Fe(II)催化重结晶促使磷和铝从网纹石中释放出来

IF 10.8 1区 环境科学与生态学 Q1 ENGINEERING, ENVIRONMENTAL
环境科学与技术 Pub Date : 2024-10-22 Epub Date: 2024-10-10 DOI:10.1021/acs.est.4c03574
Niloofar Karimian, Mark I Pownceby, Edward D Burton, Martin Wells, Andrew J Frierdich
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引用次数: 0

摘要

透辉石通常含有磷(P)和铝(Al)等杂质,这些杂质通过直接置换或与纳米晶相共沉淀的方式融入透辉石的结构中。了解促使磷和铝从网纹石中释放出来的过程对于铁矿石行业以及管理环境中的营养物质和污染物行为至关重要。本研究调查了铁(II)催化重结晶对钾和铝从鹅铁矿中释放的影响。我们评估了在无氧条件下,在中性 pH 值和室温条件下,用富含 57Fe 的 Fe(II)aq 处理 30 天后,铝和磷重结晶的鹅绿泥石悬浮液中 P 和 Al 的可溶性和可萃取性。加入 Fe(II)aq 后,鹅绿泥石的主要初始合成相(即含 P 和 Al 较低的相)发生了重结晶,而含 P 和/或 Al 较高的起始材料则发生了转变,这些起始材料实际上是鹅绿泥石与少量鳞片闪锌矿和铁氧体的混合物。我们的研究结果表明,铁(II)催化的矿物和结构演变导致了整个晶体结构、矿物表面和水溶液中 P 的重新分配,其次是 Al 的重新分配。与 Fe(II)aq 反应 30 天后,我们分别从纯 P、低 P、中 P 和高 P + Al 的鹅绿泥石中提取了约 80%、68.8%、73.9% 和 83.2%的 P。此外,我们还观察到,低、中、高 P + Al 磁铁矿的总铝去除率分别约为 17%、27% 和 25%。结果表明,与不含铁(II)的对照组相比,在室温下用铁(II)处理纯磷和磷+铝鹅卵石,然后用 1 M NaOH 进行 24 小时萃取,可显著提高磷和铝的总体萃取率,包括水萃取和表面吸附萃取。这些发现加深了我们对鹅铁矿再结晶过程和杂质置换的理解,为开发新的环境友好型方法在较低温度下从鹅铁矿中萃取磷和其他杂质提供了前景广阔的途径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Fe(II)-Catalyzed Recrystallization Drives Phosphorus and Aluminum Release from Goethite.

Fe(II)-Catalyzed Recrystallization Drives Phosphorus and Aluminum Release from Goethite.

Goethite often harbors impurities, such as phosphorus (P) and aluminum (Al), which are incorporated into its structure through direct substitution or coprecipitation with nanocrystalline phases. Understanding the processes that drive the release of P and Al from goethite is of paramount importance for the iron ore industry and for managing nutrient and pollutant behavior in the environment. This study investigates the impact of Fe(II)-catalyzed recrystallization on the release of P and Al from goethite. We evaluated the solubility and extractability of P and Al in suspensions of Al- and P-coprecipitated goethite, treated with 57Fe-enriched Fe(II)aq under oxygen-free conditions for 30 days at neutral pH and room temperatures. The addition of Fe(II)aq induced the recrystallization of goethite dominant initial synthetic phases (i.e., low P- and Al-containing phases) and the transformation of higher P- and/or Al-bearing starting material that was actually a mixture of goethite and minor amounts of lepidocrocite and feroxyhyte. Our results reveal that Fe(II)-catalyzed mineral and structural evolution led to the repartitioning of P and, to a lesser extent, Al throughout the crystal structure, mineral surface, and aqueous solution. Following a 30 day reaction with Fe(II)aq, we extracted approximately 80, 68.8, 73.9, and 83.2% of P from P-only, low, medium, and high P + Al goethite, respectively. Additionally, we observed total Al removals of approximately 17, 27, and 25% from low, medium, and high P + Al goethite, respectively. The results demonstrate that treating both P-only and P + Al goethite with Fe(II) at room temperature, followed by a 24 h extraction using 1 M NaOH, significantly enhances the overall extractability of P and Al, including both aqueous and surface-adsorbed fractions, compared to Fe(II)-free controls. These findings advance our understanding of the recrystallization process and impurity substitution in goethite, offering promising avenues for developing new environmentally friendly methods to extract P and other impurities from goethitic iron ores at lower temperatures.

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来源期刊
环境科学与技术
环境科学与技术 环境科学-工程:环境
CiteScore
17.50
自引率
9.60%
发文量
12359
审稿时长
2.8 months
期刊介绍: Environmental Science & Technology (ES&T) is a co-sponsored academic and technical magazine by the Hubei Provincial Environmental Protection Bureau and the Hubei Provincial Academy of Environmental Sciences. Environmental Science & Technology (ES&T) holds the status of Chinese core journals, scientific papers source journals of China, Chinese Science Citation Database source journals, and Chinese Academic Journal Comprehensive Evaluation Database source journals. This publication focuses on the academic field of environmental protection, featuring articles related to environmental protection and technical advancements.
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