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Simultaneous Estimation of Actual Litter Enzymatic Catalysis and Respiration Rates with a Simple Model of C Dynamics in Sphagnum-Dominated Peatlands

机译:利用泥炭占主导地位的泥炭地碳动力学简单模型同时估算实际的凋落物酶催化和呼吸速率

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摘要

C dynamics in soils plays an important role in the interactions between climate and terrestrial ecosystems. Given the importance of the soil C pool in future climate scenarios, accurate models that can then be integrated into global models are required. On the one hand, models of soil C dynamics can be very simplistic in that only solid organic matter (OM) is taken into account with constant rates. Such models can miss important features of soil C dynamics such as enzymatic activity and CO2 production. On the other hand, some models are too complicated to be experimentally calibrated, tested, and widely used. We propose a model of soil C dynamics that (i) integrates all C fluxes from the solid to the gaseous form, and (ii) can be easily implemented experimentally. Because peatlands are important C stores that are experiencing vegetation changes, the model was tested on experimental results obtained with peatland litter: Sphagnum cuspidatum (autochtonous vegetation), Molinia caerulea, and Betula spp. (both invasive species). Our model was able to accurately describe the early stages of C dynamics in litter especially when only one pool of OM was used and when catalysis and respiration rates were allowed to decrease with time. Our model is efficient in assessing the entire actual catalysis rate. This is a notable achievement as usually, enzyme activity is measured on specific enzymes in conditions often far from actual ones. Our model appeared to be sufficiently robust and worthy of development, keeping in mind that it should remain experimentally testable.
机译:土壤中的碳动力学在气候与陆地生态系统之间的相互作用中起着重要作用。考虑到土壤碳库在未来气候情景中的重要性,需要可以将其整合到全球模型中的精确模型。一方面,土壤碳动力学模型可以非常简单,因为仅以恒定速率考虑固体有机物(OM)。这种模型可能会遗漏土壤C动态的重要特征,例如酶活性和CO2产生。另一方面,某些模型过于复杂,无法通过实验进行校准,测试和广泛使用。我们提出了一种土壤碳动力学模型,该模型(i)整合了从固体到气态的所有碳通量,并且(ii)可以通过实验轻松实现。由于泥炭地是经历植被变化的重要C储量,因此对该模型进行了测试,使用泥炭垫料(虎杖(自生植物),蓝藻和桦木)获得了实验结果。 (均为入侵物种)。我们的模型能够准确地描述垃圾中C动力学的早期阶段,尤其是仅使用一个OM池时,以及允许催化和呼吸速率随时间降低时。我们的模型可以有效地评估整个实际的催化速率。通常,这是一个显着的成就,酶活性是在通常与实际条件相差很远的条件下对特定酶进行测量的。我们的模型似乎足够健壮,值得开发,但要记住它应该保持实验可测试性。

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