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Effect of mineral and organic fertilization on crop yield, nitrogen uptake, carbon and nitrogen balances, as well as soil organic carbon content and dynamics: results from 20 European long-term field experiments of the twenty-first century

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00027006%3A_____%2F13%3A00002688" target="_blank" >RIV/00027006:_____/13:00002688 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1080/03650340.2012.704548" target="_blank" >http://dx.doi.org/10.1080/03650340.2012.704548</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1080/03650340.2012.704548" target="_blank" >10.1080/03650340.2012.704548</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Effect of mineral and organic fertilization on crop yield, nitrogen uptake, carbon and nitrogen balances, as well as soil organic carbon content and dynamics: results from 20 European long-term field experiments of the twenty-first century

  • Original language description

    The soil improving effect of SOM on yields, i.e. the effect which cannot be reached by a sufficient and equivalent nutrient supply, was 6% (average of 350 yield comparisons form 16 LTEs at 12 different sites, the majority for the period 2001-2010), being lowest for winter wheat (3%) and highest for potatoes (9%). SOC contents in the topsoil of long-term (decades) unfertilized treatments range between 0.36 and 1.57% for 18 analysed sites; SOC differences between unfertilized and optimaIly fertilized treatments are on average 0.3%. Considering that under farm conditions, the 'unfertilized' treatment (i.e. no mineral or organic fertilization over a period of decades) does not exist, relevant SOC differences for farms are often <0.2% (or <9 t ha-I SOC). The course of management-induced (e.g. crop rotation, fertilization, soil tillage) changes in SOC depends on the starting level of SOC; equivalent treatments may lead to an increase in SOC from a low starting level, but a decrease from a high starting level. Bare fallow affects the soil carbon budget most strongly; without organic matter input from harvesting and root residues, the SOC content decreases considerably after a short period of 10 years. To evaluate nitrogen utilization by crops, an atmospheric N input (bulk deposition, gaseous immission, a symbiotic N2 fixation) of up to 50 kg ha-1 a - I has to be considered.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    GC - Plant growing, crop rotation

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

Others

  • Publication year

    2013

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Archives of Agronomy and Soil Science

  • ISSN

    0365-0340

  • e-ISSN

  • Volume of the periodical

    59

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    24

  • Pages from-to

    1017-1040

  • UT code for WoS article

    000321485200001

  • EID of the result in the Scopus database