Dynamika promrzání půdy

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F05%3A00087342" target="_blank" >RIV/62156489:43210/05:00087342 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00020699:_____/05:8P002893

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Dynamics of soil freezing

Popis výsledku v původním jazyce

The knowledge of the soil environment is significant from the climatological, technical and biological point of view. For plants, soil is an environment from which they get nutriments and water, soil supports them and creates conditions for wintering. Inour climatic conditions, a typical manifestation of the climate is the lowering of the soil temperatures during the winter season under the freezing point, i.e. the occurrence of the freezing of the soil. This phenomenon has not been studied very widely,and there are many more data to be found about the temperatures of soil. According to the soil temperature of 0°C, freezing is often determined, but this procedure is not the best. The scarcity of data on the freezing of soil is given also by the fact,that its measurement is difficult. Out of the agroclimatological stations of the Czech Hydrometeorological Institute, the freezing of soil is being measured by the cryopedometr. The evaluation of measurement for the period of 1961 to 2004

Název v anglickém jazyce

Dynamics of soil freezing

Popis výsledku anglicky

The knowledge of the soil environment is significant from the climatological, technical and biological point of view. For plants, soil is an environment from which they get nutriments and water, soil supports them and creates conditions for wintering. Inour climatic conditions, a typical manifestation of the climate is the lowering of the soil temperatures during the winter season under the freezing point, i.e. the occurrence of the freezing of the soil. This phenomenon has not been studied very widely,and there are many more data to be found about the temperatures of soil. According to the soil temperature of 0°C, freezing is often determined, but this procedure is not the best. The scarcity of data on the freezing of soil is given also by the fact,that its measurement is difficult. Out of the agroclimatological stations of the Czech Hydrometeorological Institute, the freezing of soil is being measured by the cryopedometr. The evaluation of measurement for the period of 1961 to 2004

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/QF3100" target="_blank" >QF3100: Posouzení nárůstu klimatického sucha v zemědělství a zmírňování jeho důsledků závlahami</a><br>

Návaznosti

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

Rok uplatnění

2005

Kód důvěrnosti údajů

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

Název periodika

Contributions to Geophysics and Geodesy

ISSN

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e-ISSN

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Svazek periodika

35

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

15

Strana od-do

229-243

Kód UT WoS článku

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EID výsledku v databázi Scopus

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