EGU General Assembly 2008
Session Programme Meeting Programme Personal Programme Search
 
Quick Search
Programme Groups
Union Symposia
Interdivision Sessions
Educational Symposia
Atmospheric Sciences
Biogeosciences
Climate: Past, Present, Future
Cryospheric Sciences
Earth & Space Science Informatics
Energy, Resources & the Environment
Geochemistry, Mineralogy, Petrology & Volcanology
Geodesy
Geodynamics
Geomorphology
Geosciences Instrumentation & Data Systems
Hydrological Sciences
Isotopes in Geosciences: Instrumentation and Applications
Magnetism, Palaeomagnetism, Rock Physics & Geomaterials
Natural Hazards
Nonlinear Processes in Geophysics
Ocean Sciences
Planetary & Solar System Sciences
Seismology
Soil System Sciences
Solar-Terrestrial Sciences
Stratigraphy, Sedimentology & Palaeontology
Tectonics & Structural Geology
Medal Lectures
Great Debates in Geosciences
Short Courses
Keynote Lectures
Townhall Meetings
Division Business Meetings
Editorial Board Meetings
Union Meetings
Splinter Meetings
  Information - SSS8 Organic soils and Carbon Sink: characterization, relevance, analysis

Event Information
Peatlands represent some of the most important carbon stores in the world. They contain nearly 30 percent of all carbon on the land, while only covering 3 percent of the area. As one of the largest carbon stories of the world, peat plays a significant function in the regulation of greenhouse gas emissions and global climate. Peat bogs are very important as carbon sinks. Peatlands in several regions revealed actively sequestering carbon. Peat organic matter regulates long-term C storage and nutrient availability to plants and microbes. Peatlands are a source of peat for horticulture, pomology, and floriculture and are also used for forestry and agriculture. Unfortunately, despite these benefits, peatlands around the world have been heavily utilized or degraded. Agricultural use of peatlands and their exploitation lead to the release of carbon. Long-term cultivation and agricultural use of peatlands has led to a number of effects including lowering of the water table, increased aeration, and changes in plant communities. The decline in peat soil moisture content resulting from drainage leads to shrinkage of the peat. Volume change due to shrinkage is the result of several forces acting at micro-scale, and its mechanism and magnitude differ from those in mineral (clay) soils. Drainage in particular results in a sharp change of biotic and abiotic properties and consequent degradation of peat organic matter. In general, this leads to the progressive differentiation of the hydrophobic and total amino acid contents. The sequential changes in physical and hydraulic properties initiated by drainage for agriculture have an important influence on chemical properties and, in turn, on the net fluxes of CH4, CO2 and N2O from agricultural peat soils. Aeration of the upper peat layers resulting from drainage and agricultural land use triggers the aerobic decomposition process that causes carbon dioxide emissions from the soil. Thus peat soils and land use play an important role in the global budgets of these gases.

Preliminary List of Solicited Speakers

Co-Sponsorship

General Statement
The information contained hereafter has been compiled and uploaded by the Session Organizers via the "Organizer Session Form". The Session Organizers have therefore the sole responsibility that this information is true and accurate at the date of publication, and the conference organizer cannot accept any legal responsibility for any errors or omissions that may be made, and he makes no warranty, expressed or implied, with regard to the material published.



Back to Session Programme

 
 
 
 


©2002-2008 Copernicus Systems + Technology GmbH