Belowground carbon turnover in a temperate ombrotrophic bog
- 20 March 2007
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 21 (1)
- https://doi.org/10.1029/2005gb002659
Abstract
No abstract availableKeywords
This publication has 49 references indexed in Scilit:
- CH4 sources estimated from atmospheric observations of CH4 and its 13C/12C isotopic ratios: 1. Inverse modeling of source processesGlobal Biogeochemical Cycles, 2004
- Atmospheric sulfur deposition alters pathways of gaseous carbon production in peatlandsGlobal Biogeochemical Cycles, 2003
- Seasonal contribution of CO2fluxes in the annual C budget of a northern bogGlobal Biogeochemical Cycles, 2003
- Modeling seasonal to annual carbon balance of Mer Bleue Bog, Ontario, CanadaGlobal Biogeochemical Cycles, 2002
- Annual cycle of CO2 exchange at a bog peatlandJournal of Geophysical Research: Atmospheres, 2001
- Seasonal patterns and controls on net ecosystem CO2 exchange in a boreal peatland complexGlobal Biogeochemical Cycles, 1998
- Carbon balance of a temperate poor fenGlobal Biogeochemical Cycles, 1997
- Groundwater flow and dissolved carbon movement in a boreal peatlandJournal of Hydrology, 1997
- Cross-correlation analysis of the dynamics of methane emissions from a boreal peatlandGlobal Biogeochemical Cycles, 1996
- The influence of temperature and water table position on carbon dioxide and methane emissions from laboratory columns of peatland soilsEuropean Journal of Soil Science, 1993