All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Dynamics of soil freezing

The result's identifiers

  • Result code in 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>

  • Alternative codes found

    RIV/00020699:_____/05:8P002893

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Dynamics of soil freezing

  • Original language description

    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

  • Czech name

    Dynamika promrzání půdy

  • Czech description

    Půda je prostředím, ze kterého rostliny čerpají živiny a vodu, vytváří podmínky pro jejich přezimování. V našich klimatických podmínkách nastává v zimním období pokles teploty půdy až pod bod mrazu a půda promrzá.Pormrzání půdy je měřeno kryopedometry nastanicích ČHMÚ, měření byla vyhodnocena pro období 1961-2004 a stanici Pohořelice.

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DG - Atmospheric sciences, meteorology

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/QF3100" target="_blank" >QF3100: Appreciation of Climatic Drought Rising in Agriculture and Mitigation of its Consequences with Irrigation</a><br>

  • Continuities

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

Others

  • Publication year

    2005

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Contributions to Geophysics and Geodesy

  • ISSN

  • e-ISSN

  • Volume of the periodical

    35

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    SK - SLOVAKIA

  • Number of pages

    15

  • Pages from-to

    229-243

  • UT code for WoS article

  • EID of the result in the Scopus database