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放牧通过改变中国东北青藏高原的地表物理环境来改变高山草原的物候。

Grazing alters the phenology of alpine steppe by changing the surface physical environment on the northeast Qinghai-Tibet Plateau, China.

机构信息

Institute of Agricultural Sci-tech Information, Beijing Academy of Agricultural and Forestry Sciences, Beijing 100097, China; National Geomatics Center of China, Beijing 100830, China.

Institute of Agricultural Sci-tech Information, Beijing Academy of Agricultural and Forestry Sciences, Beijing 100097, China.

出版信息

J Environ Manage. 2019 Oct 15;248:109257. doi: 10.1016/j.jenvman.2019.07.028. Epub 2019 Jul 22.

DOI:10.1016/j.jenvman.2019.07.028
PMID:31344560
Abstract

The response of vegetation phenology to environmental changes is very complex. We used time-lapse digital cameras to monitor the phenology of an alpine steppe in four winter pastures with different grazing intensities during 2015-2017. The results showed that the beginning of the growing season (BGS) and the growing season length (GSL) of the alpine steppe separately presented advances or prolonged trends with the increase in grazing intensity. There was no regularity in the end of the growing season (EGS) under the change in grazing intensity gradient, but the EGS of the no grazing (NG) plot occurred 24 days ahead of the other plots disturbed by grazing. Different winter grazing intensities obviously had different influences on the surface litter, soil temperature (ST), and soil moisture (SM) during spring but not during autumn. The ST under different grazing intensities played a decisive role in controlling the BGS of alpine steppe, followed by surface litter and SM. The EGS showed a significant correlation with the surface litter in autumn but did not show correlations with ST and SM. These results could further help us understand the phenological mechanisms of the soil surface and guide the scientific management of grazing to adapt to climate change.

摘要

植被物候对环境变化的响应非常复杂。我们使用延时数字摄像机,在 2015 年至 2017 年间,对四个冬季牧场的高山草原物候进行了监测,这四个牧场的放牧强度不同。结果表明,高山草原的生长季开始期(BGS)和生长季长度(GSL)分别呈现出随放牧强度增加而提前或延长的趋势。在放牧强度梯度变化下,生长季结束期(EGS)没有规律,但不受放牧干扰的不牧(NG)样地的 EGS 比其他受放牧干扰的样地提前了 24 天。不同的冬季放牧强度在春季对地表凋落物、土壤温度(ST)和土壤湿度(SM)有明显不同的影响,但在秋季则没有。不同放牧强度下的 ST 对高山草原的 BGS 起着决定性的控制作用,其次是地表凋落物和 SM。EGS 与秋季的地表凋落物呈显著相关,但与 ST 和 SM 没有相关性。这些结果可以进一步帮助我们了解土壤表面物候机制,并指导科学管理放牧以适应气候变化。

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