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Different responses of soil respiration and its components to nitrogen addition among biomes: a meta-analysis

机译:生物群落间土壤呼吸及其对氮素添加的不同反应:荟萃分析

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Anthropogenic activities have increased nitrogen (N) deposition by threefold to fivefold over the last century, which may considerably affect soil respiration (Rs). Although numerous individual studies and a few meta-analyses have been conducted, it remains controversial as to how N addition affects Rs and its components [i.e., autotrophic (Ra) and heterotrophic respiration (Rh)]. To reconcile the difference, we conducted a comprehensive meta-analysis of 295 published studies to examine the responses of Rs and its components to N addition in terrestrial ecosystems. We also assessed variations in their responses in relation to ecosystem types, environmental conditions, and experimental duration (DUR). Our results show that N addition significantly increased Rs by 2.0% across all biomes but decreased by 1.44% in forests and increased by 7.84% and 12.4% in grasslands and croplands, respectively (P < 0.05). The differences may largely result from diverse responses of Ra to N addition among biomes with more stimulation of Ra in croplands and grasslands compared with no significant change in forests. Rh exhibited a similar negative response to N addition among biomes except that in croplands, tropical and boreal forests. Methods of partitioning Rs did not induce significant differences in the responses of Ra or Rh to N addition, except that Ra from root exclusion and component integration methods exhibited the opposite responses in temperate forests. The response ratios (RR) of Rs to N addition were positively correlated with mean annual temperature (MAT), with being more significant when MAT was less than 15 degrees C, but negatively with DUR. In addition, the responses of Rs and its components to N addition largely resulted from the changes in root and microbial biomass and soil C content as indicated by correlation analysis. The response patterns of Rs to N addition as revealed in this study can be benchmarks for future modeling and experimental studies
机译:在上个世纪,人为活动使氮(N)的沉积增加了三倍至五倍,这可能会大大影响土壤呼吸(Rs)。尽管已经进行了许多单独的研究和一些荟萃分析,但是关于氮的添加如何影响Rs及其成分[即自养(Ra)和异养呼吸(Rh)]仍存在争议。为了调和差异,我们对295项已发表的研究进行了全面的荟萃分析,以研究陆地生态系统中Rs及其组分对N添加的响应。我们还评估了它们对生态系统类型,环境条件和实验持续时间(DUR)的反应差异。我们的结果表明,在所有生物群落中,氮素的添加显着增加Rs 2.0%,而在森林中则减少了1.44%,在草地和农田中分别减少了7.84%和12.4%(P <0.05)。差异可能主要是由于生物群落中Ra对N添加的不同响应,而农田和草地对Ra的刺激更大,而森林没有明显变化。 Rh在生物群落中对氮的添加表现出相似的负响应,除了农田,热带和北方森林以外。分配Rs的方法没有引起Ra或Rh对氮添加的响应的显着差异,除了根部排斥和成分整合方法产生的Ra在温带森林中表现出相反的响应。 Rs对N添加的响应比(RR)与年平均温度(MAT)正相关,当MAT低于15摄氏度时则更显着,而与DUR负相关。另外,相关分析表明,根及其微生物量和土壤碳含量的变化主要是由于Rs及其组分对N的响应。本研究揭示的Rs对N加成的响应模式可以作为未来建模和实验研究的基准

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