首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Seasonal responses of soil respiration to elevated CO2 and N addition in young subtropical forest ecosystems in southern China
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Seasonal responses of soil respiration to elevated CO2 and N addition in young subtropical forest ecosystems in southern China

机译:中国南方亚热带森林生态系统中土壤呼吸对CO 2和N添加量升高的季节性响应

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Atmospheric carbon dioxide (CO2) concentration and nitrogen (N) deposition may interactively impact soil respiration in terrestrial ecosystems. However, the effects of elevated CO2 and N deposition on soil respiration are not fully understood especially in subtropical forest ecosystems in southern China where ambient N deposition is high. In this study, we investigated the seasonal responses of soil respiration to elevated CO2 and N addition in young subtropical forest ecosystems in southern China using open-top chambers. Two CO2 treatment levels (i.e., ambient CO2 and 700 fimol mol~(-1)) and two N levels (i.e., ambient and 100 kg N ha~(-1) yr~(-1)) were considered. Forty-eight 1 -2 years old seedlings (eight seedlings per each of 6 species) were planted in each chamber. In the wet season, soil respiration significantly enhanced under elevated CO2 and N addition with no interactive effect. There was not significant relationship between treatment-enhanced soil respiration and soil moisture in the wet season, suggesting that increases in soil respiration resulted in large part from treatment-induced increases in tree growth and C inputs. In the dry season, soil respiration significantly enhanced under elevated CO2, but did not significantly change under N addition. The N-induced change in soil respiration negatively corrected with soil moisture in the dry season, indicating that decrease in soil moisture under N addition, together with increase in tree growth interactively resulted in negligible net change in soil respiration. Our results highlighted the seasonal importance of environmental controls under elevated CO2 and N deposition in the assessment of soil C sequestration potential in subtropical forest ecosystems in southern China.
机译:大气中二氧化碳(CO2)的浓度和氮(N)的沉积可能交互影响陆地生态系统中的土壤呼吸。然而,二氧化碳和氮沉降增加对土壤呼吸的影响还没有被完全理解,特别是在中国南部的亚热带森林生态系统中,氮的沉积很高。在这项研究中,我们使用开放式室调查了中国南方亚热带森林生态系统中土壤呼吸对CO 2和N添加量增加的季节响应。考虑了两个CO2处理水平(即环境CO2和700 fimol mol〜(-1))和两个N水平(即环境和100 kg N ha〜(-1)yr〜(-1))。在每个室中种植了48个1 -2岁的幼苗(每6个物种中的8个幼苗)。在雨季,在增加的CO2和N添加下,土壤呼吸作用显着增强,而没有交互作用。在雨季,处理后的土壤呼吸与土壤水分之间没有显着关系,这表明土壤呼吸的增加很大程度上是由于处理引起的树木生长和碳输入的增加。在干旱季节,CO2浓度升高,土壤呼吸作用显着增强,但氮素添加条件下土壤呼吸作用没有明显变化。在干旱季节,N引起的土壤呼吸变化被土壤水分负校正,这表明在添加N的情况下土壤水分减少以及树木生长的相互作用导致土壤呼吸的净变化可忽略不计。我们的结果强调了在评估中国南方亚热带森林生态系统中土壤碳固存潜力的过程中,在较高的CO2和N沉积下环境控制的季节性重要性。

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