Abstract
The soil contains more carbon than the vegetation and the atmosphere put together. How we manage our soils will therefore be of crucial significance for the climate in the future. The flow of carbon between earth and atmosphere is a priority research area; at the Abisko field station in northern Sweden, measurements are taken to determine what happens as the permafrost melts. Another major challenge we are facing is that of limited phosphorus resources. Currently, phosphorus is released via waste water, polluting lakes and seas, while the phosphorus in mines is running out. Maybe we can bind phosphorus from urine to charcoal, to make soils in the third world more fertile while reducing the proportion of carbon dioxide in the atmosphere. That is what the native populations in Amazonia did before the Europeans arrived and spread their diseases.
For someone who loves nature, who
appreciates plants and animals and who finds
happiness in horticulture, no problem is insoluble.
Henning E. Segerros
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Further Readings
Belshe EF et al (2013) Tundra ecosystems observed to be CO2 sources due to differential amplification of the carbon cycle. Ecol Lett 10:1307–1315
Cordell D et al (2009) The story of phosphorus: global food security and food for thought. Glob Environ Change-Hum Policy Dimensions 19:292–305
Gunwick NP et al (2013) A systematic review of biochar research, with a focus on its stability in situ, and its promise as a climate mitigation strategy. PLoS One 8:e75932
Novotny EH et al (2006) The “Terra Preta” phenomenon: a model for sustainable agriculture in the humid tropics. Naturwissenschaften 88:37–41
Olefeldt D et al (2012) Net carbon accumulation of a high-latitude permafrost palsa mire similar to permafrost-free peatlands. Geophys Res Lett 39:L03501
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Wallander, H. (2014). Soil and Climate. In: Soil. Springer, Cham. https://doi.org/10.1007/978-3-319-08458-9_8
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DOI: https://doi.org/10.1007/978-3-319-08458-9_8
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