Specifics of soil temperature under winter wheat canopy

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F13%3A00212079" target="_blank" >RIV/62156489:43210/13:00212079 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.2478/congeo-2013-0013" target="_blank" >http://dx.doi.org/10.2478/congeo-2013-0013</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2478/congeo-2013-0013" target="_blank" >10.2478/congeo-2013-0013</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Specifics of soil temperature under winter wheat canopy

Popis výsledku v původním jazyce

The aim of this study was to evaluate the course of soil temperature under the winter wheat canopy and to determine relationships between soil temperature, air temperature and partly soil moisture. In addition, the aim was to describe the dependence by means of regression equations usable for phytopathological prediction models, crop development, and yield models. The measurement of soil temperatures was performed at the experimental field station Žabčice (Europe, the Czech Republic, South Moravia). Thesoil in the first experimental plot is Gleyic Fluvisol with 49--58 percent of the content particles measuring lower than 0.01 mm, in the second experimental plot, the soil is Haplic Chernozem with 31--32 percent of the content particles measuring lowerthan 0.01 mm. The course of soil temperature and its specifics were determined under winter wheat canopy during the main growth season in the course of three years. Automatic soil temperature sensors were positioned at three depths (0.05,

Název v anglickém jazyce

Specifics of soil temperature under winter wheat canopy

Popis výsledku anglicky

The aim of this study was to evaluate the course of soil temperature under the winter wheat canopy and to determine relationships between soil temperature, air temperature and partly soil moisture. In addition, the aim was to describe the dependence by means of regression equations usable for phytopathological prediction models, crop development, and yield models. The measurement of soil temperatures was performed at the experimental field station Žabčice (Europe, the Czech Republic, South Moravia). Thesoil in the first experimental plot is Gleyic Fluvisol with 49--58 percent of the content particles measuring lower than 0.01 mm, in the second experimental plot, the soil is Haplic Chernozem with 31--32 percent of the content particles measuring lowerthan 0.01 mm. The course of soil temperature and its specifics were determined under winter wheat canopy during the main growth season in the course of three years. Automatic soil temperature sensors were positioned at three depths (0.05,

Druh

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

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

<a href="/cs/project/QJ1230056" target="_blank" >QJ1230056: Vliv očekávaných klimatických změn na půdy České republiky a hodnocení jejich produkční funkce.</a><br>

Návaznosti

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

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Contributions to Geophysics and Geodesy

ISSN

1335-2806

e-ISSN

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Svazek periodika

43

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

15

Strana od-do

209-223

Kód UT WoS článku

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EID výsledku v databázi Scopus

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