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在半干旱温带草原中,水分和氮素的可利用性共同控制着生态系统的二氧化碳交换。

Water and nitrogen availability co-control ecosystem CO2 exchange in a semiarid temperate steppe.

作者信息

Zhang Xiaolin, Tan Yulian, Li Ang, Ren Tingting, Chen Shiping, Wang Lixin, Huang Jianhui

机构信息

State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, China.

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

出版信息

Sci Rep. 2015 Oct 23;5:15549. doi: 10.1038/srep15549.

Abstract

Both water and nitrogen (N) availability have significant effects on ecosystem CO2 exchange (ECE), which includes net ecosystem productivity (NEP), ecosystem respiration (ER) and gross ecosystem photosynthesis (GEP). How water and N availability influence ECE in arid and semiarid grasslands is still uncertain. A manipulative experiment with additions of rainfall, snow and N was conducted to test their effects on ECE in a semiarid temperate steppe of northern China for three consecutive years with contrasting natural precipitation. ECE increased with annual precipitation but approached peak values at different precipitation amount. Water addition, especially summer water addition, had significantly positive effects on ECE in years when the natural precipitation was normal or below normal, but showed trivial effect on GEP when the natural precipitation was above normal as effects on ER and NEP offset one another. Nitrogen addition exerted non-significant or negative effects on ECE when precipitation was low but switched to a positive effect when precipitation was high, indicating N effect triggered by water availability. Our results indicate that both water and N availability control ECE and the effects of future precipitation changes and increasing N deposition will depend on how they can change collaboratively in this semiarid steppe ecosystem.

摘要

水分和氮素有效性均对生态系统二氧化碳交换(ECE)有显著影响,生态系统二氧化碳交换包括净生态系统生产力(NEP)、生态系统呼吸(ER)和总生态系统光合作用(GEP)。在干旱和半干旱草原地区,水分和氮素有效性如何影响生态系统二氧化碳交换仍不明确。在中国北方半干旱温带草原开展了一项连续三年添加降雨、降雪和氮素的控制实验,以检验它们在不同自然降水量条件下对生态系统二氧化碳交换的影响。生态系统二氧化碳交换随年降水量增加而增加,但在不同降水量时接近峰值。在自然降水量正常或低于正常水平的年份,添加水分尤其是夏季添加水分对生态系统二氧化碳交换有显著正向影响,但在自然降水量高于正常水平时,由于对生态系统呼吸和净生态系统生产力的影响相互抵消,添加水分对总生态系统光合作用影响不大。当降水量较低时,添加氮素对生态系统二氧化碳交换的影响不显著或呈负向影响,但当降水量较高时则转为正向影响,表明氮素的影响受水分有效性的触发。我们的研究结果表明,水分和氮素有效性均控制着生态系统二氧化碳交换,未来降水变化和氮沉降增加的影响将取决于它们在该半干旱草原生态系统中如何协同变化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3e4/4616041/6fa1606cff9b/srep15549-f1.jpg

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