4.7 Article

New soil carbon sequestration with nitrogen enrichment: a meta-analysis

期刊

PLANT AND SOIL
卷 454, 期 1-2, 页码 299-310

出版社

SPRINGER
DOI: 10.1007/s11104-020-04617-x

关键词

Isotopes; Nitrogen saturation; Nitrogen addition; Soil carbon dynamics; Soil carbon input

资金

  1. National Key Research and Development Program of China [2017YFD0300104]
  2. China Scholarship Council (CSC) [201706850042]
  3. US Department of Energy, Terrestrial Ecosystem Sciences [DE SC0008270]
  4. Lawrence Fellow award through Lawrence Livermore National Laboratory (LLNL)
  5. U.S. Department of Energy by LLNL [DE-AC52-07NA27344]
  6. LLNL-LDRD Program [20-ERD-055]

向作者/读者索取更多资源

Background and aims Through agriculture and industry, humans are increasing the deposition and availability of nitrogen (N) in ecosystems worldwide. Carbon (C) isotope tracers provide useful insights into soil C dynamics, as they allow to study soil C pools of different ages. We evaluated to what extent N enrichment affects soil C dynamics in experiments that applied C isotope tracers. Methods Using meta-analysis, we synthesized data from 35 published papers. We made a distinction between new C and old C stocks, i.e., soil C derived from plant C input since the start of the isotopic enrichment, or unlabeled, pre-existing soil C. Results Averaged across studies, N addition increased new soil C stocks (+30.3%), total soil C stocks (+6.1%) and soil C input proxies (+30.7%). Although N addition had no overall, average, effect on old soil C stocks and old soil C respiration, old soil C stocks increased with the amount of N added and respiration of old soil C declined. Nitrogen-induced effects on new soil C and soil C input both decreased with the amount of extraneous N added in control treatments. Conclusion Although our findings require additional confirmation from long-term field experiments, our analysis provides isotopic evidence that N addition stimulates soil C storage both by increasing soil C input and (at high N rates) by decreasing decomposition of old soil C. Furthermore, we demonstrate that the widely reported saturating response of plant growth to N enrichment also applies to new soil C storage.

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