| Attributes | Values |
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| rdf:type
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| Description
| - Na území České republiky je více jak 50 % zemědělské půdy ohroženo vodní erozí (Janeček et al., 2002), to pro současné hospodaření, ale především pro budoucnost představuje velmi závažný problém, který se musí řešit teď, dokud máme ještě co chránit. Charakterizovat půdní vlastnosti ve vztahu k náchylnosti půdy k vodní erozi je značně komplikované, protože se jedná o složitý vztah, ve kterém hraje roli ještě celá řada dalších faktorů. Komplexní posouzení všech hlavních činitelů podílejících se na vzniku eroze, řeší stále nejpoužívanější a nejznámější tzv. univerzální rovnice pro výpočet dlouhodobé ztráty půdy vodní erozí (dále USLE) podle Wischmeiera a Smithe (1978). Ta se skládá ze šesti faktorů, které se především a ve vzájemném působení podílejí na vzniku eroze půdy. Jedním z těchto faktorů je faktor erodovatelnosti půdy (K – faktor), jehož stanovením pro půdní poměry ČR, se zabývá tato práce. (cs)
- In the territory of the Czech Republic there are more than 50% of agricultural soils exposed to water erosion. It is rather complicated to describe the soil properties in terms of soil susceptibility to water erosion because it is a complex relation in which many factors participate. For the complex evaluation of all main factors participating in erosion origination it is possible to apply the USLE. It consists of six factors interacting with each other and participating in the origination of soil erosion. One of these factors is the soil erodibility factor (K), the revision of which for soil conditions of the CR is the subject of this study. In total ca. 5000 soil pits from the whole territory of the country were processed and evaluated in detail. The main results of this study are K-factor values (means and variances) for the soil types, subtypes and varieties (represented in the database) according to the Taxonomic Classification System of Soils of the Czech Republic.
- In the territory of the Czech Republic there are more than 50% of agricultural soils exposed to water erosion. It is rather complicated to describe the soil properties in terms of soil susceptibility to water erosion because it is a complex relation in which many factors participate. For the complex evaluation of all main factors participating in erosion origination it is possible to apply the USLE. It consists of six factors interacting with each other and participating in the origination of soil erosion. One of these factors is the soil erodibility factor (K), the revision of which for soil conditions of the CR is the subject of this study. In total ca. 5000 soil pits from the whole territory of the country were processed and evaluated in detail. The main results of this study are K-factor values (means and variances) for the soil types, subtypes and varieties (represented in the database) according to the Taxonomic Classification System of Soils of the Czech Republic. (en)
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| Title
| - Revised soil erodibility k - factor for soils in the Czech Republic
- Revised soil erodibility k - factor for soils in the Czech Republic (en)
- Nové určení faktoru erodovatelnosti půd K pro půdy v České republice (cs)
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| skos:prefLabel
| - Revised soil erodibility k - factor for soils in the Czech Republic
- Revised soil erodibility k - factor for soils in the Czech Republic (en)
- Nové určení faktoru erodovatelnosti půd K pro půdy v České republice (cs)
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| skos:notation
| - RIV/00027049:_____/07:#0000207!RIV08-MZE-00027049
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| http://linked.open.../vavai/riv/strany
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| http://linked.open...avai/riv/aktivita
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| http://linked.open...avai/riv/aktivity
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| http://linked.open...iv/cisloPeriodika
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| http://linked.open...vai/riv/dodaniDat
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| http://linked.open...aciTvurceVysledku
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| http://linked.open.../riv/druhVysledku
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| http://linked.open...iv/duvernostUdaju
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| http://linked.open...titaPredkladatele
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| http://linked.open...dnocenehoVysledku
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| http://linked.open...ai/riv/idVysledku
| - RIV/00027049:_____/07:#0000207
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| http://linked.open...riv/jazykVysledku
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| http://linked.open.../riv/klicovaSlova
| - water erosion; soil erodibility; soil structure; organic matter (en)
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| http://linked.open.../riv/klicoveSlovo
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| http://linked.open...odStatuVydavatele
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| http://linked.open...ontrolniKodProRIV
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| http://linked.open...i/riv/nazevZdroje
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| http://linked.open...in/vavai/riv/obor
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| http://linked.open...ichTvurcuVysledku
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| http://linked.open...cetTvurcuVysledku
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| http://linked.open...vavai/riv/projekt
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| http://linked.open...UplatneniVysledku
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| http://linked.open...v/svazekPeriodika
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| http://linked.open...iv/tvurceVysledku
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| issn
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| number of pages
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| is http://linked.open...avai/riv/vysledek
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