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Bulk deposition of base cationic nutrients in China's forests: Annual rates and spatial characteristics

机译:中国森林中基本阳离子养分的大量沉积:年速率和空间特征

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Base cations, such as potassium (K+), calcium (Ca2+) and magnesium (Mg2+), are essential nutrients for plant growth and their atmospheric inputs can buffer the effect of acid deposition by nitrogen (N) and sulphur (S) compounds. However, the spatial variation in atmospheric deposition of these base cationic nutrients is less understood compared with N and S deposition. By synthesizing bulk deposition data for K+, Ca2+ and Mg2+, we assessed their annual rates and spatial characteristics at 34 forested sites across China. Our synthesis showed relatively high levels of bulk deposition of base cationic nutrients in China's forests, being an order of magnitude higher than in the USA and Europe. On average, K+, Cahigher than in the USA and Europe. On average, K+, Cahigher than in the USA and Europe. On average, K+, Ca2+ and mg(2+) accounted for 13%, 72% and 15% of the and mg(2+) accounted for 13%, 72% and 15% of the and mg(2+) accounted for 13%, 72% and 15% of the bulk deposition of base cationic nutrients, respectively. Surprisingly, base cation deposition was lower at sites near semi-arid regions compared with sites in eastern and southern China, which were far from semi-arid regions. Moreover, elevated base cation deposition was associated with urban hotspots, exhibiting a significant power-law increase with closer distance to the nearest large cities. We estimated that on average base cationic nutrients neutralized a significant proportion (76%) of the potential acid load due to acid deposition. Our findings suggest that in China there is considerable anthropogenic alteration of the regional cycling of base cationic nutrients, which plays an important role in counteracting the risk of soil acidification and base cation depletion in forest ecosystems, especially in the southern regions.
机译:碱性阳离子,例如钾(K +),钙(Ca2 +)和镁(Mg2 +),是植物生长必不可少的营养素,其大气输入可以缓冲氮(N)和硫(S)化合物对酸沉积的影响。但是,与N和S沉积相比,这些基本阳离子养分在大气沉积中的空间变化了解得很少。通过综合K +,Ca2 +和Mg2 +的大量沉积数据,我们评估了中国34个林区的年增长率和空间特征。我们的合成表明,中国森林中基础阳离子养分的大量堆积水平,比美国和欧洲高一个数量级。平均而言,K +比美国和欧洲高。平均而言,K +比美国和欧洲高。平均而言,K +,Ca2 +和mg(2+)占的13%,72%和15%,而mg(2+)占的13%,72%和15%,mg(2+)占分别占基础阳离子养分总体沉积的13%,72%和15%。出乎意料的是,与中国东部和南部远离半干旱地区的地区相比,在半干旱地区附近的地区的阳离子沉积量更低。此外,升高的基础阳离子沉积与城市热点有关,随着距最近大城市的距离越来越近,功率定律显着增加。我们估计,由于酸沉积,平均而言,碱性阳离子养分中和了潜在酸负荷的很大一部分(76%)。我们的发现表明,在中国,基础阳离子养分的区域循环发生了人为变化,这在抵御森林生态系统(尤其是南部地区)土壤酸化和基础阳离子枯竭的风险方面发挥着重要作用。

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