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Effect of long-term organic and mineral fertilisation on selected physico-chemical soil properties in rye monoculture and five-year crop rotation
Author(s) -
Wojciech Stępień,
Monika Kobiałka
Publication year - 2019
Publication title -
roczniki gleboznawcze/soil science annual
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.432
H-Index - 12
eISSN - 2300-4967
pISSN - 0080-3642
DOI - 10.2478/ssa-2019-0004
Subject(s) - monoculture , fertilisation , agronomy , crop rotation , nitrogen , long term experiment , chemistry , manure , soil carbon , soil horizon , soil water , fertilizer , environmental science , crop , soil science , biology , biochemistry , reproductive technology , organic chemistry , embryogenesis , gene
The research was carried out continuously since 1923 in a permanent fertilisation experiment at the Experimental Station of SGGW in Skierniewice. The objective of the research was to determine the effect of long-term fertilisation (Ca, CaNPK, NPK) and crop rotation systems (rye monoculture without fertilisation with manure and five-field rotation with legume crop and manure fertilisation) on selected physical and chemical soil properties. Long-term fertilisation caused various degrees of change in many physio-chemical properties in three soil horizons (A p , E et , B t ): pH in KCl, cation exchange capacity, total exchangeable bases, base saturation, content of carbon, nitrogen and mineral forms of nitrogen (NO 3 , NH 4 ) as well as the carbon-nitrogen ratio. The combined manure and mineral fertilisation increased the sorption capacity, total exchangeable bases, base cation saturation and total content of C and N in comparison to organic or mineral fertilisation. As a result of lime application, an increase in these parameters was determined with the exception of total contents of carbon and nitrogen, showing no differences or a decrease. A positive effect was confirmed in five-field crop rotation, which improves physicochemical soil properties in comparison to cereal monoculture. The C:N ratio narrows down with growing depth because more nitrogen than carbon migrates down the soil profile.

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