Soil respiration in temperate forests is increased by a shift from coniferous to deciduous trees but not by an increase in temperature
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F20%3A00531449" target="_blank" >RIV/60077344:_____/20:00531449 - isvavai.cz</a>
Result on the web
<a href="https://www.sciencedirect.com/science/article/abs/pii/S0929139320303383?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/abs/pii/S0929139320303383?via%3Dihub</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.apsoil.2020.103635" target="_blank" >10.1016/j.apsoil.2020.103635</a>
Alternative languages
Result language
angličtina
Original language name
Soil respiration in temperate forests is increased by a shift from coniferous to deciduous trees but not by an increase in temperature
Original language description
The rate of litter and soil organic matter decomposition depends on temperature and on leaf carbon content and its availability to decomposers. The effects of these variables on decomposition in temperate forest soils are incompletely understood although future increases are predicted for temperature, the ratio of litter fractions, and the ratio of deciduous to coniferous forests. In this study, a 14-month laboratory incubation experiment of adding deciduous (beech) and coniferous (spruce) litter to soil (Cambisol) was carried out to test the effects of litter fraction, tree species, and temperature on soil respiration (as indicated by CO2 release). The addition of the soluble and insoluble litter fractions as well as the whole tissue caused an increase in soil respiration (relative to the no-addition treatment). The effect of the soluble fraction, however, was less persistent than the effects of whole tissue or insoluble fractions, which suggests generally greater long-term effects of the latter fractions on soil respiration. Fractions derived from the beech litter increased soil respiration more than those derived from the spruce litter. This trend was especially apparent with the soluble litter fraction. A temperature increase of 3 °C caused no difference in soil respiration after the addition of beech litter fractions and even reduced soil respiration after the addition of spruce litter fractions. These results suggest that a future increase in the soluble fraction coupled with a shift in tree species composition from coniferous to deciduous might lead to an increase in soil respiration and thus to an increase in CO2 release from the forest floor. The results, however, also suggest that a 3 °C increase in temperature will not lead to increases in CO2 release from the forest floor, even if deciduous trees become more abundant.
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
10618 - Ecology
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Applied Soil Ecology
ISSN
0929-1393
e-ISSN
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Volume of the periodical
154
Issue of the periodical within the volume
October
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
5
Pages from-to
103635
UT code for WoS article
000539994500024
EID of the result in the Scopus database
2-s2.0-85085100560