Stable isotopic constraints on global soil organic carbon turnover
Carbon dioxide release during soil organic carbon (SOC) turnover is a pivotal component of atmospheric CO<sub>2</sub> concentrations and global climate change. However, reliably measuring SOC turnover rates on large spatial and temporal scales remains challenging. Here we use a natura...
| Príomhchruthaitheoirí: | , , , , , |
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| Formáid: | Alt |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
Copernicus Publications
2018-02-01
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| Sraith: | Biogeosciences |
| Rochtain ar líne: | https://www.biogeosciences.net/15/987/2018/bg-15-987-2018.pdf |