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Effects of One-Year Simulated Nitrogen and Acid Deposition on Soil Respiration in a Subtropical Plantation in China

机译:一年模拟氮气和酸沉积对中国亚热带种植园土壤呼吸的影响

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Atmospheric nitrogen (N) and acid deposition have become global environmental issues and are likely to alter soil respiration ( R s ); the largest CO 2 source is from soil to the atmosphere. However, to date, much less attention has been focused on the interactive effects and underlying mechanisms of N and acid deposition on R s , especially for ecosystems that are simultaneously subjected to elevated levels of deposition of both N and acid. Here, to examine the effects of N addition, acid addition, and their interactions with R s , we conducted a two-way factorial N addition (control, CK; 60 kg N ha ?1 a ?1 , LN; 120 kg N ha ?1 a ?1 , HN) and acid addition (control, CK; pH 4.5, LA; pH 2.5, HA) field experiment in a subtropical plantation in China. Our results showed the following: (1) During the one-year observation period, the seasonal dynamics of R s presented a single peak curve model, which was closely related to the surface soil temperature. (2) The simulated N deposition and acid deposition significantly decreased the R s in the subtropical plantation. Compared to the CK plots, the LN and HN treatments reduced the annual mean values of R s by 41% and 56%, and the annual mean values of R s were inhibited by 26% and 31% in the LA and HA plots. The inhibition of N application on R s was stronger than that of the simulated acid deposition. (3) Significant interactions between N addition and acid addition on R s were detected, and R s was significantly inhibited under four co-addition treatments. (4) The underlying mechanism and main reason for the responses of R s to simulated N and acid deposition in this study might be the inhibition of soil microbial biomass and soil enzyme activity due to soil acidification under increased N and acid input.
机译:大气氮(n)和酸沉积已成为全球环境问题,可能会改变土壤呼吸(R s);最大的CO 2来源是从土壤到大气层。然而,迄今为止,重点关注N和酸沉积对R S的互动效果和潜在机制,特别是对于同时进行N和酸的沉积水平升高的生态系统。在这里,为了检查N添加的效果,酸加成及其与R S的相互作用,我们进行了双向因子N添加(对照,CK; 60 kg n Ha?1 a?1,ln; 120 kg n ha ?1 a?1,hn)和酸加(对照,ck; ph 4.5,la; ph 2.5,ha)野生目的地在中国的亚热带地区实验。我们的结果表明:(1)在一年的观察期间,R S的季节性动态呈现出单一峰曲线模型,与表面土壤温度密切相关。 (2)模拟的N沉积和酸沉积显着降低了亚热带种植园中的R S.与CK图相比,LN和HN治疗减少了41%和56%的年平均值,R S的年平均值抑制了La和Ha图中的26%和31%。 N施加在R S上的抑制比模拟酸沉积的抑制力强。 (3)检测N添加和酸加入之间的显着相互作用,并在四个助涂处理下显着抑制R S. (4)本研究中R s对模拟N和酸沉积反应的潜在机制和主要原因可能是由于N和酸输入的土壤酸化而抑制土壤微生物生物量和土壤酶活性。

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