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尽管自 2001 年以来已经控制了二氧化硫的排放,但硫沉降仍然导致了中国南方珠江三角洲的森林土壤酸化。

Sulfur deposition still contributes to forest soil acidification in the Pearl River Delta, South China, despite the control of sulfur dioxide emission since 2001.

机构信息

Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, 510650, China.

Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, 510650, China.

出版信息

Environ Sci Pollut Res Int. 2019 May;26(13):12928-12939. doi: 10.1007/s11356-019-04831-w. Epub 2019 Mar 20.

Abstract

Sulfur dioxide emissions have been regulated at a global scale; sulfur (S) deposition no longer contributes to soil acidification instead of an alleviation effect in temperate regions; however, it remains unclear whether S deposition still contributes to soil acidification in the tropics. The Pearl River Delta (PRD), South China, has been suffering serious soil acidification, but the contribution of S deposition was ignored because of the regulation of S emission since 2001. Here, we chose the evergreen broadleaf forests, which are the typical forest type at the regional scale in PRD to examine the contribution of S deposition and its characteristics in this acidification, based on an established urban-rural gradient in the range of 260 km. A substantial acidification was evidenced by the significant decline of soil pH from rural to urban sites, with mean pH values decreased by more than 0.60 U through the whole 40-cm depths. However, there was no significant difference in soil pH from 0-10 cm, 10-20 cm, and to 20-40 cm at each site (P > 0.05). Acid-neutralizing capacity (ANC) showed a similar trend to soil pH, with a significant decline along the urbanization gradient and no significant effect of soil depths. Soil sulfate (SO), as the most abundant species in ANC, contributed greatly to soil acidification for the whole 40-cm depth, as shown by the significant positive relationships between it with soil pH and base cations. Soils also exhibited the depletion of base cations with low base saturation (< 20%) and the release of Al and Fe. Our research demonstrated that the severe soil acidification in the PRD region has extended to the subsoil level (40-cm depth), and S deposition is still an important driver to this acidification. Therefore, both recovering the acidified soils and controlling the acidifying pollutants, especially S, are particularly difficult in southern China.

摘要

二氧化硫排放已在全球范围内得到了控制;在温带地区,硫(S)沉降不再导致土壤酸化,反而起到了缓解作用;然而,目前尚不清楚 S 沉降是否仍会导致热带地区土壤酸化。中国南方的珠江三角洲(PRD)一直遭受着严重的土壤酸化,但由于 2001 年以来对 S 排放的控制,S 沉降对土壤酸化的贡献被忽视了。在这里,我们选择了常绿阔叶林,这是 PRD 区域尺度上的典型森林类型,基于在 260km 范围内建立的城乡梯度,研究了 S 沉降及其在该酸化过程中的特征。从农村到城市,土壤 pH 值显著下降,证明了土壤发生了严重酸化,整个 40cm 深度的平均 pH 值下降了 0.60U 以上。然而,每个地点的 0-10cm、10-20cm 和 20-40cm 土层的土壤 pH 值没有显著差异(P > 0.05)。中和能力(ANC)与土壤 pH 呈相似趋势,随着城市化梯度的下降而显著下降,而土壤深度没有显著影响。土壤硫酸盐(SO)是 ANC 中最丰富的物质,对整个 40cm 深度的土壤酸化有很大贡献,这表现在它与土壤 pH 值和碱金属阳离子之间存在显著的正相关关系。土壤还表现出碱金属阳离子的消耗,碱饱和度低(<20%),以及 Al 和 Fe 的释放。我们的研究表明,PRD 地区严重的土壤酸化已经扩展到了亚土层(40cm 深度),S 沉降仍然是酸化的一个重要驱动因素。因此,在中国南方,恢复酸化土壤和控制酸化污染物,特别是 S,都是特别困难的。

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