Soil Processes and the Carbon Cycle 2018
DOI: 10.1201/9780203739273-23
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Investigations of Carbon and Nitrogen Dynamics In Different Long-Term Experiments by Means of Biological Soil Properties

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Cited by 4 publications
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“…15%) shows the importance of the fine soil particles for the increased C stabilization, as emphasized by Hassink (1997), Weigel et al (1997) and Albert and Lippold (2002). Our finding is also in line with the conceptional model proposed by von Lützow et al (2007), which considers organo-mineral associations as an important pool for C stabilization and also with the Rothamsted Carbon Model, which calculates a decreasing fraction of CO 2 produced to C sequestered in the pools microbial biomass and humified organic matter with increasing clay contents (Coleman and Jenkinson, 1999).…”
Section: Soil Organic Matter and Total Nitrogenmentioning
confidence: 80%
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“…15%) shows the importance of the fine soil particles for the increased C stabilization, as emphasized by Hassink (1997), Weigel et al (1997) and Albert and Lippold (2002). Our finding is also in line with the conceptional model proposed by von Lützow et al (2007), which considers organo-mineral associations as an important pool for C stabilization and also with the Rothamsted Carbon Model, which calculates a decreasing fraction of CO 2 produced to C sequestered in the pools microbial biomass and humified organic matter with increasing clay contents (Coleman and Jenkinson, 1999).…”
Section: Soil Organic Matter and Total Nitrogenmentioning
confidence: 80%
“…Only some selected improvements of soil quality induced by OM increase will be mentioned. OM can provide organic substances like vitamins and auxins to stimulate plant growth and microbial activity (Weigel et al, 1997;Brady and Weil, 1997). An increase in soil C stocks results in a higher storage of nutrients as well as higher water holding capacity and pH buffering capacity.…”
Section: Sequestration In Agricultural Soilsmentioning
confidence: 99%
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