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放牧禁牧对高寒灌丛草甸温室气体排放和土壤有机碳周转的影响。

Effect of grazing exclusion on emission of greenhouse gases and soil organic carbon turnover in alpine shrub meadow.

作者信息

Dang Zhiqiang, Guo Na, Li Shanshan, Degen A Allan, Cao Jingjuan, Deng Bin, Wang Aidong, Peng Zhen, Ding Luming, Long Ruijun, Shang Zhanhuan

机构信息

State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, College of ecology, Lanzhou University, Lanzhou 730000, China.

State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, College of Pastoral Agriculture Science and Technology, Lanzhou University, Lanzhou 730020, China.

出版信息

Sci Total Environ. 2023 Feb 1;858(Pt 1):159758. doi: 10.1016/j.scitotenv.2022.159758. Epub 2022 Nov 4.

Abstract

Grazing exclusion (GE) is a management option used widely to restore degraded grassland and improve grassland ecosystems. However, the impacts of GE on soil properties and greenhouse gas emissions of alpine shrub meadow are still unclear, especially long-term GE of more than ten years. To fill part of this gap, we examined the effects of long-term GE of alpine shrub meadow on soil nutrients, soil properties, greenhouse gas emissions (CO and CH) and soil organic carbon (SOC) turnover. When compared to grazed grassland (GG), long-term GE resulted in: 1) greater SOC, nitrogen (N), and phosphorous (P) content, especially in the 20-30 cm soil layer; 2) greater soil C:N, C:P and N:P ratios in the 20-30 cm depth; 3) greater soil CO, but lesser CH emission during the growing season; and 4) much faster SOC turnover time (0-30 cm). GE of more than ten years can increase grassland C reserves and improve the C sequestration capacity of the ecosystem. Results from this study can have important implications in developing future grassland management policies on soil nutrient balances, restoration of degraded grassland and controlling shrub expansion.

摘要

禁牧是一种广泛应用于恢复退化草地和改善草地生态系统的管理措施。然而,禁牧对高寒灌丛草甸土壤性质和温室气体排放的影响仍不明确,尤其是超过十年的长期禁牧。为了填补这一空白,我们研究了高寒灌丛草甸长期禁牧对土壤养分、土壤性质、温室气体排放(CO和CH)以及土壤有机碳(SOC)周转的影响。与放牧草地(GG)相比,长期禁牧导致:1)SOC、氮(N)和磷(P)含量更高,尤其是在20-30厘米土层;2)20-30厘米深度的土壤C:N、C:P和N:P比值更高;3)生长季土壤CO排放更高,但CH排放更低;4)SOC周转时间(0-30厘米)快得多。超过十年的禁牧可以增加草地碳储量,提高生态系统的碳固存能力。本研究结果对制定未来关于土壤养分平衡、退化草地恢复和控制灌丛扩张的草地管理政策具有重要意义。

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