Changes of nutrients and microbial communities in recovery process of abandoned rare earth tailings

IF 5.2 2区 农林科学 Q1 SOIL SCIENCE
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Abstract

Rare earth element (REE) mining has wrought severe ecosystem destruction, particularly in the loss of carbon (C), nitrogen (N), and phosphorus (P). Furthermore, its effects on nutrient recovery characteristics and associated microbial abundance are still poorly understood. In this study, an investigation was conducted to determine C, N, and P recovery patterns and microbial communities in abandoned REE mining tailings with different abandoned durations of 1.5 (1.5-Y), 7 (7-Y), 10 (10-Y), and 14 (14-Y) years and at an unmined site (the control group) in Jiangxi Province, China. Longitudinal tailing delamination at each site was investigated in 0–15 (layer 1) and 15–30 (layer 2) cm tailing layers. During the abandoned duration of REE tailings, C and P in layer 1 continued to recover from 1.62 to 8.51 g kg-1 and from 0.71 to 1.94 g kg-1, respectively; N losses of 0.60 and 0.22 g kg-1 occurred at the 1.5-Y and 10-Y sites, while N in layer 1 slightly increased at the 14-Y site. Mesorhizobium, Methylosinus, Bradyrhizobium, Pseudomonas, and Azospirillum were dominant bacteria at the 14-Y site and in the control. The relative abundances of N-fixing bacteria Mesorhizobium (32.94%), Sinorhizobium (0.24%), Frankia (0.71%), and Burkholderia (2.38%) at the 14-Y site were 1.33–3.97 times those in the control (24.19%, 0.18%, 0.32% and 0.60%, respectively), which was helpful for tailing N recovery. At the 14-Y site, Tylospora (50.24%), Luellia (11.02%), Tomentella (6.94%), and Chaetomium (4.34%) were the dominant fungal genera, while Tylospora (56.93%), Suillus (11.45%), and Penicillium (6.78%) predominated in the control. The relative abundance of the P-dissolving fungus Aspergillus at the 14-Y site (0.42%) was 4.2 times that in the control (0.1%), which may lead to the improved tailing P solubility. At the 14-Y site, woody plants such as Pinus massoniana and native pioneering herbs and ferns such as Dicranopteris dichotoma and Nephrolepis auriculata probably invaded from adjacent areas. This study unraveled the natural restoration of plant and microbial communities along with soil nutrient changes in abandoned REE tailings, thus providing a novel insight into ecological recovery and restoration after mining.

废弃稀土尾矿回收过程中养分和微生物群落的变化
稀土元素(REE)开采造成了严重的生态系统破坏,尤其是碳(C)、氮(N)和磷(P)的损失。此外,人们对其对营养恢复特征和相关微生物丰度的影响还知之甚少。本研究调查了中国江西省废弃的稀土金属采矿尾矿(废弃时间分别为 1.5 年、7 年、10 年和 14 年)以及未采矿点(对照组)的碳、氮、磷恢复模式和微生物群落。调查了每个矿址 0-15 厘米(第 1 层)和 15-30 厘米(第 2 层)尾矿层的纵向尾矿分层情况。在稀土尾矿弃置期间,第 1 层中的碳和磷分别从 1.62 克/千克持续恢复到 8.51 克/千克,从 0.71 克/千克恢复到 1.94 克/千克;1.5 年和 10 年矿点的氮损失分别为 0.60 克/千克和 0.22 克/千克,而 14 年矿点第 1 层中的氮略有增加。中生孢子菌、甲基酵母菌、子囊孢子菌、假单胞菌和氮气酵母菌是 14 Y 处和对照组的优势菌。在 14-Y 地块,固氮菌中生孢子球菌(32.94%)、单胞菌(0.24%)、法兰克菌(0.71%)和伯克霍尔德菌(2.38%)的相对丰度是对照的 1.33-3.97 倍(分别为 24.19%、0.18%、0.32% 和 0.60%),这有助于尾部氮的恢复。在 14-Y 地块,主要真菌属为 Tylospora(50.24%)、Luellia(11.02%)、Tomentella(6.94%)和 Chaetomium(4.34%),而对照组主要为 Tylospora(56.93%)、Suillus(11.45%)和 Penicillium(6.78%)。在 14-Y 地段,溶解 P 的真菌曲霉的相对丰度(0.42%)是对照组(0.1%)的 4.2 倍,这可能是尾矿 P 溶解性提高的原因。在 14-Y 地段,木本植物(如 Pinus massoniana)和本地先锋草本植物及蕨类植物(如 Dicranopteris dichotoma 和 Nephrolepis auriculata)可能从邻近地区入侵。这项研究揭示了废弃的稀土金属尾矿中植物和微生物群落的自然恢复以及土壤养分的变化,从而为采矿后的生态恢复和复原提供了新的视角。
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来源期刊
Pedosphere
Pedosphere 环境科学-土壤科学
CiteScore
11.70
自引率
1.80%
发文量
147
审稿时长
5.0 months
期刊介绍: PEDOSPHERE—a peer-reviewed international journal published bimonthly in English—welcomes submissions from scientists around the world under a broad scope of topics relevant to timely, high quality original research findings, especially up-to-date achievements and advances in the entire field of soil science studies dealing with environmental science, ecology, agriculture, bioscience, geoscience, forestry, etc. It publishes mainly original research articles as well as some reviews, mini reviews, short communications and special issues.
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