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Short-term simulated nitrogen deposition increases carbon sequestration in a Pleioblastus amarus plantation

机译:短期模拟氮沉降增加了P苦竹人工林的固碳

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In order to understand the influence of nitrogen (N) deposition on the key processes relevant to the carbon (C) balance in a bamboo plantation, a two-year field experiment involving the simulated deposition of N in a Pleioblastus amarus plantation was conducted in the rainy region of SW China. Four levels of N treatments: control (no N added), low-N (50 kg N ha−1 year−1), medium-N (150 kg N ha−1 year−1), and high-N (300 kg N ha−1 year−1) were set in the present study. The results showed that soil respiration followed a clear seasonal pattern, with the maximum rates in mid-summer and the minimum in late winter. The annual cumulative soil respiration was 585 ± 43 g CO2-C m−2 year−1 in the control plots. Simulated N deposition significantly increased the mean annual soil respiration rate, fine root biomass, soil microbial biomass C (MBC), and N concentration in fine roots and fresh leaf litter. Soil respirations exhibited a positive exponential relationship with soil temperature, and a linear relationship with MBC. The net primary production (NPP) ranged from 10.95 to 15.01 Mg C ha−1 year−1 and was higher than the annual soil respiration (5.85 to 7.62 Mg C ha−1 year−1) in all treatments. Simulated N deposition increased the net ecosystem production (NEP), and there was a significant difference between the control and high N treatment NEP, whereas, the difference of NEP among control, low-N, and medium-N was not significant. Results suggest that N controlled the primary production in this bamboo plantation ecosystem. Simulated N deposition increased the C sequestration of the P. amarus plantation ecosystem through increasing the plant C pool, though CO2 emission through soil respiration was also enhanced.
机译:为了了解氮(N)沉积对竹人工林中与碳(C)平衡相关的关键过程的影响,进行了为期两年的田间试验,其中包括在苦竹中人工模拟氮的沉积。中国西南多雨地区。 N处理的四个级别:对照(不添加N),低氮(50 kg N ha -1 年 -1 ),中N(150 kg N ha -1 年 -1 )和高氮(300千克N ha -1 年 -1 )被设置在本研究中。结果表明,土壤呼吸遵循明显的季节性模式,夏中最高,夏末最低。对照区土壤年累积呼吸量为585±43 g CO 2 -C m -2 年 -1 。模拟的氮沉降显着提高了年均土壤呼吸速率,细根生物量,土壤微生物生物量碳(MBC)以及细根和鲜叶凋落物中的氮浓度。土壤呼吸与土壤温度呈正指数关系,与MBC呈线性关系。净初级生产力(NPP)在10.95至15.01 Mg C ha -1 年 -1 范围内,并且高于年度土壤​​呼吸(5.85至7.62 Mg C ha <在所有治疗中均使用sup> -1 year -1 )。模拟的氮沉降增加了生态系统的净产量(NEP),而对照和高氮处理的NEP之间存在显着差异,而对照,低氮和中等氮之间的NEP差异不显着。结果表明,氮控制了这个竹林生态系统的初级生产。模拟的氮沉降通过增加植物的碳库增加了红a人工林生态系统的碳固存,尽管通过土壤呼吸增加了CO 2 的排放。

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