The role of pit‑mound microrelief in the redistribution of rainwater in forest soils: a natural legacy facilitating groundwater recharge?

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F22%3APU143620" target="_blank" >RIV/00216305:26110/22:PU143620 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/62156489:43210/22:43921172 RIV/62156489:43410/22:43921172 RIV/62156489:43110/22:43921172 RIV/60460709:41330/22:91332

Výsledek na webu

<a href="https://link.springer.com/article/10.1007/s10342-022-01439-7" target="_blank" >https://link.springer.com/article/10.1007/s10342-022-01439-7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10342-022-01439-7" target="_blank" >10.1007/s10342-022-01439-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The role of pit‑mound microrelief in the redistribution of rainwater in forest soils: a natural legacy facilitating groundwater recharge?

Popis výsledku v původním jazyce

In commercial forest plantations dominated by Norway spruce (Picea abies L. Karst), the typically densely rooted forest floor and a poor understory contribute to the formation of surface or shallow hypodermic runoff, which limits the redistribution of infiltrated water to deeper soil layers. Pit-mound microrelief is a natural legacy in forest soils that originate from historical tree uprootings. This paper analyses the hydrological processes associated within the pit-mound microrelief based on the monitoring of soil electrical resistance (Rx). In two forested slopes, paired-tube profile probes were used to monitor the dynamics of Rx along four transects through pit-mound pairs at different soil depths. Cross-corelation analysis was used to detect the time-lag responses of deeper soil layers as compared to surface horizons within 15 pre-selected precipitation periods per site. Unlike other microsites, the Rx of deeper soil layers at pit microsites were mostly correlated to the Rx of surface horizons with a time lag of 0–6 h, demonstrating a fast redistribution of infiltrated water throughout the soil profile. Our results indicate that the pit-mound microrelief on forested slopes can positively contribute to the retention and redistribution of infiltrated water to the subsoil, not only through direct infiltration from the soil surface but also likely by the disruption and redirection of shallow lateral flow. Thereby, the pit-mound microrelief may facilitate groundwater recharge similarly as the technical measures that are currently used in arid and semiarid regions.

Název v anglickém jazyce

The role of pit‑mound microrelief in the redistribution of rainwater in forest soils: a natural legacy facilitating groundwater recharge?

Popis výsledku anglicky

In commercial forest plantations dominated by Norway spruce (Picea abies L. Karst), the typically densely rooted forest floor and a poor understory contribute to the formation of surface or shallow hypodermic runoff, which limits the redistribution of infiltrated water to deeper soil layers. Pit-mound microrelief is a natural legacy in forest soils that originate from historical tree uprootings. This paper analyses the hydrological processes associated within the pit-mound microrelief based on the monitoring of soil electrical resistance (Rx). In two forested slopes, paired-tube profile probes were used to monitor the dynamics of Rx along four transects through pit-mound pairs at different soil depths. Cross-corelation analysis was used to detect the time-lag responses of deeper soil layers as compared to surface horizons within 15 pre-selected precipitation periods per site. Unlike other microsites, the Rx of deeper soil layers at pit microsites were mostly correlated to the Rx of surface horizons with a time lag of 0–6 h, demonstrating a fast redistribution of infiltrated water throughout the soil profile. Our results indicate that the pit-mound microrelief on forested slopes can positively contribute to the retention and redistribution of infiltrated water to the subsoil, not only through direct infiltration from the soil surface but also likely by the disruption and redirection of shallow lateral flow. Thereby, the pit-mound microrelief may facilitate groundwater recharge similarly as the technical measures that are currently used in arid and semiarid regions.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10501 - Hydrology

Projekt

<a href="/cs/project/LF13019" target="_blank" >LF13019: Systém sledování vybraných parametrů porézních látek metodou EIS v širokém spektru aplikací</a><br>

Návaznosti

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

Rok uplatnění

2022

Kód důvěrnosti údajů

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

Název periodika

EUROPEAN JOURNAL OF FOREST RESEARCH

ISSN

1612-4669

e-ISSN

1612-4677

Svazek periodika

141

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

25

Strana od-do

1-25

Kód UT WoS článku

000756192000001

EID výsledku v databázi Scopus

2-s2.0-85124834154