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  • Soil organic matter positively affects the development of structural elements and therefore it is important to supply organic matter to the soil. In terms of soil protection before water erosion are important structural aggregates. Soil structure is defined as the arrangement of particles and associated pores in soils across the size. The aim of this paper is to highlight the impact of water erosion on soil structure and soil organic matter Chernozem on loess in southern Moravia, and process the correlation between soil organic matter and macroaggregates. Soil organic matter was determined by determining the total carbon content on the wet road method Walkley - Black. The structure was determined by a modified method according to Novák. The stability of soil structure in the arable layer was highest at site Domanín u Bzence in the top position, which reaches 89%. The lowest coefficient stability is of site Svatobořice-Mistřín, where it reaches only 15% in the middle of the slope. There is a positive correlation between the organic matter content of the soil and aggregation. Positive Spearman correlation relationship macroaggregates and humus content, we managed to prove only one case at the site Domanín u Bzence.
  • Soil organic matter positively affects the development of structural elements and therefore it is important to supply organic matter to the soil. In terms of soil protection before water erosion are important structural aggregates. Soil structure is defined as the arrangement of particles and associated pores in soils across the size. The aim of this paper is to highlight the impact of water erosion on soil structure and soil organic matter Chernozem on loess in southern Moravia, and process the correlation between soil organic matter and macroaggregates. Soil organic matter was determined by determining the total carbon content on the wet road method Walkley - Black. The structure was determined by a modified method according to Novák. The stability of soil structure in the arable layer was highest at site Domanín u Bzence in the top position, which reaches 89%. The lowest coefficient stability is of site Svatobořice-Mistřín, where it reaches only 15% in the middle of the slope. There is a positive correlation between the organic matter content of the soil and aggregation. Positive Spearman correlation relationship macroaggregates and humus content, we managed to prove only one case at the site Domanín u Bzence. (en)
Title
  • Soil aggregate stability and soil organic matter on Chernozems of South Moravia
  • Soil aggregate stability and soil organic matter on Chernozems of South Moravia (en)
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  • Soil aggregate stability and soil organic matter on Chernozems of South Moravia
  • Soil aggregate stability and soil organic matter on Chernozems of South Moravia (en)
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  • RIV/62156489:43210/14:00230324!RIV15-MSM-43210___
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  • 45826
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  • RIV/62156489:43210/14:00230324
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  • macroaggregates; Chernozem; soil; soil organic matter; water erosion; soil structure (en)
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  • [DCAC6FA0E64B]
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  • Brno, Czech Republic
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  • Brno, Czech Republic
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  • MendelNet 2014 - Proceedings of International PhD Students Conference
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  • Jandák, Jiří
  • Vlček, Vítězslav
  • Hammerová, Anna
  • Šimečková, Jana
  • Mičulková, Beáta
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  • Mendel University in Brno
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  • 978-80-7509-174-1
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  • 43210
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