Belowground carbon turnover in a temperate ombrotrophic bog-Reference-Cited by-同舟云学术

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Belowground carbon turnover in a temperate ombrotrophic bog

Published:2007-03 Issue:1 Volume:21 Page:
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Blodau Christian¹,Roulet Nigel T.²,Heitmann Tobias¹,Stewart Heather²,Beer Julia¹,Lafleur Peter³,Moore Tim R.²

Affiliation:

1. Limnological Research Station and Department of Hydrology; University of Bayreuth; Bayreuth Germany

2. Department of Geography and Global Environmental and Climate Change Centre; McGill University; Montreal, Quebec Canada

3. Department of Geography; Trent University; Peterborough Ontario Canada

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2005GB002659/fullpdf

Reference53 articles.

1. Interpretation of measured concentration profiles in sediment pore water;Berg;Limnol. Oceanogr.,1998

2. Microbial carbon mineralisation in an acid surface peat: Effects of environmental factors in laboratory incubations;Bergman;Soil Biol. Biochem.,1999

3. Macroporosity affects water movement and pore water sampling in peat soils;Blodau;Soil Sci.,2002

4. Micro-scale CO2 and CH4 dynamics in a peat soil during a water fluctuation and sulfate pulse;Blodau;Soil Biol. Biochem.,2003

5. Iron, sulfur and dissolved carbon dynamics in a northern peatland;Blodau;Arch. Hydrobiol.,2002

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