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Simulating ectomycorrhiza in boreal forests: implementing ectomycorrhizal fungi model MYCOFON in CoupModel (v5)

机译:模拟北方森林中的Eccycorrhiza:在CoupModel中实施Eccycorrohizal真菌模型Mycofon(V5)

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The symbiosis between plants and Ectomycorrhizal fungi (ECM) is shown to considerably influence the carbon (C) and nitrogen (N) fluxes between the soil, rhizosphere, and plants in boreal forest ecosystems. However, ECM are either neglected or presented as an implicit, undynamic term in most ecosystem models, which can potentially reduce the predictive power of models.In order to investigate the necessity of an explicit consideration of ECM in ecosystem models, we implement the previously developed MYCOFON model into a detailed process-based, soil–plant–atmosphere model, Coup-MYCOFON, which explicitly describes the C and N fluxes between ECM and roots. This new Coup-MYCOFON model approach (ECM explicit) is compared with two simpler model approaches: one containing ECM implicitly as a dynamic uptake of organic N considering the plant roots to represent the ECM (ECM implicit), and the other a static N approach in which plant growth is limited to a fixed N level (nonlim). Parameter uncertainties are quantified using Bayesian calibration in which the model outputs are constrained to current forest growth and soil C?∕?N ratio for four forest sites along a climate and N deposition gradient in Sweden and simulated over a 100-year period.The nonlim approach could not describe the soil C?∕?N ratio due to large overestimation of soil N sequestration but simulate the forest growth reasonably well. The ECM implicit and explicit approaches both describe the soil C?∕?N ratio well but slightly underestimate the forest growth. The implicit approach simulated lower litter production and soil respiration than the explicit approach. The ECM explicit Coup–MYCOFON model provides a more detailed description of internal ecosystem fluxes and feedbacks of C and N between plants, soil, and ECM. Our modeling highlights the need to incorporate ECM and organic N uptake into ecosystem models, and the nonlim approach is not recommended for future long-term soil C and N predictions. We also provide a key set of posterior fungal parameters that can be further investigated and evaluated in future ECM studies.
机译:植物和颈菌毒性真菌(ECM)之间的共生显着影响土壤,根际和北部森林生态系统中的碳(C)和氮气(N)助熔剂。然而,ECM在大多数生态系统模型中被忽略或被呈现为隐含的,无难以列出的术语,这可能会降低模型的预测力量。为了调查ECM在生态系统模型中明确考虑ECM的必要性,我们实施了先前开发的MyCofon模型进入了一种详细的基于过程,土壤 - 植物 - 大气模型,Coup-Mycofon,其明确描述了ECM和根部之间的C和N助熔剂。这种新的Coup-Mycofon模型方法(ECM显式)与两种更简单的模型方法进行比较:考虑到工厂根源以代表ECM(ECM隐式)的有机N,含有ECM的一个含有ECM作为有机的摄取,以及另一个静态N方法其中植物生长仅限于固定的n级(非目的)。使用贝叶斯校准量化参数不确定因素,其中模型输出受到当前森林生长和土壤C?/αn沿着瑞典的气候和N沉积梯度的四种森林网站的比例,并在100年期间模拟。非领域由于大于土壤n螯合,方法无法描述土壤c?/ηn/η的比例。合理良好地模拟森林生长。 ECM隐含和明确的方法都描述了土壤C?/η的比率良好,但略微低估了森林生长。隐含方法模拟落下的垃圾生产和土壤呼吸,而不是明确的方法。 ECM显式COUP-MYCOFON模型提供了植物,土壤和ECM之间的内部生态系统助熔剂和反馈的更详细描述。我们的建模突出了将ECM和有机N吸收将ECM和有机N带入生态系统模型的需要,并且不建议未来的长期土壤C和N预测。我们还提供了一组关键的后验证参数,可以在未来的ECM研究中进一步调查和评估。

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