Approaches to the sollution of a soil map of the Czech Republic at the scale 1:250.000 using SOTER methodology

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41210%2F03%3A00005920" target="_blank" >RIV/60460709:41210/03:00005920 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Approaches to the sollution of a soil map of the Czech Republic at the scale 1:250.000 using SOTER methodology

Popis výsledku v původním jazyce

Soil map at the scale 1:250.000 was set up by menas of transformation of the published and later digitised soil map of theCzech Republic. The legend to this map reflects a new classification systemof Czech soils that can easily be correlated swith the reference international classification system FAO-WRB. In the next step this map was converted into the SOTER system, which links the soil cover tothe geomorphology. The modification of the original SOTER procedure consisted in the abandoning of the consequent hierarchy geomorphology-lithology-soil associations. Only in terriotories characterised by rather shallow transpored slope deposits over compact or consolidated rocks was this principle observed in the SOTER unit delimination. In flat landscapes covered with deep sediment deposits the prevailing soil cover (mosaics of taxonomic units and their parent materials) determines the borders of SOTER units. Ten major landscape units were delineated. They re based on relief intensity and hyp

Název v anglickém jazyce

Approaches to the sollution of a soil map of the Czech Republic at the scale 1:250.000 using SOTER methodology

Popis výsledku anglicky

Soil map at the scale 1:250.000 was set up by menas of transformation of the published and later digitised soil map of theCzech Republic. The legend to this map reflects a new classification systemof Czech soils that can easily be correlated swith the reference international classification system FAO-WRB. In the next step this map was converted into the SOTER system, which links the soil cover tothe geomorphology. The modification of the original SOTER procedure consisted in the abandoning of the consequent hierarchy geomorphology-lithology-soil associations. Only in terriotories characterised by rather shallow transpored slope deposits over compact or consolidated rocks was this principle observed in the SOTER unit delimination. In flat landscapes covered with deep sediment deposits the prevailing soil cover (mosaics of taxonomic units and their parent materials) determines the borders of SOTER units. Ten major landscape units were delineated. They re based on relief intensity and hyp

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DF - Pedologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA526%2F00%2F0620" target="_blank" >GA526/00/0620: Digitální půdně-stanovištní mapa ČR v systému SOTER</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2003

Kód důvěrnosti údajů

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

Název periodika

Plant, Soil and Environment

ISSN

1214-1178

e-ISSN

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Svazek periodika

49

Číslo periodika v rámci svazku

7

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

7

Strana od-do

291-297

Kód UT WoS článku

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EID výsledku v databázi Scopus

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