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黄河源区退化高寒草甸裸斑恢复过程中碳通量组分的比较响应

Comparative responses of carbon flux components in recovering bare patches of degraded alpine meadow in the Source Zone of the Yellow River.

机构信息

College of Agriculture and Animal Husbandry, State Key Laboratory of Plateau Ecology and Agriculture, Qinghai University, Xining 810016, China.

College of Agriculture and Animal Husbandry, State Key Laboratory of Plateau Ecology and Agriculture, Qinghai University, Xining 810016, China.

出版信息

Sci Total Environ. 2024 Jan 15;908:168343. doi: 10.1016/j.scitotenv.2023.168343. Epub 2023 Nov 4.

Abstract

The patchy degradation of alpine grasslands is a common phenomenon on the Qinghai-Tibetan Plateau, and the presence of bare patches (BP) in degraded grasslands significantly affects the functioning of the alpine meadow ecosystem. The succession of vegetation-recovered BP may lead to significant changes in ecosystem carbon (C) cycling. To date, it is unclear whether different components of net ecosystem carbon exchange (NEE) respond similarly or differently to the succession of recovering BP. Here, we conducted a field monitoring experiment in a degraded alpine meadow, and selected three successional stages for recovering BP to study the response of NEE and its components. We found that the succession of recoevering BP increased ecosystem respiration (ER) during the growing season and decreased ER during the off-growing season, with the differences in annual carbon output between different successional stages being insignificant. However, gross primary productivity increased with the successional gradient, and carbon input at the later stage of succession was significantly greater than that at the middle stage of succession. The succession of recovering BP promoted the carbon sequestration function of the alpine grassland, with the grassland acting as a carbon sink when it reached the state of healthy alpine meadow, while it acted as a carbon source during the middle stage of succession. Compared with BP, the amount of carbon sequested by healthy alpine meadows increased significantly by 219 g·C·m·yr. We also found that the responses of other components to the succession of recovering BP were inconsistent. In addition, the effects of succession of recovering BP on carbon flux were related to field-monitored variables (soil temperature and water content) and other considered variables (biomass, organic carbon, and microbial biomass carbon). These research findings highlight the importance of restoring vegetation in BPs, and are crucial for predicting the carbon balance in the future and formulating sustainable grassland management strategies.

摘要

高山草地的斑块状退化是青藏高原普遍存在的现象,退化草地中裸斑块(BP)的存在显著影响高寒草甸生态系统的功能。植被恢复的 BP 的演替可能导致生态系统碳(C)循环发生重大变化。迄今为止,尚不清楚净生态系统碳交换(NEE)的不同组成部分对恢复 BP 的演替是否有相似或不同的响应。在这里,我们在退化的高寒草甸中进行了现场监测实验,选择了恢复 BP 的三个演替阶段来研究 NEE及其组成部分的响应。我们发现,恢复 BP 的演替增加了生长季的生态系统呼吸(ER),减少了非生长季的 ER,不同演替阶段之间的年碳输出差异不显著。然而,总初级生产力随演替梯度增加,演替后期的碳输入明显大于中期。恢复 BP 的演替促进了高寒草地的碳固存功能,当草地达到健康高寒草甸状态时,草地作为碳汇,而在演替中期则作为碳源。与 BP 相比,健康高寒草甸的碳固存量增加了 219 g·C·m·yr。我们还发现,其他组件对恢复 BP 的演替的响应不一致。此外,恢复 BP 的演替对碳通量的影响与现场监测变量(土壤温度和水分含量)和其他考虑变量(生物量、有机碳和微生物生物量碳)有关。这些研究结果强调了恢复 BP 植被的重要性,对于预测未来的碳平衡和制定可持续的草地管理策略至关重要。

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