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

By Nina Buchmann. 2000

573 citations recorded by the source corpus.

Subfields: Civil and Structural Engineering, Global and Planetary Change, Soil Science

View Paper: https://www.semanticscholar.org/paper/452de39f840e2ce96936da037f75530d888d0dcd

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In Civil and Structural Engineering

In Global and Planetary Change

In Soil Science

Citations in the corpus

Root trenching: a useful tool to estimate autotrophic soil respiration? A case study in an Austrian mountain forest (2008, background): “In contrast to soil moisture, root parameters and soil microbial community structure have not been regularly assessed (Bowden et al. 1993; Buchmann 2000; Epron et al. 1999b; Lee et al. 2003; Rey et al. 2002; Sulzman et al. 2005).”
REVIEW: Time lag between photosynthesis and carbon dioxide efflux from soil: a review of mechanisms and controls (2010, background): “For tree stands, the common interruption is trenching (Buchmann, 2000; Ross et al., 2001; Lee et al., 2003) or girdling (Högberg et al., 2001; Bhupinderpal-Singh et al., 2003; Olsson et al., 2005).”
Comparison of the eddy covariance and automated closed chamber methods for evaluating nocturnal CO2 exchange in a Japanese cypress forest (2007, background): “However, these studies have the following problems related to obtaining the average Fs, Ft, and Ffateachsite:soilrespirationrateshowshighspatialand temporal variation (e.g., Hanson et al., 1993; Davidson etal.,1998; Buchmann,2000; RaymentandJarvis,2000; Stoyan et al., 2000; Law et al., 2001; Xu and ”
A global relationship between the heterotrophic and autotrophic components of soil respiration? (2004, background): “Högberg P, Nordgren A, Buchmann N et al. (2001) Large-scale”
Soil CO 2 efflux from a podzolic forest soil before and after forest clear-cutting and site preparation (2004, methodology): “Simultaneously with the increased decomposition of litter material, the amount of root and rhizosphere respiration decreases (Bowden et al. 1993, Nakane et al. 1996, Boone et al. 1998, Buchmann 2000).”
Spatial variability and optimal sampling strategy of soil respiration (2008, background): “The CVof soil CO2 efflux has been reported to largely vary between 10 and 150% in forest, grassland and cropland ecosystems (Hanson et al., 1993; Cambardella et al., 1994; Fang et al., 1998; Buchmann, 2000; Stoyan et al., 2000; Law et al., 2001; Xu and Qi, 2001; Davidson et al., 2002; Yim et al., 20”
Does the temperature sensitivity of decomposition of soil organic matter depend upon water content, soil horizon, or incubation time? (2005, background): “While Buchmann (2000) concluded from direct measurements following the removal of organic horizons that the majority of respired CO2 originates from the mineral layer, Subke et al. (2003) argued that the correlation between temperature and surface efflux suggest that the organic layer has the…”
Below‐ground carbon flux and partitioning: global patterns and response to temperature (2008, unknown): “, NM 391 4·0 773 (Gower, Vogt & Grier 1992) Picea abies; 47 years¶ Bavaria, Germany 470 5·6 768 (Buchmann 2000) Pseudotsuga menziesii; 50 years¶ Kettle River Range, WA 700 5·7 660 (McDowell et al.”
Annual Q10 of soil respiration reflects plant phenological patterns as well as temperature sensitivity (2004, methodology): “…Blackwell Publishing Ltd 161 used to estimate SR rates from temperature (Schlentner & van Cleve, 1985; Cropper & Gholz, 1991; Hanson et al., 1993; Peterjohn et al., 1994; Raich & Potter, 1995; Boone et al., 1998; Davidson et al., 1998; Epron et al., 1999; Buchmann, 2000; Morén & Lindroth, 2000).”