw, Poland
 
2
Institute of Horticulture – National Research Institute (INHORT), Konstytucji 3 Maja Str. 1/3, 96-100 Skierniewice, Poland
 
 
Submission date: 2025-11-24
 
 
Final revision date: 2026-01-20
 
 
Acceptance date: 2026-02-23
 
 
Online publication date: 2026-02-23
 
 
Publication date: 2026-02-23
 
 
Corresponding author
Tomasz Niedziński   

Faculty of Agriculture and Ecology, Division of Agricultural Chemistry, Institute of Agriculture, Warsaw University of Life Sciences-SGGW, Nowoursynowska 159, 02-776, Warsaw, Polska
 
 
Soil Sci. Ann., 2026, 77(1)218478
 
KEYWORDS
ABSTRACT
Composite biochar-manure-mineral pellets were evaluated under 100-day incubation conducted under controlled laboratory conditions to elucidate mechanisms controlling nitrogen transformation and soil chemical buffering. Eight formulations combining biochar from various feedstocks, poultry manure, gypsum, lime, and organic substrates were tested on Luvisol soil and designed to represent contrasting pellet chemistries. Soil pH initially increased to 6.7 in lime- and gypsum-enriched variants, then gradually declined, whereas mushroom substrate and fruit-stone biochar maintained near-neutral pH (>6.0) at the end of incubation. Electrical conductivity rose steadily from 102 to 1100–1180 µS cm-1 in manure-gypsum treatments, confirming controlled ionic release without salinity stress. Ammonium reached 250 mg N kg-1 (G1–G3) before gradually converting to nitrate, which peaked above 200 mg N kg-1 by day 100. The rate of Kjeldahl nitrogen change from the granules was moderate, with 62–92% of the initial content remaining at the end of incubation. The results reveal dual-phase kinetics: early nitrate accumulation in soil followed by delayed intragranular peaks, driven by oxygen diffusion and pH-dependent nitrification. Integration of biochar, gypsum, and lime produced three synergistic buffering effects: temporal (delayed nitrification), chemical (pH stabilization), and hydro-ionic (gradual ECe evolution). These findings establish a basis for designing composite organo-mineral fertilizers that synchronize nitrogen release with soil microbial activity while minimizing acidification and nutrient losses.
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