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Effects of Nitrogen Deposition on CH_4 Uptake and CO_2 Emission from temperate forests in Northeastern China

机译:氮沉积对中国东北地区温带森林CH_4摄取和CO_2排放的影响

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Little is known about how N deposition affects greenhouse gas balances in different temporal patterns (daytime and nighttime), and few studies have been conducted to quantify the effects of N deposition on soil CH_4 uptake and CO_2 emission in a typical temperate forests. To investigate the effects of N deposition on soil CH_4 uptake and CO_2 emission, simulated N deposition experiment was initiated in temperate forests in Northeastern China in May 2011. In this study, NH_4NO_3 fertilizer was applied throughout the growing season at four N treatment levels (three replicates): control (CK), no added N; low-N (T_L), 5 g N m~(-2)·yr~(-1); medium-N (T_M), 10 g N m~(-2)·yr~(-1); and high-N (T_H), 15 g N m~(-2)·yr~(-1). Diurnal soil CH_4 uptake and CO_2 emission rates were observed in August 2014 using Greenhouse Gas Analyzers. Our results showed that N deposition tended to restrict CH_4 uptake and significantly increased soil CO_2 emission (except in the T_H treatment). In addition, the CO_2 and CH_4 fluxes in daytime and nighttime were significantly different. These results indicate that N deposition controls the CH_4 uptake and suggest that alterations of the N cycle due to N deposition may convert sequestered C in forest soils into a C source. However, this paper is also to promote a better understanding of the impact of N deposition on soil C fluxes under the different temporal patterns.
机译:众所周知,N沉积如何影响不同的时间模式(白天和夜间),并且已经进行了很少的研究,以量化N沉积对典型的温带森林中的土壤CH_4摄取和CO_2排放的影响。为了探讨N沉积对土壤CH_4摄取和CO_2排放的影响,2011年5月在中国东北部的温带森林中启动了模拟的N沉积实验。在这项研究中,在整个生长季节的治疗水平期间应用NH_4NO_3肥料(三个复制):控制(CK),没有添加n; Low-N(T_L),5 G N M〜(-2)·Yr〜(-1);中等-N(T_M),10g n m〜(-2)·Yr〜(-1);和高N(T_H),15g n m〜(-2)·Yr〜(-1)。利用温室气体分析仪于2014年8月观察到昼夜土壤CH_4摄取和CO_2排放率。我们的研究结果表明,N沉积倾向于限制CH_4摄取,显着增加土壤CO_2排放(T_H处理除外)。此外,白天和夜间的CO_2和CH_4助熔剂显着不同。这些结果表明,N沉积控制CH_4摄取并表明由于N沉积引起的N循环的改变可以将森林土壤中的螯合的C转化为C源。然而,本文还促进了在不同时间模式下更好地了解n沉积对土壤C通量的影响。

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