Improved understanding of changes in soil recalcitrant organic carbon (C) in response to global warming is critical for predicting changes in soil organic C (SOC) storage. Here, we took advantage of a long-term field experiment with increased temperature and precipitation to investigate the effects of warming, increased precipitation and their interactions on SOC fraction in a semiarid Inner Mongolian grassland of northern China since April 2005. We quantified labile SOC, recalcitrant SOC and stable SOC at 0–10 and 10–20 cm depths.
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/warming-rather-increased-precipitation-increases-soil-recalcitrant-organic-carbon
[2] http://admin.indiaenvironmentportal.org.in/category/author/xiaoqi-zhou
[3] http://admin.indiaenvironmentportal.org.in/category/author/chengrong-chen
[4] http://admin.indiaenvironmentportal.org.in/category/author/yanfen-wang-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/plos-one
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/soil-capability
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/global-warming
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/grasslands
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/carbon-sequestration
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/carbon-sinks
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/china
[12] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change