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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Microbial carbon use efficiency and priming effect regulate soil carbon storage under nitrogen deposition by slowing soil organic matter decomposition
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Microbial carbon use efficiency and priming effect regulate soil carbon storage under nitrogen deposition by slowing soil organic matter decomposition

机译:通过减缓土壤有机质分解,微生物碳利用效率和引发效果调节氮沉积下的土壤碳储存

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Microbial carbon use efficiency (CUE) strongly influences the rate of soil organic carbon (SOC) formation by mediating C loss via microbial respiration, whereas the priming effect plays a crucial role in regulating the stability of SOC. Nitrogen (N) deposition increases N availability and alters litter quality and quantity, both of which could strongly affect the CUE and priming effect. However, it remains unclear whether and how, under N deposition, the CUE and priming effect could affect soil C cycling. In this study, we conducted a consecutive 12-yr N addition experiment in a temperate steppe. We evaluated how increasing N inputs affect soil C accumulation, microbial respiration, microbial biomass and composition in the field. We also performed an incubation experiment by adding C-13 labeled glucose and phenol to the pre-incubated soils to test how N addition affects microbial CUE and the priming effects on stable soil C. Our field experiment showed that N addition increased soil organic C concentration and decreased soil microbial respiration, microbial total phospholipid fatty acids (PLFAs), and fungi to bacteria (F:B) ratio. Our incubation experiments indicated that N addition increased microbial CUE of glucose but decreased that of phenol. The priming effects of both glucose and phenol were suppressed by N addition. Redundancy analysis (RDA) showed the importance of fungi in regulating microbial CUE and priming effect Specifically, multi-model averaging suggested that the decreased fungal biomass under N addition was the most important predictor for changes in CUE of glucose, while decreased fungal biomass and F:B ratio were the most important predictors for changes in the CUE and priming effects. In addition, the increased CUE of glucose best explained the decreased microbial respiration, and the reduced priming effect of glucose best explained the increased SOC under N addition. Overall, our finding suggested that N addition would alter microbial CUE and the priming effects on stable soil C. The different responses of CUE and priming effects to glucose and phenol addition imply that the decreased microbial respiration and increased C storage under N deposition could be more attributed to labile C inputs rather than recalcitrant C inputs.
机译:微生物碳利用效率(提示)强烈影响通过微生物呼吸介导C损失的土壤有机碳(SoC)形成的速率,而引发效果在调节SoC的稳定性方面发挥着至关重要的作用。氮气(n)沉积增加N可用性并改变垃圾质量和数量,这两者都能强烈影响提示和引发效果。然而,仍然不清楚是否和如何在n沉积,提示和引发效果下会影响土壤c循环。在这项研究中,我们在温带草原中进行了连续的12 yR N添加实验。我们评估了N个输入如何影响土壤C累积,微生物呼吸,微生物生物量和田间组成的程度。我们还通过将C-13标记的葡萄糖和苯酚添加到预培养的土壤中进行培养实验,以测试N添加影响微生物提示和对稳定土壤C的引发效果。我们的田间实验表明N添加增加的土壤有机C浓度土壤微生物呼吸,微生物总磷脂脂肪酸(PLFA)和真菌(F:B)比例减少。我们的孵育实验表明,N添加增加的葡萄糖微生物提示,但降低了苯酚。通过添加抑制葡萄糖和苯酚的引发效果。冗余分析(RDA)表明真菌在调节微生物提示和引发效果方面的重要性,多模型平均表明,N添加下的真菌生物量减少是葡萄糖提示变化的最重要的预测因素,而真菌生物量和F降低:B比率是提示和引发效应的变化最重要的预测因子。此外,葡萄糖的增加最佳解释了降低的微生物呼吸,而且葡萄糖的引发效果降低最佳地解释了N添加下的SOC增加。总体而言,我们的发现表明,N添加会改变微生物提示和对稳定土壤Cue的引发效果。提示和灌注对葡萄糖和酚添加的不同反应意味着N沉积下的微生物呼吸和增加的C储存增加可能更多归因于不稳定的C输入而不是rulalcrant C输入。

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