Soil C, N and P dynamics along a 13 ka chronosequence of landslides under semi-natural temperate forest

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F19%3AA20024HM" target="_blank" >RIV/61988987:17310/19:A20024HM - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/19:10403136

Výsledek na webu

<a href="https://reader.elsevier.com/reader/sd/pii/S0277379118303676?token=89E7570DE6B4E32FE1C49F98F216A697251786BBFFB2991649A9ADB3B9D48BDF12AA12ABB365DF501091266837D7E182" target="_blank" >https://reader.elsevier.com/reader/sd/pii/S0277379118303676?token=89E7570DE6B4E32FE1C49F98F216A697251786BBFFB2991649A9ADB3B9D48BDF12AA12ABB365DF501091266837D7E182</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quascirev.2019.04.001" target="_blank" >10.1016/j.quascirev.2019.04.001</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Soil C, N and P dynamics along a 13 ka chronosequence of landslides under semi-natural temperate forest

Popis výsledku v původním jazyce

Soils represent a key component of the global carbon (C) cycle containing 2 to 3 times more C than the atmosphere. Understanding the dynamics of soil carbon storage is crucial for the prediction of its potential and future feedback to climate change. Traditionally, it has been accepted that millennia are required for soils to reach their C storage capacities. For the first time, we investigated long-term soil development on sedimentary substrate under semi-natural temperate forest, using a unique chronosequence of 26 landslides ranging in age from 4 to ~13,000 years. Both carbon and nitrogen (N) stocks in the 0e30 cm of mineral soil increased rapidly and reached levels resembling that of undisturbed sites already within 100 years of pedogenesis. The mineral soil C stock then did not change while the N stock decreased significantly in older landslides ( 900 years). Phosphorus (P) in <2mm soil showed a rapid increase in the first 100 years followed by a slow decrease. This decrease was significant also for total soil P (including rocks) and may be caused by leaching, erosion and wood harvest. In contrast, the O horizon C, N and P stocks increased linearly throughout the chronosequence. The C:N, N:P, C:P ratios increased along the chronosequence in mineral soil but not in O horizon. Further experiments are needed to explain the mechanisms behind the observed dynamics of C and N. The possible mechanisms include saturation of soil mineral surfaces, the decreasing availability of soil phosphorus or erosion.

Název v anglickém jazyce

Soil C, N and P dynamics along a 13 ka chronosequence of landslides under semi-natural temperate forest

Popis výsledku anglicky

Soils represent a key component of the global carbon (C) cycle containing 2 to 3 times more C than the atmosphere. Understanding the dynamics of soil carbon storage is crucial for the prediction of its potential and future feedback to climate change. Traditionally, it has been accepted that millennia are required for soils to reach their C storage capacities. For the first time, we investigated long-term soil development on sedimentary substrate under semi-natural temperate forest, using a unique chronosequence of 26 landslides ranging in age from 4 to ~13,000 years. Both carbon and nitrogen (N) stocks in the 0e30 cm of mineral soil increased rapidly and reached levels resembling that of undisturbed sites already within 100 years of pedogenesis. The mineral soil C stock then did not change while the N stock decreased significantly in older landslides ( 900 years). Phosphorus (P) in <2mm soil showed a rapid increase in the first 100 years followed by a slow decrease. This decrease was significant also for total soil P (including rocks) and may be caused by leaching, erosion and wood harvest. In contrast, the O horizon C, N and P stocks increased linearly throughout the chronosequence. The C:N, N:P, C:P ratios increased along the chronosequence in mineral soil but not in O horizon. Further experiments are needed to explain the mechanisms behind the observed dynamics of C and N. The possible mechanisms include saturation of soil mineral surfaces, the decreasing availability of soil phosphorus or erosion.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

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

2019

Kód důvěrnosti údajů

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

Název periodika

Quaternary Science Reviews

ISSN

0277-3791

e-ISSN

—

Svazek periodika

213

Číslo periodika v rámci svazku

1 June 2019

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

12

Strana od-do

18-29

Kód UT WoS článku

000474671600002

EID výsledku v databázi Scopus

2-s2.0-85064450267