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Effects of experimental nitrogen deposition on peatland carbon pools and fluxes: a modelling analysis

机译:实验氮沉降对泥炭地碳库和通量的影响:模型分析

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Nitrogen (N) pollution of peatlands alters their carbon (C) balances, yetlong-term effects and controls are poorly understood. We applied the modelPEATBOG to explore impacts of long-term nitrogen (N) fertilization on Ccycling in an ombrotrophic bog. Simulations of summer gross ecosystemproduction (GEP), ecosystem respiration (ER) and net ecosystem exchange(NEE) were evaluated against 8 years of observations and extrapolated for 80 years to identify potential effects of N fertilization and factorsinfluencing model behaviour. The model successfully simulated moss declineand raised GEP, ER and NEE on fertilized plots. GEP was systematicallyoverestimated in the model compared to the field data due to factors thatcan be related to differences in vegetation distribution (e.g. shrubs vs.graminoid vegetation) and to high tolerance of vascular plants to Ndeposition in the model. Model performance regarding the 8-year response ofGEP and NEE to N input was improved by introducing an N content thresholdshifting the response of photosynthetic capacity (GEPmax) to N contentin shrubs and graminoids from positive to negative at high N contents. Suchchanges also eliminated the competitive advantages of vascular species andled to resilience of mosses in the long-term. Regardless of the largechanges of C fluxes over the short-term, the simulated GEP, ER and NEE after80 years depended on whether a graminoid- or shrub-dominated system evolved.When the peatland remained shrub–Sphagnum-dominated, it shifted to a C source afteronly 10 years of fertilization at 6.4 g N m?2 yr?1, whereas thiswas not the case when it became graminoid-dominated. The modelling resultsthus highlight the importance of ecosystem adaptation and reaction of plantfunctional types to N deposition, when predicting the future C balance ofN-polluted cool temperate bogs.
机译:泥炭地的氮(N)污染改变了它们的碳(C)平衡,但是人们对其长期影响和控制知之甚少。我们应用了模型PEATBOG来探索长期营养施肥对混养沼泽中Ccycling的影响。对照8年的观测值对夏季生态系统总产值(GEP),生态系统呼吸(ER)和净生态系统交换(NEE)进行了模拟,并推断了80年,以确定氮肥的潜在影响和影响模型行为的因素。该模型成功模拟了青苔的下降并提高了施肥区的GEP,ER和NEE。由于可能与植被分布差异有关的因素(例如灌木与草状植被)以及模型中维管植物对N沉积的高度耐受性,与实地数据相比,GEP在模型中被系统高估了。通过引入N含量阈值,将灌木和类粒动物的光合作用能力(GEP max )对N含量的响应从正向高转变为负,改善了GEP和NEE对N输入的8年响应的模型性能。 N个内容。这种变化还消除了血管物种的竞争优势,并长期导致苔藓的复原力。不管短期内C通量的变化如何,80年后的模拟GEP,ER和NEE都取决于是否以粒状或灌木为主的系统演化。当泥炭地保持灌木状-水藓-在仅受精10年后,在6.4 g N m ?2 yr ?1 的作用下,它转变为C源,而当它成为类粉质体时则不是这样。当预测未来氮污染的凉爽温带沼泽的碳平衡时,模拟结果突出了生态系统适应和植物功能类型对氮沉降的反应的重要性。

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