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Nonlinear response of soil respiration to increasing nitrogen additions in a Tibetan alpine steppe
Peng, Yunfeng1; Li, Fei1,2; Zhou, Guoying3,4; Fang, Kai1; Zhang, Dianye1; Li, Changbin2,3,4; Yang, Guibiao1; Wang, Guanqin1; Wang, Jun1; Mohammat, Anwar5; Yang, Yuanhe1
2017-02-01
发表期刊ENVIRONMENTAL RESEARCH LETTERS
卷号12期号:2
文章类型Article
摘要Nitrogen (N) availability is a key regulator of carbon (C) cycling in terrestrial ecosystems. Anthropogenic N input, such as N deposition and fertilization, increases N availability in soil, which has important implications for an ecosystem's C storage and loss. Soil respiration (Rs), which is the second largest C flux from terrestrial ecosystems to the atmosphere, plays an important role in terrestrial C cycles. The direction and magnitude of the responses of Rs and its components to N addition have been widely evaluated, but it remains unclear how these processes change across multiple N addition levels. Here we conducted a two-year field experiment to examine the changes of Rs and its autotrophic respiration (Ra) and heterotrophic respiration (Rh) components along a gradient of eight N levels (0, 1 2, 4, 8, 16, 24, 32 g m(-2) yr(-1)) in a Tibetan alpine steppe, and used structural equation modeling (SEM) to explore the relative contributions of biotic and abiotic variables and their direct and indirect pathways regulating the Ra and Rh. Our results indicated that both Rs and Ra exhibited first increasing and then subsequent decreasing trends at the threshold of 8 g N m(-2) yr(-1). In contrast, the Rh declined linearly with the N addition rate continuously increasing. SEM analysis revealed that, among various environmental factors, soil temperature was the most important one modulating Rs, which not only had a direct effect on the two Rs components, but also indirectly regulated the Ra and Rh via root and microbial biomass. These findings suggest that the nonlinear response patterns of Rs should be considered for better predicting terrestrial C balance, given that anthropogenic N input to the terrestrial ecosystems is increasing continuously.
关键词Autotrophic Respiration Carbon (c) Cycling Heterotrophic Respiration Nitrogen (n) Input Structural Equation Modeling (Sem)
WOS标题词Science & Technology ; Life Sciences & Biomedicine ; Physical Sciences
DOI10.1088/1748-9326/aa5ba6
关键词[WOS]ECOSYSTEM CARBON EXCHANGE ; TEMPERATE STEPPE ; FOREST ECOSYSTEMS ; MICROBIAL BIOMASS ; CO2 EFFLUX ; NUTRIENT AVAILABILITY ; ROOT PRODUCTION ; CLIMATE-CHANGE ; DEPOSITION ; ENRICHMENT
收录类别SCI
语种英语
项目资助者National Natural Science Foundation of China(31670482 ; China Postdoctoral Science Foundation(2013M540160 ; Chinese Academy of Sciences-Peking University Pioneer Collaboration Team ; Thousand Young Talents Program ; 31400417 ; 2014T70140) ; 31322011)
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS记录号WOS:000395741500002
引用统计
被引频次:45[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://210.75.249.4/handle/363003/6801
专题中国科学院西北高原生物研究所
作者单位1.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Northwest Inst Plateau Biol, Xining 810008, Peoples R China
4.Chinese Acad Sci, Key Lab Tibetan Med Res, Xining 810008, Peoples R China
5.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
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GB/T 7714
Peng, Yunfeng,Li, Fei,Zhou, Guoying,et al. Nonlinear response of soil respiration to increasing nitrogen additions in a Tibetan alpine steppe[J]. ENVIRONMENTAL RESEARCH LETTERS,2017,12(2).
APA Peng, Yunfeng.,Li, Fei.,Zhou, Guoying.,Fang, Kai.,Zhang, Dianye.,...&Yang, Yuanhe.(2017).Nonlinear response of soil respiration to increasing nitrogen additions in a Tibetan alpine steppe.ENVIRONMENTAL RESEARCH LETTERS,12(2).
MLA Peng, Yunfeng,et al."Nonlinear response of soil respiration to increasing nitrogen additions in a Tibetan alpine steppe".ENVIRONMENTAL RESEARCH LETTERS 12.2(2017).
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