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Nitrogen deposition interacts with climate in affecting production and decomposition rates in Sphagnum mosses

机译:氮沉积与气候相互作用,影响泥炭藓的产生和分解速率

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Increasing rates of atmospheric nitrogen (N) deposition may reduce growth and accelerate decomposition of Sphagnum mosses in bogs. Sphagnum growth and rates of Sphagnum litter decomposition may also vary because of climate change as both processes are controlled by climatic factors. The initial purpose of this study was to assess if growth and litter decomposition of hummock and lawn Sphagnum species varied with increasing N input in a factorial mid-term (2002-2005) experiment of N and phosphorus (P) addition, in a bog on the southern Alps of Italy. However, as the experimental period was characterized by an exceptional heat wave in summer 2003, we also explored the interacting effects of fertilization and strongly varying climate on growth and decomposition rates of Sphagnum. The heat wave implied strong dehydration of the upper Sphagnum layer even if precipitation in summer 2003 did not differ appreciably from the overall mean. Sphagnum production was somewhat depressed by high levels (3 g m(-2) yr(-1)) of N addition without concomitant addition of P presumably because of nutrient imbalance in the tissues, but production rates were much lower than the overall means in 2003, when no effect of nutrient addition could be observed. Adding N at high level also increased the potential decay of Sphagnum litter. Higher CO2 emission from N-fertilized litter was due to amelioration of litter chemistry showing lower C/N quotients in the N-fertilized treatments. Rates of CO2 emission from incubated litter also were more strongly affected by water content than by nutrient status, with practically no CO2 emission detected when litter was dry. We conclude that higher rates of atmospheric N availability input may depress Sphagnum growth because of P, and presumably potassium, (co-)limitation. Higher N availability is also expected to promote potential decay of Sphagnum litter by ameliorating litter chemistry. However, both effects are less pronounced if the growing Sphagnum apex and the underlying senescing tissues dry out.
机译:大气中氮(N)沉积速率的增加可能会减少生长并加速沼泽中泥炭藓的分解。由于气候变化,泥炭的生长和泥炭凋落物分解的速率也可能变化,因为这两个过程均受气候因素控制。这项研究的最初目的是评估在一个过渡期(2002-2005年)进行的氮和磷(P)添加的析因中期试验中,浮床和草坪水草物种的生长和凋落物分解是否随氮输入的增加而变化。意大利的南部阿尔卑斯山。但是,由于实验期的特征是2003年夏季出现了异常热浪,因此我们还探讨了施肥和气候变化对泥炭藓生长和分解速率的相互作用。即使2003年夏季的降水与总体平均值没有明显差异,热浪也暗示了泥炭上层的强烈脱水。高水平(3 gm(-2)yr(-1))的氮添加而没有同时添加P可能会降低泥炭藓的产量,这可能是因为组织中的营养失衡,但是生产率远低于2003年的总体平均值,当没有观察到营养添加的效果时。高水平添加氮也增加了泥炭凋落物的潜在衰减。氮肥处理后的垫料的二氧化碳排放量较高,是由于氮肥处理后垫料化学成分的降低,显示了较低的C / N值。孵化后的垫料产生的CO2排放率也受水分含量的影响大于受养分状况的影响,当垫料干燥时几乎没有检测到CO2排放。我们得出的结论是,由于P(大概是钾)的限制,大气氮素输入的较高比率可能会抑制泥炭藓的生长。通过改善凋落物化学特性,更高的氮利用率也有望促进泥炭草凋落物的潜在腐烂。但是,如果正在生长的泥炭顶和下层的衰老组织变干,则两种作用都不太明显。

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