Teplota půdy na stanici Pohořelice v období 1961 - 2000
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F06%3A00095939" target="_blank" >RIV/62156489:43210/06:00095939 - 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
The soil temterature at Pohořelice station during the years 1961 -- 2000
Popis výsledku v původním jazyce
Out of the agroclimatological stations of the Czech Hydrometeorological Institute, the soil temperature is being measured by the mercurial soil bent thermometers with range from -30 °C to +45 °C for low depth (5, 10, 20 cm) and in-depth mercurial thermometer with range of -25 °C to +35 °C, which is used for measuring of soil temperature in 50 cm and 100 cm. The evaluation of measurement for the period of 1961 to 2000 at the Pohořelice station, where the soil is formed by chernozems, has brought the following results. On average the soil temperature drops bellow 0 °C in depth of 5 cm from 4th January to 7th February i.e. 35 days and in 10 cm from 10th January to 6th February i.e. 28 days. The absolute maximum of soil temperature during the observed period (12.8 °C) was reached 30th March 1973 in depth 5 and 100 cm and absolute minimum of soil temperature (-9.5 °C) was measured in 5 cm 2nd and 3rd February 1963. The data have been processed by application Surfer 8.0. By the aid of this s
Název v anglickém jazyce
The soil temterature at Pohořelice station during the years 1961 -- 2000
Popis výsledku anglicky
Out of the agroclimatological stations of the Czech Hydrometeorological Institute, the soil temperature is being measured by the mercurial soil bent thermometers with range from -30 °C to +45 °C for low depth (5, 10, 20 cm) and in-depth mercurial thermometer with range of -25 °C to +35 °C, which is used for measuring of soil temperature in 50 cm and 100 cm. The evaluation of measurement for the period of 1961 to 2000 at the Pohořelice station, where the soil is formed by chernozems, has brought the following results. On average the soil temperature drops bellow 0 °C in depth of 5 cm from 4th January to 7th February i.e. 35 days and in 10 cm from 10th January to 6th February i.e. 28 days. The absolute maximum of soil temperature during the observed period (12.8 °C) was reached 30th March 1973 in depth 5 and 100 cm and absolute minimum of soil temperature (-9.5 °C) was measured in 5 cm 2nd and 3rd February 1963. The data have been processed by application Surfer 8.0. By the aid of this s
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/2B06101" target="_blank" >2B06101: Optimalizace zemědělské a říční krajiny v ČR s důrazem na rozvoj biodiverzity.</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2006
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Contributions to Geophysics and Geodesy
ISSN
1335-2806
e-ISSN
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Svazek periodika
36
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
SK - Slovenská republika
Počet stran výsledku
13
Strana od-do
329-341
Kód UT WoS článku
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EID výsledku v databázi Scopus
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