Details
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 151-159 |
| Seitenumfang | 9 |
| Fachzeitschrift | Russian journal of ecology |
| Jahrgang | 39 |
| Ausgabenummer | 3 |
| Publikationsstatus | Veröffentlicht - 11 Mai 2008 |
| Extern publiziert | Ja |
Abstract
Fluxes of dissolved organic matter (DOM) in larch biogeocenoses and its export from the drainage basin have been studied in the zone of continuous permafrost. A comparative assessment of DOM input into the soil has been made on slopes of northern and southern exposures (as variants reflecting the current state and warming). The dynamics of DOM export in a creek depending on the increasing depth of the active soil horizon in the drainage area have been revealed. It is concluded that an increase in the depth of the seasonally thawing layer induced by global warming will not have any significant effect on the amount of annual DOM export. Reduction of DOM export may be expected upon a decrease in litter stocks under the effect of their mineralization and forest fires.
ASJC Scopus Sachgebiete
- Agrar- und Biowissenschaften (insg.)
- Ökologie, Evolution, Verhaltenswissenschaften und Systematik
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in: Russian journal of ecology, Jahrgang 39, Nr. 3, 11.05.2008, S. 151-159.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - Fluxes of Dissolved Organic Matter in Larch Forests in the Cryolithozone of Central Siberia
AU - Prokushkin, A. S.
AU - Tokareva, I. V.
AU - Prokushkin, S. G.
AU - Abaimov, A. P.
AU - Guggenberger, H.
N1 - Funding information: ACKNOWLEDGMENTS This study was supported by the Fundamental Research Project of the Siberian Branch of the Russian Academy of Sciences (no. 22.1.4), the Russian Foundation for Basic Research (project nos. 03-04-48037 and 05-05-64208), and the European Science Foundation RSTCB Programme Exchange grant 667.
PY - 2008/5/11
Y1 - 2008/5/11
N2 - Fluxes of dissolved organic matter (DOM) in larch biogeocenoses and its export from the drainage basin have been studied in the zone of continuous permafrost. A comparative assessment of DOM input into the soil has been made on slopes of northern and southern exposures (as variants reflecting the current state and warming). The dynamics of DOM export in a creek depending on the increasing depth of the active soil horizon in the drainage area have been revealed. It is concluded that an increase in the depth of the seasonally thawing layer induced by global warming will not have any significant effect on the amount of annual DOM export. Reduction of DOM export may be expected upon a decrease in litter stocks under the effect of their mineralization and forest fires.
AB - Fluxes of dissolved organic matter (DOM) in larch biogeocenoses and its export from the drainage basin have been studied in the zone of continuous permafrost. A comparative assessment of DOM input into the soil has been made on slopes of northern and southern exposures (as variants reflecting the current state and warming). The dynamics of DOM export in a creek depending on the increasing depth of the active soil horizon in the drainage area have been revealed. It is concluded that an increase in the depth of the seasonally thawing layer induced by global warming will not have any significant effect on the amount of annual DOM export. Reduction of DOM export may be expected upon a decrease in litter stocks under the effect of their mineralization and forest fires.
KW - Creek
KW - Dissolved organic matter
KW - Drainage basin
KW - Export
KW - Larch biogeocenoses
KW - Permafrost
UR - http://www.scopus.com/inward/record.url?scp=43549104919&partnerID=8YFLogxK
U2 - 10.1134/S1067413608030016
DO - 10.1134/S1067413608030016
M3 - Article
AN - SCOPUS:43549104919
VL - 39
SP - 151
EP - 159
JO - Russian journal of ecology
JF - Russian journal of ecology
SN - 1067-4136
IS - 3
ER -