Measuring of infiltration rate in different types of soil in the Czech Republic using a rainfall simulator

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00027049%3A_____%2F23%3AN0000070" target="_blank" >RIV/00027049:_____/23:N0000070 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60076658:12220/23:43907153 RIV/60460709:41330/23:95587 RIV/62156489:43210/23:43923575

Výsledek na webu

<a href="https://swr.agriculturejournals.cz/pdfs/swr/2023/02/06.pdf" target="_blank" >https://swr.agriculturejournals.cz/pdfs/swr/2023/02/06.pdf</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.17221/132/2022-SWR" target="_blank" >10.17221/132/2022-SWR</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Measuring of infiltration rate in different types of soil in the Czech Republic using a rainfall simulator

Popis výsledku v původním jazyce

Knowledge of the issue of water movement in the soil is the basis for agricultural activity, but also for many other sectors. One of the basic indicators that is evaluated in soil science is the rate of water infiltration into the soil. The article specifically states how soil texture and soil moisture affect the rate of water infiltration. The results show that changes in water infiltration can be significant and certain trends can be traced. The rate of water infiltration into the soil is most affected by the sand fraction (soil particles 0.05–2 mm). The higher the percentage of these soil particles in the soil, the lower the changes in infiltration rate depending on the degree of saturation. The article further evaluates soil moisture in relation to texture. The results were obtained at several research locations within the period 2014–2021 in the territory of the Czech Republic. The above findings are primarily applicable to the region of Central Europe or can be used as comparative values for regions in the rest of the world.

Název v anglickém jazyce

Measuring of infiltration rate in different types of soil in the Czech Republic using a rainfall simulator

Popis výsledku anglicky

Knowledge of the issue of water movement in the soil is the basis for agricultural activity, but also for many other sectors. One of the basic indicators that is evaluated in soil science is the rate of water infiltration into the soil. The article specifically states how soil texture and soil moisture affect the rate of water infiltration. The results show that changes in water infiltration can be significant and certain trends can be traced. The rate of water infiltration into the soil is most affected by the sand fraction (soil particles 0.05–2 mm). The higher the percentage of these soil particles in the soil, the lower the changes in infiltration rate depending on the degree of saturation. The article further evaluates soil moisture in relation to texture. The results were obtained at several research locations within the period 2014–2021 in the territory of the Czech Republic. The above findings are primarily applicable to the region of Central Europe or can be used as comparative values for regions in the rest of the world.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

40104 - Soil science

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

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

Název periodika

Soil and Water Research

ISSN

1801-5395

e-ISSN

1805-9384

Svazek periodika

18

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

10

Strana od-do

128-137

Kód UT WoS článku

000992431700001

EID výsledku v databázi Scopus

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