the soil n cycle: new insights and key challenges
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2015
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The study of soil N cycling processes has been, is, and will be at the centre
of attention in soil science research. The importance of N as a nutrient for
all biota; the ever-increasing rates of its anthropogenic input in
terrestrial (agro)ecosystems; its resultant losses to the environment; and
the complexity of the biological, physical, and chemical factors that
regulate N cycling processes all contribute to the necessity of further
understanding, measuring, and altering the soil N cycle. Here, we review
important insights with respect to the soil N cycle that have been made over
the last decade, and present a personal view on the key challenges of future
research. We identify three key challenges with respect to basic N cycling
processes producing gaseous emissions:
1. quantifying the importance of nitrifier denitrification and its main controlling factors;
2. characterizing the greenhouse gas mitigation potential and microbiological basis for N2O consumption;
3. characterizing hotspots and hot moments of denitrification
Furthermore, we identified a key challenge with respect to modelling:
1. disentangling gross N transformation rates using advanced 15N / 18O tracing models
Finally, we propose four key challenges related to how ecological interactions control N cycling processes:
1. linking functional diversity of soil fauna to N cycling processes beyond mineralization;
2. determining the functional relationship between root traits and soil N cycling;
3. characterizing the control that different types of mycorrhizal symbioses exert on N cycling;
4. quantifying the contribution of non-symbiotic pathways to total N fixation fluxes in natural systems
We postulate that addressing these challenges will constitute a comprehensive research agenda with respect to the N cycle for the next decade. Such an agenda would help us to meet future challenges on food and energy security, biodiversity conservation, water and air quality, and climate stability.
1. quantifying the importance of nitrifier denitrification and its main controlling factors;
2. characterizing the greenhouse gas mitigation potential and microbiological basis for N2O consumption;
3. characterizing hotspots and hot moments of denitrification
Furthermore, we identified a key challenge with respect to modelling:
1. disentangling gross N transformation rates using advanced 15N / 18O tracing models
Finally, we propose four key challenges related to how ecological interactions control N cycling processes:
1. linking functional diversity of soil fauna to N cycling processes beyond mineralization;
2. determining the functional relationship between root traits and soil N cycling;
3. characterizing the control that different types of mycorrhizal symbioses exert on N cycling;
4. quantifying the contribution of non-symbiotic pathways to total N fixation fluxes in natural systems
We postulate that addressing these challenges will constitute a comprehensive research agenda with respect to the N cycle for the next decade. Such an agenda would help us to meet future challenges on food and energy security, biodiversity conservation, water and air quality, and climate stability.
| คีย์อ้างอิง |
groenigen2015soilthe
ใช้คีย์นี้เพื่ออ้างอิงอัตโนมัติในต้นฉบับขณะใช้งาน
SciMatic Manuscript Manager หรือ Thesis Manager
|
|---|---|
| ผู้เขียน | ;J. W. van Groenigen;D. Huygens;P. Boeckx;Th. W. Kuyper;I. M. Lubbers;T. Rütting;P. M. Groffman |
| วารสาร | energy and environment |
| ปี | 2015 |
| DOI |
10.5194/soil-1-235-2015
|
| URL | |
| คำสำคัญ |
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