Site and temporal variation of soil respiration in European beech, Norway spruce, and Scots pine forests

By W. Borken, Yi-Jun Xu, Eric Davidson, F. Beese. 2002

208 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/c91c4a991e5a21157486a1de1fc20520a532eb06

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In Civil and Structural Engineering

In Global and Planetary Change

In Soil Science

Citations in the corpus

N fertilization affects on soil respiration, microbial biomass and root respiration in Larix gmelinii and Fraxinus mandshurica plantations in China (2010, unknown): “The seasonal dynamics of soil respiration Similar to the previous reports (Keith et al. 1997; Widén and Majdi 2001; Borken and Xu 2002; Kang et al. 2003), soil respiration rates in the present study showed obvious seasonal dynamics and increased exponentially with soil temperature (Fig.”
On the variability of respiration in terrestrial ecosystems: moving beyond Q10 (2006, background): “Borken et al. (2002) correlated the change in soil matric potential since the last respiration measurement with the residuals of a temperature model of soil respiration in three European forests.”
Annual Q10 of soil respiration reflects plant phenological patterns as well as temperature sensitivity (2004, background): “However, in the temperate maritime climate at our site, the Scots pines continue to photosynthesize (Carrara et al., 2003), whereas in the continental conditions of the Borken et al. (2002) study, this may not have been the case.”
Soil respiration and soil carbon balance in a northern hardwood forest ecosystem (2005, background): “Several other studies have reported that severe soil drought reduces FCO2 in temperate broadleaf forest ecosystems (Hanson et al. 1993; Epron et al. 1999; Borken et al. 2002), though the confounding effects of temperature and moisture are notoriously difficult to separate (Davidson et al.”