Modeling Heat Fluxes in Macroporous Soil under Sparse Young Forest of Temperate Humid Climate

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F11%3A00179889" target="_blank" >RIV/68407700:21110/11:00179889 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.jhydrol.2011.03.030" target="_blank" >http://dx.doi.org/10.1016/j.jhydrol.2011.03.030</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.jhydrol.2011.03.030" target="_blank" >10.1016/j.jhydrol.2011.03.030</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Modeling Heat Fluxes in Macroporous Soil under Sparse Young Forest of Temperate Humid Climate

Popis výsledku v původním jazyce

This research is focused on improved quantitative understanding of processes controlling the movement of water and heat below the land surface under natural vegetation. Special attention is paid to the advective transport of soil heat during rainfall events and the role of preferential flow in the soil heat transfer system. Transient flow of water and transport of heat were simulated using dual-continuum model with semi-separate flow domains representing the soil matrix and the network of preferential pathways. The model was able to reproduce quite well the measured variations of soil temperatures, and, at least in principle, also the measured temperatures of shallow subsurface discharge, closely associated with the preferential flow.

Název v anglickém jazyce

Modeling Heat Fluxes in Macroporous Soil under Sparse Young Forest of Temperate Humid Climate

Popis výsledku anglicky

This research is focused on improved quantitative understanding of processes controlling the movement of water and heat below the land surface under natural vegetation. Special attention is paid to the advective transport of soil heat during rainfall events and the role of preferential flow in the soil heat transfer system. Transient flow of water and transport of heat were simulated using dual-continuum model with semi-separate flow domains representing the soil matrix and the network of preferential pathways. The model was able to reproduce quite well the measured variations of soil temperatures, and, at least in principle, also the measured temperatures of shallow subsurface discharge, closely associated with the preferential flow.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F08%2F1174" target="_blank" >GA205/08/1174: Hydrologické toky v systému půda-rostlina-atmosféra</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Journal of Hydrology

ISSN

0022-1694

e-ISSN

—

Svazek periodika

402

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

10

Strana od-do

367-376

Kód UT WoS článku

000291192900018

EID výsledku v databázi Scopus

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