Variability of topsoil hydraulic conductivity along the hillslope transects delineated in four areas strongly affected by soil erosion

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41210%2F21%3A85407" target="_blank" >RIV/60460709:41210/21:85407 - isvavai.cz</a>

Výsledek na webu

<a href="https://sciendo.com/de/article/10.2478/johh-2021-0008" target="_blank" >https://sciendo.com/de/article/10.2478/johh-2021-0008</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2478/johh-2021-0008" target="_blank" >10.2478/johh-2021-0008</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Variability of topsoil hydraulic conductivity along the hillslope transects delineated in four areas strongly affected by soil erosion

Popis výsledku v původním jazyce

Soil hydraulic conductivities of topsoils were studied at 5 points of the hillslope transects delineated at 4 geomorphologically diverse areas, where the original soil types Chernozem, Luvisol and two Cambisols were due to erosion transformed into different soil unites. Hydraulic conductivities of saturated soils and for a pressure head of 2 cm were measured directly in the field using a Guelph permeameter and mini disk tension infiltrometer, and in the laboratory using a multistep outflow method. While Ks,GP Ks,MSO in the Chernozem and Cambisol regions, and Ks,GP Ks,MSO in the Luvisol and Cambisol loam regions. The Ks values obtained using different methods showed different trends along the hillslope transects.

Název v anglickém jazyce

Variability of topsoil hydraulic conductivity along the hillslope transects delineated in four areas strongly affected by soil erosion

Popis výsledku anglicky

Soil hydraulic conductivities of topsoils were studied at 5 points of the hillslope transects delineated at 4 geomorphologically diverse areas, where the original soil types Chernozem, Luvisol and two Cambisols were due to erosion transformed into different soil unites. Hydraulic conductivities of saturated soils and for a pressure head of 2 cm were measured directly in the field using a Guelph permeameter and mini disk tension infiltrometer, and in the laboratory using a multistep outflow method. While Ks,GP Ks,MSO in the Chernozem and Cambisol regions, and Ks,GP Ks,MSO in the Luvisol and Cambisol loam regions. The Ks values obtained using different methods showed different trends along the hillslope transects.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

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)

Rok uplatnění

2021

Kód důvěrnosti údajů

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

Název periodika

Journal of Hydrology and Hydromechanics

ISSN

0042-790X

e-ISSN

1338-4333

Svazek periodika

69

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

12

Strana od-do

220-231

Kód UT WoS článku

000655253300009

EID výsledku v databázi Scopus

2-s2.0-85106977938