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Impact of Different Land Use on Topsoil Organic Carbon Density in Anhui Province

机译:不同土地利用对安徽省表土有机碳密度的影响

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Carbon storage and sequestration is considered to be an important issue in study of terrestrial C cycling and global climatic change.Regional C pool estimate is a fundamental data for describing C pool dynamics under human activities.This paper deals with a provincial baseline topsoil C pool estimate by using the soil series data collected from the 2nd national soil survey. The total topsoil SOC density is(31.64±16.39)C/hm~2, with (36.36±18.75)C/hm~2 from the forest soils, (17.58±6.07)C/hm~2 from dryland soils and(27.7±6.72)C/hm~2 from the plow layer of paddy soil and(14.11±6.44)C/hm~2 from plow layer.The estimated total topsoil SOC pool is 0.28Pg, with 0.14Pg in the forest soils, 0.05Pg in the dryland soils and 0.09Pg in paddy soils.The SOC density and pool was found reflecting the impacts by land use patterns.The SOC storage was found related to the clay content and N enrichment in soils.
机译:碳储存和封存被认为是陆地C骑自行车和全球气候变化研究的重要问题。详细的C池估计是用于描述人类活动下的C池动态的基本数据。本文涉及省级基线表土C池估计通过使用第二次国家土壤调查所收集的土壤系列数据。总皮索SOC密度为(31.64±16.39)C / HM〜2,森林土壤(36.36±18.75)C / HM〜2,旱地土壤(17.58±6.07)C / HM〜2)和(27.7± 6.72)C / HM〜2从水稻土的犁层和(14.11±6.44)C / HM〜2来自犁层。估计总皮索SOC池为0.28pg,森林土壤中有0.14pg,0.05pg Dryland土壤和0.09pg在水稻土中。发现SOC密度和池反映了土地利用模式的影响。发现SOC储存与土壤中的粘土含量和N富集有关。

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