Soil aggregate stability and soil organic matter on Chernozems of South Moravia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F14%3A00230324" target="_blank" >RIV/62156489:43210/14:00230324 - isvavai.cz</a>

Výsledek na webu

<a href="http://mnet.mendelu.cz/mendelnet2014/index.php?page=82&lang=eng" target="_blank" >http://mnet.mendelu.cz/mendelnet2014/index.php?page=82&lang=eng</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Soil aggregate stability and soil organic matter on Chernozems of South Moravia

Popis výsledku v původním jazyce

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

Název v anglickém jazyce

Soil aggregate stability and soil organic matter on Chernozems of South Moravia

Popis výsledku anglicky

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

Druh

D - Stať ve sborníku

CEP obor

DF - Pedologie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název statě ve sborníku

MendelNet 2014 - Proceedings of International PhD Students Conference

ISBN

978-80-7509-174-1

ISSN

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e-ISSN

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Počet stran výsledku

6

Strana od-do

260-265

Název nakladatele

Mendel University in Brno

Místo vydání

Brno, Czech Republic

Místo konání akce

Brno, Czech Republic

Datum konání akce

19. 11. 2014

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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