Lu Xuyang, Yan Yan, Sun Jian, Zhang Xiaoke, Chen Youchao, Wang Xiaodan, Cheng Genwei
Key Laboratory of Mountain Surface Processes and Ecological Regulation Chinese Academy of Sciences Chengdu 610041 China ; Xainza Alpine Steppe and Wetland Ecosystem Observation and Experiment Station Chinese Academy of Sciences Xainza 853100 China.
Key Laboratory of Mountain Surface Processes and Ecological Regulation Chinese Academy of Sciences Chengdu 610041 China.
Ecol Evol. 2015 Sep 23;5(19):4492-504. doi: 10.1002/ece3.1732. eCollection 2015 Oct.
In recent decades, alpine grasslands have been seriously degraded on the Tibetan Plateau and grazing exclusion by fencing has been widely adopted to restore degraded grasslands since 2004. To elucidate how alpine grasslands carbon (C), nitrogen (N), and phosphorus (P) storage responds to this management strategy, three types of alpine grassland in nine counties in Tibet were selected to investigate C, N, and P storage in the environment by comparing free grazing (FG) and grazing exclusion (GE) treatments, which had run for 6-8 years. The results revealed that there were no significant differences in total ecosystem C, N, and P storage, as well as the C, N, and P stored in both total biomass and soil (0-30 cm) fractions between FG and GE grasslands. However, precipitation played a key role in controlling C, N, and P storage and distribution. With grazing exclusion, C and N stored in aboveground biomass significantly increased by 5.7 g m(-2) and 0.1 g m(-2), respectively, whereas the C and P stored in the soil surface layer (0-15 cm) significantly decreased by 862.9 g m(-2) and 13.6 g m(-2), respectively. Furthermore, the storage of the aboveground biomass C, N, and P was positively correlated with vegetation cover and negatively correlated with the biodiversity index, including Pielou evenness index, Shannon-Wiener diversity index, and Simpson dominance index. The storage of soil surface layer C, N, and P was positively correlated with soil silt content and negatively correlated with soil sand content. Our results demonstrated that grazing exclusion had no impact on total C, N, and P storage, as well as C, N, and P in both total biomass and soil (0-30 cm) fractions in the alpine grassland ecosystem. However, grazing exclusion could result in increased aboveground biomass C and N pools and decreased soil surface layer (0-15 cm) C and P pools.
近几十年来,青藏高原的高寒草原严重退化,自2004年以来,广泛采用围栏禁牧来恢复退化草原。为阐明高寒草原碳(C)、氮(N)和磷(P)储量对这种管理策略的响应,选取了西藏9个县的三种类型高寒草原,通过比较自由放牧(FG)和禁牧(GE)处理(已进行6 - 8年)来调查环境中的C、N和P储量。结果表明,FG和GE草原在生态系统总C、N和P储量以及总生物量和土壤(0 - 30厘米)部分中储存的C、N和P方面没有显著差异。然而,降水在控制C、N和P储量及分布方面起关键作用。禁牧后,地上生物量中储存的C和N分别显著增加了5.7克/平方米和0.1克/平方米,而土壤表层(0 - 15厘米)中储存的C和P分别显著减少了862.9克/平方米和13.6克/平方米。此外,地上生物量C、N和P的储量与植被覆盖呈正相关,与包括皮洛均匀度指数、香农 - 威纳多样性指数和辛普森优势度指数在内的生物多样性指数呈负相关。土壤表层C、N和P的储量与土壤粉粒含量呈正相关,与土壤砂粒含量呈负相关。我们的结果表明,禁牧对高寒草原生态系统的总C、N和P储量以及总生物量和土壤(0 - 30厘米)部分中的C、N和P没有影响。然而,禁牧可能导致地上生物量C和N库增加,土壤表层(0 - 15厘米)C和P库减少。