光电子注入诱导二线水合铁快速相变为赤铁矿

IF 3.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Lixia Yan , Jing Liu , Zihe Ren , Qingze Chen , Hongyan Wei , Jianxi Zhu , Runliang Zhu
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引用次数: 0

摘要

二线水合铁(Fh)的相变在调节地球近地表环境中的元素循环和能量转移中起着至关重要的作用。氧化还原转化已被确定为Fh相变的重要途径。半导体矿物作为典型的电子给体,可以诱导Fh的氧化还原转化,也可以作为非均相表面,影响其聚集和结晶过程。在这项工作中,我们研究了纳米TiO2(一种天然半导体)在光照射下Fh转化的速率和产物类型。我们的研究结果表明,光照射以及TiO2和小有机分子(甲醇)的共存对于Fh(在3 h内)的快速相变(主要是向Hem)是必不可少的。较高的甲醇含量和较低的O2含量有利于Hem的形成,产物中Hem的转化速度较快,含量较高。对反应过程中固相的分析表明Fe(II)的存在,表明TiO2的光电子对Fh进行了还原。令人惊讶的是,与通常认为的Fh在室温还原条件下向针铁矿的转变不同,Hem在本研究中被确定为主要产物,而不考虑溶液pH (pH 4,7和12)。这一现象可归因于TiO2存在下的固-固电子转移和Fh的易聚集,两者都促进了Fh的结构重排,从而形成赤铁矿,同时抑制了Fh的溶解-再结晶为蛭石和针铁矿。本研究强调了光电子在加速Fh相变和影响Fh相变途径中的作用。考虑到天然半导体和有机化学物质的广泛存在,我们提出在地球近地表环境中,光电子诱导的Fh转变是一个重要但被忽视的过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fast phase transformation of 2-line ferrihydrite to hematite as induced by the injection of photoelectrons
The phase transformation of 2-line ferrihydrite (Fh) to more thermodynamically stable iron (oxyhydr)oxides plays a crucial role in regulating the element cycling and energy transfer in Earth's near-surface environments. Redox transformation has been identified as a significant pathway in the phase transformation of Fh. As typical electron-donors, semiconducting minerals can induce the redox transformation of Fh and also serve as heterogeneous surfaces, influencing the aggregation and crystallization processes. In this work, we investigated the rate and product type of Fh transformation in the presence of nanosized TiO2, a natural semiconductor, under light irradiation. Our findings demonstrate that light irradiation and the coexistence of both TiO2 and small organic molecules (methanol) are essential for the rapid phase transformation of Fh (within 3 h), primarily to Hem. Higher methanol content and lower O2 content facilitate the formation of Hem, as evidenced by the faster transformation rate and the higher Hem content in the products. Analysis of the solid phase during the reaction reveals the presence of Fe(II), indicating the reduction of Fh by photoelectrons from TiO2. Surprisingly, unlike the commonly recognized transformation of Fh to goethite under reduction conditions at room temperature, Hem is identified as the primary product in this study, regardless of the solution pH (pH 4, 7, and 12). This phenomenon can be attributed to the solid-to-solid electron transfer and the facilitated aggregation of Fh in the presence of TiO2, both of which promote the structural rearrangement of Fh leading to the formation of hematite while inhibiting its dissolution-recrystallization into lepidocrocite and goethite. This study highlights the role of photoelectrons in accelerating the phase transformation and influencing the transformation pathway of Fh. Considering the widespread occurrence of natural semiconductors and organic chemicals, we propose that photoelectron-induced transformation of Fh is an important yet overlooked process in Earth's near-surface environments.
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来源期刊
Chemical Geology
Chemical Geology 地学-地球化学与地球物理
CiteScore
7.20
自引率
10.30%
发文量
374
审稿时长
3.6 months
期刊介绍: Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry. The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry. Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry. The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.
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