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过量的硫和铁元素导致中国贵州废弃煤矸石土壤和植被发生变化。

Excess sulfur and Fe elements drive changes in soil and vegetation at abandoned coal gangues, Guizhou China.

机构信息

State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China.

出版信息

Sci Rep. 2020 Jun 26;10(1):10456. doi: 10.1038/s41598-020-67311-z.

Abstract

Coal gangue piles accumulate outside mines and can persist for years, negatively impacting the regional environment. To determine the main cause of soil pollution at coal gangues, several coal gangues in Guizhou Province, China that had undergone natural recovery via native plants for 8 years were investigated in summer 2019. Three plots (2 m × 2 m) from the coal gangue area were selected for the treatment (GP). Control plots that were 100 m away from GP were also investigated in contrast (CK-near). In addition, plots from forest, farmland and lake land that were far from GP and largely undisturbed were also investigated as more extreme contrasts (CK-far). A series of soil indicators that can be affected by coal-gangue, such as heavy metals (Mn, Cr, Cd, Ni, Zn, Cu, Pb), As, pH, cation exchange capacity (CEC), sulfur (S) and iron (Fe), were tested for in the plots. Plant species, coverage and height were also analyzed to uncover biodiversity and dominant species information. The results suggested that coal gangue significantly influences soil S, pH and plant species after 8 years of natural recovery. The CK-far plots contained relatively low soil sulfur content, normal pH (close to 7) and abundant plant biodiversity. Generally, pH related positively with both the Patrick (R = 0.79, n = 22, p < 0.001) and Shannon indices (R = 0.67, n = 22, p < 0.001); the soil S related negatively with both the Patrick (R = 0.85, n = 22, p < 0.001) and Shannon indices (R = - 0.79, n = 22, p < 0.001). S content was highest (S = 1.0%) in GP plots, was lower in CK-near plots (S = 0.3%) and was the lowest of all in the plots distant from the coal mine (S = 0.1%, CK-far). S content was negatively correlated with pH. Soil pH decreased significantly, from 7.0 in CK-far, to 5.9 in CK-near, to 4.2 in GP. Soil Fe was 3.4 times higher in GP and CK-near than in CK-far. The excess sulfur and Fe elements and the acidified soil drove changes in soil and vegetation in the coal gangue areas. After 8 years of natural recovery, only a few plants, like Miscanthus floridulus, were able to live near the coal gangue in the area where the soil was still acidic and high in S and Fe.

摘要

矸石山在矿区外堆积,可存在多年,对区域环境造成负面影响。为了确定矸石山土壤污染的主要原因,对中国贵州省经过 8 年自然恢复的原生植物的几个矸石山进行了研究。2019 年夏季,从矸石山地区选择了三个试验区(2 m×2 m)(GP)。还对距离 GP 约 100 m 的对照试验区(CK-近)进行了调查。此外,还对远离 GP 且基本未受干扰的林地、农田和湖滨地的试验区(CK-远)进行了调查,作为更为极端的对照。对试验区的一系列可能受矸石影响的土壤指标进行了测试,如重金属(Mn、Cr、Cd、Ni、Zn、Cu、Pb)、As、pH 值、阳离子交换量(CEC)、硫(S)和铁(Fe)。还分析了植物物种、覆盖率和高度,以揭示生物多样性和优势物种信息。结果表明,矸石山在自然恢复 8 年后对土壤 S、pH 值和植物物种有显著影响。CK-远试验区的土壤硫含量相对较低,pH 值接近 7,植物生物多样性丰富。一般来说,pH 值与 Patrick 指数(R=0.79,n=22,p<0.001)和 Shannon 指数(R=0.67,n=22,p<0.001)均呈正相关;土壤 S 与 Patrick 指数(R=0.85,n=22,p<0.001)和 Shannon 指数(R=−0.79,n=22,p<0.001)均呈负相关。GP 试验区的 S 含量最高(S=1.0%),CK-近试验区的 S 含量较低(S=0.3%),远离矿区的 CK-远试验区的 S 含量最低(S=0.1%)。S 含量与 pH 值呈负相关。土壤 pH 值显著下降,从 CK-远的 7.0 降至 CK-近的 5.9,再降至 GP 的 4.2。GP 和 CK-近的土壤 Fe 含量分别是 CK-远的 3.4 倍和 2.5 倍。过多的硫和 Fe 元素以及酸化的土壤导致了矸石山地区土壤和植被的变化。经过 8 年的自然恢复,只有少数植物,如芒草,能够在矸石山附近的酸性土壤中生长,该土壤中 S 和 Fe 含量较高。

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