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轻度放牧有利于中国草原表土以下土壤碳的积累:一项荟萃分析。

Light grazing facilitates carbon accumulation in subsoil in Chinese grasslands: A meta-analysis.

机构信息

School of Geography, South China Normal University, Guangzhou, China.

Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai, China.

出版信息

Glob Chang Biol. 2020 Dec;26(12):7186-7197. doi: 10.1111/gcb.15326. Epub 2020 Oct 4.

Abstract

Grazing by livestock greatly affects the soil carbon (C) cycle in grassland ecosystems. However, the effects of grazing at different intensities and durations on the dynamics of soil C in its subsoil layers are not clearly understood. Here, we compiled data from 78 sites (in total 122 published studies) to examine the effects of varying grazing intensities and durations on soil C content at different depths for grasslands in China. Our meta-analysis revealed that grazing led to an overall decrease in soil C content and productivity of above-ground vegetation (e.g., above-ground biomass and litter) but an increase in below-ground biomass. Specifically, the effects of grazing on soil C content became less negative or even positive with increasing soil depths. An increase of soil C content was consequently found under light grazing (LG), although soil C content still decreased under moderate and heavy grazing. The increase in soil C content under LG could be largely attributed to the increase of soil C content in subsoil layers (>20 cm), despite that soil C content in surface soil layer (0-20 cm) decreased. Moreover, the magnitude of increase in soil C content under LG in subsoil layers increased with grazing duration. A possible reason of the increase in soil C content in the subsoil layers was due to the increases in below-ground biomass. Our study highlights that LG may modify the allocation of C input and promote its accumulation in subsoil layers, thus offsetting the negative impact of grazing on surface soil C content, a finding that has significant implications for C sequestration in grasslands.

摘要

放牧对草原生态系统土壤碳(C)循环有很大的影响。然而,不同强度和持续时间的放牧对土壤中下层土壤 C 动态的影响尚不清楚。在这里,我们汇总了来自 78 个地点(共 122 个已发表的研究)的数据,以研究中国草原不同放牧强度和持续时间对不同深度土壤 C 含量的影响。我们的荟萃分析表明,放牧导致土壤 C 含量和地上植被生产力(如地上生物量和凋落物)总体下降,但地下生物量增加。具体来说,随着土壤深度的增加,放牧对土壤 C 含量的影响变得不那么负面,甚至可能是正面的。尽管在中度和重度放牧下土壤 C 含量仍在下降,但轻度放牧(LG)下发现土壤 C 含量增加。LG 下土壤 C 含量的增加主要归因于亚表层土壤(>20 cm)中土壤 C 含量的增加,尽管表层土壤(0-20 cm)中的土壤 C 含量下降。此外,LG 下亚表层土壤 C 含量增加的幅度随着放牧持续时间的增加而增加。亚表层土壤 C 含量增加的一个可能原因是地下生物量的增加。我们的研究强调,LG 可能会改变 C 输入的分配,并促进其在亚表层土壤中的积累,从而抵消放牧对表层土壤 C 含量的负面影响,这一发现对草原碳固存具有重要意义。

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