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Litter decay controlled by temperature, not soil properties, affecting future soil carbon

机译:凋落物腐烂受温度控制,而不是土壤性质,影响未来的土壤碳

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Widespread global changes, including rising atmospheric CO2 concentrations, climate warming and loss of biodiversity, are predicted for this century; all of these will affect terrestrial ecosystem processes like plant litter decomposition. Conversely, increased plant litter decomposition can have potential carbon-cycle feedbacks on atmospheric CO2 levels, climate warming and biodiversity. But predicting litter decomposition is difficult because of many interacting factors related to the chemical, physical and biological properties of soil, as well as to climate and agricultural management practices. We applied C-13-labelled plant litter to soil at ten sites spanning a 3500-km transect across the agricultural regions of Canada and measured its decomposition over five years. Despite large differences in soil type and climatic conditions, we found that the kinetics of litter decomposition were similar once the effect of temperature had been removed, indicating no measurable effect of soil properties. A two-pool exponential decay model expressing undecomposed carbon simply as a function of thermal time accurately described kinetics of decomposition. (R-2 = 0.94; RMSE = 0.0508). Soil properties such as texture, cation exchange capacity, pH and moisture, although very different among sites, had minimal discernible influence on decomposition kinetics. Using this kinetic model under different climate change scenarios, we projected that the time required to decompose 50 of the litter (i.e. the labile fractions) would be reduced by 1-4 months, whereas time required to decompose 90 of the litter (including recalcitrant fractions) would be reduced by 1 year in cooler sites to as much as 2 years in warmer sites. These findings confirm quantitatively the sensitivity of litter decomposition to temperature increases and demonstrate how climate change may constrain future soil carbon storage, an effect apparently not influenced by soil properties.
机译:预计本世纪将发生广泛的全球变化,包括大气中二氧化碳浓度上升、气候变暖和生物多样性丧失;所有这些都将影响陆地生态系统过程,如植物凋落物分解。相反,植物凋落物分解的增加会对大气中的CO2水平、气候变暖和生物多样性产生潜在的碳循环反馈。但是,由于许多与土壤的化学、物理和生物特性以及气候和农业管理实践相关的相互作用因素,预测凋落物分解是困难的。我们将C-13标记的植物凋落物应用于加拿大农业地区3500公里横断面的十个地点的土壤中,并测量了其五年的分解情况。尽管土壤类型和气候条件差异很大,但我们发现,一旦消除了温度的影响,凋落物分解的动力学是相似的,表明土壤性质没有可测量的影响。一个双池指数衰变模型,将未分解的碳简单地表示为热时间的函数,准确地描述了分解动力学。(R-2 = 0.94;RMSE = 0.0508)。土壤性质,如质地、阳离子交换能力、pH值和水分,虽然在不同地点之间有很大差异,但对分解动力学的影响很小。在不同的气候变化情景下使用这种动力学模型,我们预计分解50%的凋落物(即不稳定部分)所需的时间将减少1-4个月,而分解90%的凋落物(包括顽固部分)所需的时间将在较冷的地方减少1年,在较温暖的地方将减少2年。这些发现定量证实了凋落物分解对温度升高的敏感性,并证明了气候变化如何限制未来的土壤碳储存,这种影响显然不受土壤特性的影响。

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