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Forms of A l in soil and soil solution in a long‐term fertilizer application experiment
Author(s) -
Rutkowska B.,
Szulc W.,
Hoch M.,
SpychajFabisiak E.
Publication year - 2015
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/sum.12150
Subject(s) - chemistry , fertilizer , soil water , aluminium , amendment , manure , organic matter , environmental chemistry , soil ph , agronomy , soil science , environmental science , biology , organic chemistry , political science , law
Under the conditions of a long‐term fertilizer experiment, this study aimed to determine the contents of total and exchangeable aluminium in soil as well as the Al concentration in the soil solution. Additionally, Al speciation was evaluated with the use of the MINTEQA2 software. The results obtained indicated that under the conditions of long‐term application of different mineral fertilizers or farmyard manure, the soil reaction changed to a great extent ( pH 3.58–6.78). At the same time, the content of total Al in soil fluctuated from 18.85 to 22.13 g/kg and that of exchangeable Al ranged from 1.42 to 102.66 mg/kg. The concentration of Al in the soil solution was highly differentiated (5.19–124.07 μ mol/L) as well as that of free aluminium ions (Al 3+ ) (0–16.9 μ mol/L). In acidic soils, aluminium complexes with organic matter are the predominant forms of Al in the soil solution. In soils with neutral soil reaction, there were no free aluminium ions. Soil liming and addition of organic amendment were the treatments that restricted the presence of toxic aluminium forms in soil.