{"title":"Mn2+ 浓度对酸性条件下 δ-MnO2 晶体生长的影响","authors":"Liyan Bi, Haoran Hu, Lei Wang, Zuran Li, Fangdong Zhan, Yongmei He, Yanqun Zu, Yuan Li, Xinran Liang","doi":"10.1186/s12932-024-00091-x","DOIUrl":null,"url":null,"abstract":"<div><p>δ-MnO<sub>2</sub> is an important component of environmental minerals and is among the strongest sorbents and oxidants. The crystalline morphology of δ-MnO<sub>2</sub> is one of the key factors affecting its reactivity. In this work, δ-MnO<sub>2</sub> was initially synthesized and placed in an acidic environment to react with Mn<sup>2+</sup> and undergo a crystalline transformation. During the transformation of crystalline δ-MnO<sub>2</sub>, kinetic sampling was conducted, followed by analyses of the structures and morphologies of the samples. The results showed that at pH 2.5 and 4, δ-MnO<sub>2</sub> nanoflakes spontaneously self-assembled into nanoribbons via edge-to-edge assembly in the initial stage. Subsequently, these nanoribbons attached to each other to form primary nanorods through a face-to-face assembly along the <i>c</i>-axis. These primary nanorods then assembled along the (001) planes and lateral surfaces, achieving further growth and thickening. Since a lower pH is more favorable for the formation of vacancies in δ-MnO<sub>2</sub>, δ-MnO<sub>2</sub> can rapidly adsorb Mn<sup>2+</sup> directly onto the vacancies to form tunnel walls. At the same time, the rapid formation of the tunnel walls leads to a quick establishment of hydrogen bonding between adjacent nanoribbons, enabling the assembly of these nanoribbons into primary nanorods. Therefore, in a solution with the same concentration of Mn<sup>2+</sup>, the structure transformation and morphology evolution of δ-MnO<sub>2</sub> to α-MnO<sub>2</sub> occur faster at pH 2.5 than at pH 4. These findings provide insights into the mechanism for crystal growth from layer-based to tunnel-based nanorods and methods for efficient and controlled syntheses of nanomaterials.</p></div>","PeriodicalId":12694,"journal":{"name":"Geochemical Transactions","volume":"25 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2024-09-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://geochemicaltransactions.biomedcentral.com/counter/pdf/10.1186/s12932-024-00091-x","citationCount":"0","resultStr":"{\"title\":\"Effect of Mn2+ concentration on the growth of δ-MnO2 crystals under acidic conditions\",\"authors\":\"Liyan Bi, Haoran Hu, Lei Wang, Zuran Li, Fangdong Zhan, Yongmei He, Yanqun Zu, Yuan Li, Xinran Liang\",\"doi\":\"10.1186/s12932-024-00091-x\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>δ-MnO<sub>2</sub> is an important component of environmental minerals and is among the strongest sorbents and oxidants. The crystalline morphology of δ-MnO<sub>2</sub> is one of the key factors affecting its reactivity. In this work, δ-MnO<sub>2</sub> was initially synthesized and placed in an acidic environment to react with Mn<sup>2+</sup> and undergo a crystalline transformation. During the transformation of crystalline δ-MnO<sub>2</sub>, kinetic sampling was conducted, followed by analyses of the structures and morphologies of the samples. The results showed that at pH 2.5 and 4, δ-MnO<sub>2</sub> nanoflakes spontaneously self-assembled into nanoribbons via edge-to-edge assembly in the initial stage. Subsequently, these nanoribbons attached to each other to form primary nanorods through a face-to-face assembly along the <i>c</i>-axis. These primary nanorods then assembled along the (001) planes and lateral surfaces, achieving further growth and thickening. Since a lower pH is more favorable for the formation of vacancies in δ-MnO<sub>2</sub>, δ-MnO<sub>2</sub> can rapidly adsorb Mn<sup>2+</sup> directly onto the vacancies to form tunnel walls. At the same time, the rapid formation of the tunnel walls leads to a quick establishment of hydrogen bonding between adjacent nanoribbons, enabling the assembly of these nanoribbons into primary nanorods. Therefore, in a solution with the same concentration of Mn<sup>2+</sup>, the structure transformation and morphology evolution of δ-MnO<sub>2</sub> to α-MnO<sub>2</sub> occur faster at pH 2.5 than at pH 4. These findings provide insights into the mechanism for crystal growth from layer-based to tunnel-based nanorods and methods for efficient and controlled syntheses of nanomaterials.</p></div>\",\"PeriodicalId\":12694,\"journal\":{\"name\":\"Geochemical Transactions\",\"volume\":\"25 1\",\"pages\":\"\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2024-09-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://geochemicaltransactions.biomedcentral.com/counter/pdf/10.1186/s12932-024-00091-x\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geochemical Transactions\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1186/s12932-024-00091-x\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemical Transactions","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1186/s12932-024-00091-x","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Effect of Mn2+ concentration on the growth of δ-MnO2 crystals under acidic conditions
δ-MnO2 is an important component of environmental minerals and is among the strongest sorbents and oxidants. The crystalline morphology of δ-MnO2 is one of the key factors affecting its reactivity. In this work, δ-MnO2 was initially synthesized and placed in an acidic environment to react with Mn2+ and undergo a crystalline transformation. During the transformation of crystalline δ-MnO2, kinetic sampling was conducted, followed by analyses of the structures and morphologies of the samples. The results showed that at pH 2.5 and 4, δ-MnO2 nanoflakes spontaneously self-assembled into nanoribbons via edge-to-edge assembly in the initial stage. Subsequently, these nanoribbons attached to each other to form primary nanorods through a face-to-face assembly along the c-axis. These primary nanorods then assembled along the (001) planes and lateral surfaces, achieving further growth and thickening. Since a lower pH is more favorable for the formation of vacancies in δ-MnO2, δ-MnO2 can rapidly adsorb Mn2+ directly onto the vacancies to form tunnel walls. At the same time, the rapid formation of the tunnel walls leads to a quick establishment of hydrogen bonding between adjacent nanoribbons, enabling the assembly of these nanoribbons into primary nanorods. Therefore, in a solution with the same concentration of Mn2+, the structure transformation and morphology evolution of δ-MnO2 to α-MnO2 occur faster at pH 2.5 than at pH 4. These findings provide insights into the mechanism for crystal growth from layer-based to tunnel-based nanorods and methods for efficient and controlled syntheses of nanomaterials.
期刊介绍:
Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.