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利用欧洲长期生态研究站点观测数据对土壤 C、N 和 pH 对空气污染和气候变化的响应进行建模研究。

Modelling study of soil C, N and pH response to air pollution and climate change using European LTER site observations.

机构信息

Finnish Environment Institute (SYKE), Mechelininkatu 34a, FI-00251 Helsinki, Finland.

Environmental and Resource Studies, Trent University, Peterborough, Ontario K9J 7B8, Canada.

出版信息

Sci Total Environ. 2018 Nov 1;640-641:387-399. doi: 10.1016/j.scitotenv.2018.05.299. Epub 2018 May 31.

Abstract

Current climate warming is expected to continue in coming decades, whereas high N deposition may stabilize, in contrast to the clear decrease in S deposition. These pressures have distinctive regional patterns and their resulting impact on soil conditions is modified by local site characteristics. We have applied the VSD+ soil dynamic model to study impacts of deposition and climate change on soil properties, using MetHyd and GrowUp as pre-processors to provide input to VSD+. The single-layer soil model VSD+ accounts for processes of organic C and N turnover, as well as charge and mass balances of elements, cation exchange and base cation weathering. We calibrated VSD+ at 26 ecosystem study sites throughout Europe using observed conditions, and simulated key soil properties: soil solution pH (pH), soil base saturation (BS) and soil organic carbon and nitrogen ratio (C:N) under projected deposition of N and S, and climate warming until 2100. The sites are forested, located in the Mediterranean, forested alpine, Atlantic, continental and boreal regions. They represent the long-term ecological research (LTER) Europe network, including sites of the ICP Forests and ICP Integrated Monitoring (IM) programmes under the UNECE Convention on Long-range Transboundary Air Pollution (LRTAP), providing high quality long-term data on ecosystem response. Simulated future soil conditions improved under projected decrease in deposition and current climate conditions: higher pH, BS and C:N at 21, 16 and 12 of the sites, respectively. When climate change was included in the scenario analysis, the variability of the results increased. Climate warming resulted in higher simulated pH in most cases, and higher BS and C:N in roughly half of the cases. Especially the increase in C:N was more marked with climate warming. The study illustrates the value of LTER sites for applying models to predict soil responses to multiple environmental changes.

摘要

当前,预计未来几十年气候变暖仍将持续,而高氮沉积量可能会稳定下来,与之相反的是,硫沉积量则明显减少。这些压力具有独特的区域模式,其对土壤状况的影响因当地地点特征而有所不同。我们应用 VSD+土壤动态模型研究了沉积和气候变化对土壤性质的影响,使用 MetHyd 和 GrowUp 作为预处理程序,为 VSD+提供输入。单层土壤模型 VSD+可以模拟有机 C 和 N 转化过程,以及元素的电荷和质量平衡、阳离子交换和碱金属风化等过程。我们使用观测到的条件在欧洲 26 个生态系统研究点对 VSD+进行了校准,并模拟了关键土壤特性:土壤溶液 pH(pH)、土壤基础饱和度(BS)以及在预测的 N 和 S 沉积和气候变暖的情况下的土壤有机碳和氮比(C:N),直至 2100 年。这些地点是森林、地中海、森林高山、大西洋、大陆和北方地区,代表了欧洲的长期生态研究(LTER)网络,包括欧洲经委会《远距离越境空气污染公约》(LRTAP)下的国际比较方案森林和综合监测(IM)方案的站点,这些站点提供了有关生态系统响应的高质量长期数据。在预测的沉积减少和当前气候条件下,模拟的未来土壤条件有所改善:21 个站点中分别有 16 个和 12 个站点的 pH、BS 和 C:N 更高。当在情景分析中纳入气候变化时,结果的可变性增加。在大多数情况下,气候变暖导致模拟的 pH 升高,在大约一半的情况下,BS 和 C:N 升高。特别是随着气候变暖,C:N 的增加更为明显。该研究说明了 LTER 站点对于应用模型来预测土壤对多种环境变化的响应的价值。

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