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Impact of tropical land-use change on soil organic carbon stocks - a meta-analysis.

机译:热带土地利用变化对土壤有机碳储量的影响-荟萃分析。

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Land-use changes are the second largest source of human-induced greenhouse gas emission, mainly due to deforestation in the tropics and subtropics. CO2 emissions result from biomass and soil organic carbon (SOC) losses and may be offset with afforestation programs. However, the effect of land-use changes on SOC is poorly quantified due to insufficient data quality (only SOC concentrations and no SOC stocks, shallow sampling depth) and representativeness. In a global meta-analysis, 385 studies on land-use change in the tropics were explored to estimate the SOC stock changes for all major land-use change types. The highest SOC losses were caused by conversion of primary forest into cropland (-25%) and perennial crops (-30%) but forest conversion into grassland also reduced SOC stocks by 12%. Secondary forests stored less SOC than primary forests (-9%) underlining the importance of primary forests for C stores. SOC losses are partly reversible if agricultural land is afforested (+29%) or under cropland fallow (+32%) and with cropland conversion into grassland (+26%). Data on soil bulk density are critical in order to estimate SOC stock changes because (i) the bulk density changes with land-use and needs to be accounted for when calculating SOC stocks and (ii) soil sample mass has to be corrected for bulk density changes in order to compare land-use types on the same basis of soil mass. Without soil mass correction, land-use change effects would have been underestimated by 28%. Land-use change impact on SOC was not restricted to the surface soil, but relative changes were equally high in the subsoil, stressing the importance of sufficiently deep sampling.
机译:土地利用变化是人为引起的温室气体排放的第二大来源,主要是由于热带和亚热带地区的森林砍伐。 CO 2 排放源于生物量和土壤有机碳(SOC)的损失,并可能被造林计划所抵消。但是,由于数据质量不足(仅SOC浓度而无SOC存量,采样深度较浅)和代表性不足,土地利用变化对SOC的影响难以量化。在一项全球荟萃分析中,对热带地区的土地利用变化进行了385项研究,以估算所有主要土地利用变化类型的SOC储量变化。 SOC损失最高的是原始森林转化为农田(-25%)和多年生作物(-30%),但森林转化为草地也使SOC储量减少了12%。次生林的SOC低于原生林(-9%),这突显了原始林对C库的重要性。如果农地被绿化(+ 29%)或耕地休耕(+ 32%)并且农田转化为草地(+ 26%),则SOC损失可部分逆转。关于土壤容重数据对于估算SOC存量变化至关重要,因为(i)容重随土地使用而变化,在计算SOC存量时需要考虑在内,并且(ii)必须针对容重校正土壤样品质量为了在相同的土壤质量基础上比较土地利用类型而进行的改变。如果不进行土壤质量校正,土地利用变化的影响将被低估28%。土地利用变化对土壤有机碳的影响不仅限于表层土壤,而且相对变化在地下土壤中同样高,从而强调了进行足够深度采样的重要性。

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