Soil Respiration in Larch Forests

  • T. Morishita
  • O. V. Masyagina
  • T. Koike
  • Y. Matsuura
Chapter
Part of the Ecological Studies book series (ECOLSTUD, volume 209)

Abstract

Soil respiration is an important component process of the carbon cycle (Schlesinger and Andrews 2000). It is derived from both soil microbial respiration and plant root respiration (Luo and Zhou 2006). In boreal forests, substrate supply, soil temperature, and soil moisture control the soil respiration (Luo and Zhou 2006). The litterfall on the soil surface was found to have a liner relationship with an increase in soil respiration (Bowden et al. 1993; Boone et al. 1998; Maier and Kress 2000; Sulzman et al. 2005). Soil respiration responds to aboveground herbivory (Ruess et al. 1998), carbon supply from aboveground photosynthesis to roots (Högberg et al. 2001), fine root density (Shibistova et al. 2002), and availability of nutrients (Nadelhoffer 2000; Burton et al. 2000). Soil temperature strongly affects the soil respiration (Chen and Tian 2005). The soil respiration is also affected by soil moisture as very high soil moisture can block soil pores (Bouma and Bryla 2000), and very low soil moisture limits microbial and root respiration (Yuste et al. 2003). However, the soil respiration is not related to soil moisture in relatively mesic environments (e.g., Palmroth et al. 2005).

Keywords

Biomass Burning Methane Fermentation Hydroxyl 

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Copyright information

© Springer Science+Business Media B.V. 2010

Authors and Affiliations

  • T. Morishita
    • 1
  • O. V. Masyagina
    • 2
  • T. Koike
    • 3
  • Y. Matsuura
    • 1
  1. 1.Department of Forest Site EnvironmentForestry and Forest Products Research InstituteTsukubaJapan
  2. 2.V.N. Sukachev Institute of Forest, Siberian Branch, Russian Academy of SciencesKrasnoyarskRussia
  3. 3.Department of Forest ScienceHokkaido UniversitySapporoJapan

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