共生赤铁矿诱导并加速铁水云母的转化:途径和内在机制

IF 2.7 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS American Mineralogist Pub Date : 2024-07-04 DOI:10.2138/am-2023-9281
Hongyan Wei, Jing Liu, Qingze Chen, Yixuan Yang, H. Xian, Xiaoliang Liang, Yiping Yang, Jianxi Zhu, Runliang Zhu
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引用次数: 0

摘要

异质表面诱导的结晶是地球化学、生物矿化和材料合成中的一个重要过程,但异质表面对蜕变相转化为新晶体的影响仍然知之甚少。在这项工作中,我们研究了在不同 pH 值(4、7 和 12)下,具有特定暴露面({001} 和 {113})的赤铁矿(Hem)纳米板存在下的铁水物(Fhy)转化行为。我们的研究结果表明,Hem 纳米板可诱导 Fhy 向 Hem/Gth(鹅铁矿)转化,并加快转化速度。这种效果主要是通过调节溶解-再结晶过程实现的,即加速 Fhy 的溶解和促进添加 Hem 纳米板表面的异质结晶(形成新的 Hem/Gth),而溶液的 pH 值在这些过程中起着至关重要的作用。具体来说,在 pH 值为 4 时,Fhy 提供的溶解 Fe3+ 相对较少,这有利于新 Hem 在 Hem 纳米板的{001}面呈岛状生长,并在{113}面呈层状生长,最终形成热力学上稳定的伪立方体形态(露出{012}面)。由于 Fhy 在 pH 值为 7 时的溶解度非常低,因此 Hem 纳米板对 Fhy 的诱导转化相当微弱。而在 pH 值为 12 时,来自 Fhy 的大量溶解 Fe3+ 有利于 Hem 在{001}面上的逐层生长,以及 Gth 在{113}面上的显著异外延生长。除了诱导转化外,Fhy 向 Hem 的直接固态转化和溶解的 Fe3+ 的均匀结晶也有助于 Fhy 的转化。这项研究首次很好地揭示了在Hem纳米粒子存在下Fhy的诱导转化机制,这将推进我们对异质表面在调节蜕变相转化中的重要作用的理解,并补充了Fhy的转化机制。
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Coexisting hematite induces and accelerates the transformation of ferrihydrite: pathway and underlying mechanisms
Crystallization induced by heterogeneous surfaces is an important process in geochemistry, biomineralization, and material synthesis, but the effects of heterogeneous surfaces on the transformation of metastable phases into new crystals remain poorly understood. In this work, we studied the transformation behaviors of ferrihydrite (Fhy) in the presence of hematite (Hem) nanoplates with specific exposed facets ({001} and {113}) at different pH (4, 7, and 12). Our results reveal that the Hem nanoplates can induce the transformation of Fhy to Hem/Gth (goethite) and accelerate the transformation rate. This effect is primarily achieved by modulating the dissolution-recrystallization process, i.e., accelerating the dissolution of Fhy and promoting the heterogeneous crystallization (to form new Hem/Gth) at the surface of added Hem nanoplates, and solution pH plays crucial roles in these processes. In specific, a relatively low supply of dissolved Fe3+ from Fhy at pH 4 favors island growth of new Hem at the {001} facets of Hem nanoplates and layer-by-layer growth at the {113} facets, which eventually results in the formation of thermodynamically stable pseudo-cubic morphology (exposing {012} facets). Because of the very low solubility of Fhy at pH 7, the induced transformation of Fhy by Hem nanoplates is rather weak. While at pH 12, a high supply of dissolved Fe3+ from Fhy benefits the layer-by-layer growth at {001} facets of Hem and the significant heteroepitaxial growth of Gth at the {113} facets. Besides the induced transformation, the direct solid-state transformation of Fhy into Hem and the homogeneous crystallization of dissolved Fe3+ also contribute to the transformation of Fhy. This study, for the first time, well reveals the mechanisms of induced transformation of Fhy in the presence of Hem nanoparticles, which will advance our understanding of the significant effects of heterogeneous surfaces in modulating the transformation of metastable phases, and supplement the transformation mechanisms of Fhy.
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来源期刊
American Mineralogist
American Mineralogist 地学-地球化学与地球物理
CiteScore
5.20
自引率
9.70%
发文量
276
审稿时长
1 months
期刊介绍: American Mineralogist: Journal of Earth and Planetary Materials (Am Min), is the flagship journal of the Mineralogical Society of America (MSA), continuously published since 1916. Am Min is home to some of the most important advances in the Earth Sciences. Our mission is a continuance of this heritage: to provide readers with reports on original scientific research, both fundamental and applied, with far reaching implications and far ranging appeal. Topics of interest cover all aspects of planetary evolution, and biological and atmospheric processes mediated by solid-state phenomena. These include, but are not limited to, mineralogy and crystallography, high- and low-temperature geochemistry, petrology, geofluids, bio-geochemistry, bio-mineralogy, synthetic materials of relevance to the Earth and planetary sciences, and breakthroughs in analytical methods of any of the aforementioned.
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