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[中国青藏高原不同退化阶段高寒草甸的植物群落与土壤养分]。

[Plant community and soil nutrient of alpine meadow in different degradation stages on the Tibetan Plateau, China.].

作者信息

Yang Jun, Liu Qiu-Rong, Wang Xiang-Tao

机构信息

CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization/Ecological Restoration and Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China.

University of Chinese Academy of Sciences, Beijing 100049, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2020 Dec;31(12):4067-4072. doi: 10.13287/j.1001-9332.202012.008.

Abstract

We examined soil physical and chemical properties and plant community characteristics of four alpine meadows at different degradation stages in Damxung County, Lhasa City, Tibet Autonomous Region, China, with the method of spatial sequence instead of time succession. The results showed that soil organic carbon, total nitrogen, available phosphorus, available potassium, ammonium, nitrate, and water content showed a decreasing trend as the degree of soil degradation increased, while pH showed an increasing trend. Plant community height, richness, diversity index and evenness index of the moderately degraded meadow were the highest. Community coverage and total biomass were the largest in undegraded meadow and the smallest in the severely degraded meadow. As the degree of meadow degradation intensifies, the biomass and proportion of Cyperaceae decreased, the biomass and proportion of legumes and weeds increased, and the biomass and proportion of Gramineae first increased and then decreased. The aboveground biomass of meadow was significantly positively correlated with soil organic carbon content, total nitrogen content, total phosphorus content, and soil water content, and significantly negatively correlated with soil pH. With the vegetation degradation in meadow, soil degradation had worsened, which ultimately manifested as a significant decline in grassland productivity.

摘要

我们采用空间序列代替时间演替的方法,对中国西藏自治区拉萨市当雄县四个不同退化阶段的高寒草甸的土壤理化性质和植物群落特征进行了研究。结果表明,随着土壤退化程度的增加,土壤有机碳、全氮、有效磷、速效钾、铵态氮、硝态氮和含水量呈下降趋势,而pH值呈上升趋势。中度退化草甸的植物群落高度、丰富度、多样性指数和均匀度指数最高。群落盖度和总生物量在未退化草甸中最大,在重度退化草甸中最小。随着草甸退化程度的加剧,莎草科的生物量和比例下降,豆科和杂草的生物量和比例增加,禾本科的生物量和比例先增加后下降。草甸地上生物量与土壤有机碳含量、全氮含量、全磷含量和土壤含水量呈显著正相关,与土壤pH值呈显著负相关。随着草甸植被的退化,土壤退化加剧,最终表现为草地生产力显著下降。

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