A global relationship between the heterotrophic and autotrophic components of soil respiration?

By B. Bond‐Lamberty, Chuankuan Wang, S. T. Gower. 2004

623 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/1b7fa6b8020b191943968cda43315a377d3f2544

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Civil and Structural Engineering

1. E. Baggs

In Global and Planetary Change

1. P. Högberg
2. M. Bahn
3. D. Metcalfe
4. E. Baggs

In Soil Science

1. E. Baggs
2. P. Högberg
3. Jingxin Wang
4. Shirong Liu

Citations in the corpus

• Bridging the gap between micro - and macro-scale perspectives on the role of microbial communities in global change ecology (2006, neutral): “Autotrophic respiration can comprise up to 60% of the total respiration, while the more dominant heterotrophic component can comprise between 50 and 100% of total soil respiration ( Bond-Lamberty et al. 2004a, b). The Q10 model (which states that as temperature increases, soil respiration increases”
• Root respiration in temperate mountain grasslands differing in land use (2006, background): “…CO2 efflux have so far rarely been investigated (Davidson et al., 2000), and virtually nothing is known on how they influence components of grassland soil respiration, which so far have been mainly explored for forest ecosystems (cf. reviews by Hanson et al., 2000 and Bond-Lamberty et al., 2004).”
• Global annual soil respiration in relation to climate, soil properties and vegetation characteristics: Summary of available data (2014, neutral): “Similar to Bond-Lamberty et al. (2004), we also nd soil/vegetation characteristics. r2 P RMSE ME MAE AIC r2×n 6pH − 1.276 0.540 <0.001 0.348 0.537 0.269 −1082.5 9.956 0.521 <0.001 0.354 0.521 0.266 −1096.4 6 0.459 <0.001 0.342 0.459 0.267 −1503.6 2.828 0.455 <0.001 0.344 0.455 0.267 −1507.3 0.488…”
• Rhizospheric and heterotrophic respiration of a warm-temperate oak chronosequence in China (2011, background): “Our estimated seasonal fluxes of RS, RH and RR, as well as the RC values for the four forests were within the range of reported values for temperate forests (Hanson et al., 2000; Bond-Lamberty et al., 2004a; Subke et al., 2006).”
• Contrasting effects of low and high nitrogen additions on soil CO2 flux components and ectomycorrhizal fungal sporocarp production in a boreal forest (2012, background): “Aboveground vegetation was removed by hand from the C2 and C4 collars 10 months prior to the first measurements to minimize the effect of transient CO2 flush from dead roots (Bowden et al., 1993; Haynes & Gower, 1995; Bond-Lamberty et al., 2004a).”
• Partitioning the components of soil respiration: a research challenge (2006, methodology): “Bond-Lamberty et al. (2004) in part attribute this large variability to technical and theoretical problems associated with the different methods adopted for partitioning the respiration components, although it is”