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Soil organic carbon pools in the northern circumpolar permafrost region

机译:北部极地多年冻土区的土壤有机碳库

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摘要

The Northern Circumpolar Soil Carbon Database was developed in order to determine carbon pools in soils of the northern circumpolar permafrost region. The area of all soils in the northern permafrost region is approximately 18,782 × 10~3 km~2, or approximately 16% of the global soil area. In the northern permafrost region, organic soils (peatlands) and cryoturbated permafrost-affected mineral soils have the highest mean soil organic carbon contents (32.2-69.6 kg m~(-2)). Here we report a new estimate of the carbon pools in soils of the northern permafrost region, including deeper layers and pools not accounted for in previous analyses. Carbon pools were estimated to be 191.29 Pg for the 0-30 cm depth, 495.80 Pg for the 0-100 cm depth, and 1024.00 Pg for the 0-300 cm depth. Our estimate for the first meter of soil alone is about double that reported for this region in previous analyses. Carbon pools in layers deeper than 300 cm were estimated to be 407 Pg in yedoma deposits and 241 Pg in deltaic deposits. In total, the northern permafrost region contains approximately 1672 Pg of organic carbon, of which approximately 1466 Pg, or 88%, occurs in perennially frozen soils and deposits. This 1672 Pg of organic carbon would account for approximately 50% of the estimated global belowground organic carbon pool.
机译:开发了北极地极土壤碳数据库,以便确定北极地极多年冻土地区土壤中的碳库。北部多年冻土区的所有土壤面积约为18782×10〜3 km〜2,约占全球土壤面积的16%。在北部多年冻土地区,有机土壤(草原)和受冻土冻土影响的矿物土壤的平均土壤有机碳含量最高(32.2-69.6 kg m〜(-2))。在这里,我们报告了北部多年冻土地区土壤碳库的新估计,包括先前分析中未考虑的更深层和碳库。碳池估计为0-30厘米深度为191.29 Pg,0-100厘米深度为495.80 Pg,0-300厘米深度为1024.00 Pg。我们仅对第一米土壤的估计约为先前分析中该地区报告的两倍。据估计,在深度大于300 cm的层中,碳氢化合物在yedoma沉积物中为407 Pg,在三角洲沉积物中为241 Pg。总体而言,北部多年冻土地区含有约1672 Pg的有机碳,其中约1466 Pg或88%的有机碳存在于常年冻结的土壤和沉积物中。这1672 Pg的有机碳将占估计的全球地下有机碳库的大约50%。

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