Soil organic carbon content decreases in both surface and subsoil mineral horizons by simulated future increases in labile carbon inputs in a temperate coniferous forest
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F21%3A00551571" target="_blank" >RIV/60077344:_____/21:00551571 - isvavai.cz</a>
Alternative codes found
RIV/61388971:_____/21:00551571 RIV/00216208:11310/21:10437183
Result on the web
<a href="https://link.springer.com/article/10.1007%2Fs10021-021-00632-w" target="_blank" >https://link.springer.com/article/10.1007%2Fs10021-021-00632-w</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10021-021-00632-w" target="_blank" >10.1007/s10021-021-00632-w</a>
Alternative languages
Result language
angličtina
Original language name
Soil organic carbon content decreases in both surface and subsoil mineral horizons by simulated future increases in labile carbon inputs in a temperate coniferous forest
Original language description
Soils represent important pools of soil organic carbon (SOC) that can be greatly influenced by labile C inputs, which are expected to increase in future due to CO2 enrichment of atmosphere and a concomitant rise in plant primary productivity. Studying effects of variable labile C inputs on SOC pool helps to understand how soils respond to global change. However, this knowledge is missing for coniferous forest soils despite being widespread throughout the northern temperate zone. We conducted a 7-month field manipulation experiment to study the effects of variable labile C inputs (simulated by additions of C-4 sucrose) on the C content in soil fractions and on microbial abundance in the organic (O), surface mineral (A), and subsoil mineral (B) horizons of a temperate coniferous forest soil. SOC in less-protected soil fractions and total organic C were substantially decreased by labile C additions that simulated future increases in C inputs. The SOC losses were comparable between the A and B horizon (40% vs. 30%). However, because sucrose availability estimated from its incorporation into soil fractions and microbial biomass sharply decreased with soil depth, the loss of C was higher in the B than in the A horizon when related to the amount of sucrose added. Utilization of sucrose was highest by fungi in the O horizon and by bacteria in the mineral soil horizons. The results indicate that future increases in labile C inputs to coniferous forest soils will cause rapid and substantial losses of SOC in both the surface and subsoil mineral horizons.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10511 - Environmental sciences (social aspects to be 5.7)
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Ecosystems
ISSN
1432-9840
e-ISSN
1435-0629
Volume of the periodical
24
Issue of the periodical within the volume
8
Country of publishing house
US - UNITED STATES
Number of pages
14
Pages from-to
2028-2041
UT code for WoS article
000637632700001
EID of the result in the Scopus database
2-s2.0-85103878634