Organic matter decomposition and carbon content in soil fractions as affected by a gradient of labile carbon input to a temperate forest soil
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F20%3A43901160" target="_blank" >RIV/60076658:12310/20:43901160 - isvavai.cz</a>
Alternative codes found
RIV/60077344:_____/20:00531022 RIV/61388971:_____/20:00531022 RIV/00216208:11310/20:10414081
Result on the web
<a href="https://link.springer.com/article/10.1007/s00374-020-01433-4" target="_blank" >https://link.springer.com/article/10.1007/s00374-020-01433-4</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00374-020-01433-4" target="_blank" >10.1007/s00374-020-01433-4</a>
Alternative languages
Result language
angličtina
Original language name
Organic matter decomposition and carbon content in soil fractions as affected by a gradient of labile carbon input to a temperate forest soil
Original language description
Labile carbon (C) input to soils is expected to affect soil organic matter (SOM) decomposition and soil organic C (SOC) stocks in temperate coniferous forests. We hypothesized that the SOM decomposition rate, C content in soil fractions, and microbial and faunal abundance and activity were increased along the gradient in labile C input around wood ant nests. Three distances from the nest that differed in annual labile C input to soil were selected: 4 m with 6379 mg C m(-2), 30 m with 9060 mg C m(-2), and 70 m with 9215 mg C m(-2). Soil from the organic horizon (Oe+Oa), surface mineral horizon (A), and subsoil mineral horizon (B) was analyzed for C content in soil fractions and for activity and abundance of soil microorganisms and fauna. In addition, a 1-year litter-bag and soil-bag decomposition experiment was conducted. Although the rate of soil decomposition did not differ along the labile C input gradient, the rate of litter decomposition in the B horizon increased as labile C input increased with distance from the nest. Correspondingly, the C content in bulk soil and in the labile and less-protected soil fractions in the B horizon decreased as labile C input increased. We infer that, because the O and A horizons are less C-limited than the B horizon, the changes in the labile C input along the gradient affected the B horizon more than the surface O and A horizons. However, soil microbial and faunal activity and abundances were not consistently affected by the gradient. Apparently, C stocks in soil fractions are more important for microbial and faunal communities than labile C inputs. Although the results indicate that SOC content changes very slowly in the coniferous forest soil of the current study, increases in the input of natural labile C leads to decreases in the SOC stock in the B horizon. By increasing the labile C input to temperate forest soils, future increases in atmospheric CO2 concentration may therefore lead to a significant loss of SOC in deep soil layers.
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
40104 - Soil science
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
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Biology and Fertility of Soils
ISSN
0178-2762
e-ISSN
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Volume of the periodical
56
Issue of the periodical within the volume
3
Country of publishing house
US - UNITED STATES
Number of pages
11
Pages from-to
411-421
UT code for WoS article
000518728100010
EID of the result in the Scopus database
2-s2.0-85078239722