globalchange  > 全球变化的国际研究计划
DOI: 10.1111/1365-2435.13433
WOS记录号: WOS:000484020400001
论文题名:
Nitrogen addition reduces soil respiration but increases the relative contribution of heterotrophic component in an alpine meadow
作者: Wang, Jinsong1; Song, Bing1,2; Ma, Fangfang1,2; Tian, Dashuan1; Li, Yong3; Yan, Tao4; Quan, Quan1,2; Zhang, Fangyue1,2; Li, Zhaolei1; Wang, Bingxue1; Gao, Qiang5; Chen, Weinan1,2; Niu, Shuli1,2
通讯作者: Niu, Shuli
刊名: FUNCTIONAL ECOLOGY
ISSN: 0269-8463
EISSN: 1365-2435
出版年: 2019
语种: 英语
英文关键词: nitrogen addition gradient ; nonlinear response ; plant community composition ; sensitivity ; soil respiration components ; soil substrate quality ; soil temperature
WOS关键词: CARBON-USE EFFICIENCY ; EXTRACELLULAR ENZYME-ACTIVITIES ; MICROBIAL BIOMASS ; AUTOTROPHIC RESPIRATION ; TEMPERATE GRASSLAND ; GLOBAL CHANGE ; FERTILIZATION ; RESPONSES ; DEPOSITION ; CO2
WOS学科分类: Ecology
WOS研究方向: Environmental Sciences & Ecology
英文摘要:

Disentangling the relative response sensitivity of soil autotrophic (R-a) and heterotrophic respiration (R-h) to nitrogen (N) enrichment is pivotal for evaluating soil carbon (C) storage and stability in the scenario of intensified N deposition. However, the mechanisms underlying differential sensitivities of R-a and R-h and relative contribution of R-h to soil respiration (R-s) with increasing N deposition remain elusive. A manipulative field experiment with multi-level N addition rates was conducted over 3 years (2015-2017) in an alpine meadow to explore the relative impact of N enrichment on R-a and R-h and the response of R-h/R-s ratio to the gradient of N addition. Soil respiration components had different sensitivities to N enrichment, with R-a decreasing more than R-h, leading to a higher R-h/R-s ratio as a function of increasing N addition rates. R-a and R-h decreased nonlinearly as N addition rates increased, with a critical load of 8 g N m(-2) year(-1) above which N enrichment significantly inhibited them. R-a and R-h were controlled by different abiotic and biotic factors, and the regulation of controlling factors on soil respiration components varied over time. N-induced reduction in the relative abundance of forb significantly affected R-a, and this effect was mainly evident in the second and third years. Nitrogen enrichment significantly changed R-h in the third year, and the decreased R-h under high doses of N addition could be attributed to the changes in microbial biomass C, soil substrate quality and microbial composition. Our study highlights the leading role of R-a in regulating R-s responses to N enrichment and the enhancement of R-h/R-s ratio with increasing N addition. We also emphasize that N-induced shifts in plant community composition play a vital role in regulating R-a instead of R-h. The changing drivers of R-a and R-h with time suggests that long-term experiments with multiple levels of N addition are further needed to test the nonlinear responses and underlying mechanisms of soil respiration components in face to aggravating N deposition. A free Plain Language Summary can be found within the Supporting Information of this article.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/145789
Appears in Collections:全球变化的国际研究计划

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作者单位: 1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Chinese Acad Forestry, Inst Wetland Res, Beijing Key Lab Wetland Serv & Restorat, Beijing, Peoples R China
4.Lanzhou Univ, Coll Pastoral Agr Sci & Technol, Key Lab Grassland & Agroecosyst, Lanzhou, Gansu, Peoples R China
5.East Normal Univ, Sch Ecol & Environm Sci, Shanghai, Peoples R China

Recommended Citation:
Wang, Jinsong,Song, Bing,Ma, Fangfang,et al. Nitrogen addition reduces soil respiration but increases the relative contribution of heterotrophic component in an alpine meadow[J]. FUNCTIONAL ECOLOGY,2019-01-01
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