Biotic and abiotic factors controlling soil respiration rates in Picea abies stands

Authors
Citation
N. Buchmann, Biotic and abiotic factors controlling soil respiration rates in Picea abies stands, SOIL BIOL B, 32(11-12), 2000, pp. 1625-1635
Citations number
51
Categorie Soggetti
Environment/Ecology
Journal title
SOIL BIOLOGY & BIOCHEMISTRY
ISSN journal
00380717 → ACNP
Volume
32
Issue
11-12
Year of publication
2000
Pages
1625 - 1635
Database
ISI
SICI code
0038-0717(200010)32:11-12<1625:BAAFCS>2.0.ZU;2-O
Abstract
The response of soil respiration to varying environmental factors was studi ed in four Picea abies stands (47-, 87-, 111- and 146-year old) during the 1998 growing season. While within-site Variations of soil CO2 efflux (up to 1.6 mu mol CO2 m(-2) s(-1)) were larger than their diurnal variability (<0 .25 mu mol CO2 m(-2) s(-1)), spatial variations within a site were smaller than seasonal changes in soil respiration rates (up to 4.4 mu mol CO2 m(-2) s(-1)). Highest within-site variability of soil efflux was generally found during the summer months when maximum flux rates of 4-6 mu mol CO2 m(-2) s (-1) were reached (coefficient of variation 40%). Soil temperatures (in the O-f and O-h layers, and A(h) horizon) showed a pronounced seasonal course, in contrast to soil moisture. An exponential equation best described the r elationships between soil temperature in the Of layer and soil CO2 efflux ( r(2) between 0.75 and 0.81). However, an Arrhenius type equation always res ulted in lower r(2) values (0.52-0.71). The Q(10) values ranged between 2.3 9 (146-year old stand) and 3.22 (87-year old stand), averaging 2.72 for the P. abies stands within the watershed. The removal of litter and organic la yers generally affected soil CO2 efflux negatively. In three of the four P. abies stands (47-, 87-, 146-year old stands), soil respiration rates were reduced by 10-20% after removal of the L and O-f layer, and by 30-40% after removal of the L and most of the O-f and O-h layers. Thus, mineral soil re spiration seemed to contribute a major fraction to the total soil CO2 flux (> 60%). Trenching shallow fine roots during collar insertion and mechanica l inhibition of root in-growth during the following months allowed fine roo t respiration to be separated from microbial respiration only in times of h ighest root growth. Microbial respiration seemed to dominate the respirator y CO2 loss from the forest floor (>70%). The comparison of the annual soil CO2 efflux in the 47-year old P. abies stand (about 710 g C m(-2) yr(-1)) w ith annual litterfall and root net primary productivity estimates supported this conclusion. (C) 2000 Elsevier Science Ltd. All rights reserved.