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by Staff Writers
Munich, Germany (SPX) Jan 17, 2014
Global carbon dioxide (CO2) emissions continue to rise - in 2012 alone, 35.7 billion tons of this greenhouse gas entered the atmosphere*. Some of this CO2 is absorbed by the oceans, plants and soil.
As such, they provide a significant reservoir of carbon, stemming the release of CO2. Scientists have now discovered how organic carbon is stored in soil. Basically, the carbon only binds to certain soil structures. This means that soil's capacity to absorb CO2 needs to be re-assessed and incorporated into today's climate models.
Previous studies have established that carbon binds to tiny mineral particles. In this latest study, published in Nature Communications, researchers of the Technische Universitat Munchen (TUM) and the Helmholtz Zentrum Munchen have shown that the surface of the minerals plays just as important a role as their size.
"The carbon binds to minerals that are just a few thousandths of a millimeter in size - and it accumulates there almost exclusively on rough and angular surfaces," explains Prof. Ingrid Kogel-Knabner, TUM Chair of Soil Science.
The role of microorganisms in sequestering carbon
These carbon hot spots are, however, only found on around 20 percent of the mineral surfaces. It was previously assumed that carbon is evenly distributed in the soil. "Thanks to our study, we can now pin-point the soil that is especially good for sequestering CO2," continues Kogel-Knabner. "The next step is to include these findings in carbon cycle models."
Mass spectrometer helps to visualize molecules
Submicron structures provide preferential spots for carbon and nitrogen sequestration in soils, Cordula Vogel, Carsten W. Muller, Carmen Hoschen, Franz Buegger, Katja Heister, Stefanie Schulz, Michael Schloter and Ingrid Kogel-Knabner, Nature Communications, DOI: 10.1038/ncomms3947.
Technische Universitat Munchen
Carbon Worlds - where graphite, diamond, amorphous, fullerenes meet
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