Pedotransferové funkce jako metoda odhadu retenčních čar půdní vlhkosti
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41210%2F07%3A22014" target="_blank" >RIV/60460709:41210/07:22014 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Estimation of the Soil Water Retention Curve (SWRC) Using Pedotransfer Functions (PTFs)
Popis výsledku v původním jazyce
Soil hydraulic characteristics, especially the soil water retention curve and hydraulic conductivity, are essential for many agricultural, environmental, and engineering applictions. Their measuremetn is time-consuming and thus costly. Hence, many researchesrs focused on methods enabling their indirect estmation. In this paper, Wöstens continuous pedtransfer functions were applied to the data from a selected locality in the curves, and the informtion about the soil textue, bulk denstiy d, and organic matter content detrmined at the sme time. Own continuous pedotransfer functions were derived, following the methodology used in continuous pedotranser functions. Two types of fitting, 4-parameters and 3-parameters, were tested. In 4-parameters fitting, allparameters of the van Genuchten equation, were otimized, in 3-parameter fititing, only three parameters, were otpimised while the measured value of was set as constant. Based on the result, it can be concluded that the general equations
Název v anglickém jazyce
Estimation of the Soil Water Retention Curve (SWRC) Using Pedotransfer Functions (PTFs)
Popis výsledku anglicky
Soil hydraulic characteristics, especially the soil water retention curve and hydraulic conductivity, are essential for many agricultural, environmental, and engineering applictions. Their measuremetn is time-consuming and thus costly. Hence, many researchesrs focused on methods enabling their indirect estmation. In this paper, Wöstens continuous pedtransfer functions were applied to the data from a selected locality in the curves, and the informtion about the soil textue, bulk denstiy d, and organic matter content detrmined at the sme time. Own continuous pedotransfer functions were derived, following the methodology used in continuous pedotranser functions. Two types of fitting, 4-parameters and 3-parameters, were tested. In 4-parameters fitting, allparameters of the van Genuchten equation, were otimized, in 3-parameter fititing, only three parameters, were otpimised while the measured value of was set as constant. Based on the result, it can be concluded that the general equations
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DF - Pedologie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/1G58095" target="_blank" >1G58095: Předpovědní půdně-agrohydrologické modely retence vody v půdě v ČR a jejich integrace do databází zemí EU</a><br>
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2007
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Soil and Water Research
ISSN
1801-5395
e-ISSN
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Svazek periodika
2
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
10
Strana od-do
113-122
Kód UT WoS článku
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EID výsledku v databázi Scopus
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