| 有机质对纳米级磁铁矿热稳定性的影响 |
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| 引用本文： | 吴文芳,李金华,张春霞,潘永信.有机质对纳米级磁铁矿热稳定性的影响[J].地球物理学报,2010,53(10):2427-2434. |
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| 作者姓名： | 吴文芳 李金华 张春霞 潘永信 |
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| 作者单位： | 1. 中国科学院地质与地球物理研究所地球深部研究重点实验室,北京 100029;
2. 中国科学院研究生院,北京 100049;
3. 中法生物矿化与纳米结构联合实验室, 北京 100029;
4. 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室,北京 100029 |
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| 基金项目： | 国家自然科学基金委创新群体，中国科学院创新团队国际合作伙伴计划项目 |
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| 摘 要： | 单畴磁铁矿颗粒是地质样品中最重要的磁性载体,其稳定性一直备受关注.为了认识有机质对纳米级磁铁矿颗粒热稳定性的影响,本文对比研究了趋磁细菌AMB-1合成的单畴磁铁矿分别在全细胞中和经去胞提纯后的纯化磁小体中的热磁性质,以及热处理后样品的磁滞参数和低温磁性的变化.发现仅有磁小体膜包裹的纯化磁小体中单畴磁铁矿热稳定性极强,而全细胞中的单畴磁铁矿加热过程中发生了显著的热变化:磁铁矿在约270℃即开始转化,400℃以前几乎完全被有机质还原为顺磁性物质;同时在400℃以前,有机质的还原作用与有机质热分解引起磁小体链的坍塌,共同导致了样品矫顽力(Bc)、剩磁矫顽力(Bcr)和剩磁比(Mrs/Ms)的减小,以及矫顽力比(Bcr/Bc)的增加. 我们的实验结果清楚地表明,当地质样品中含有较多有机质组分并受热事件影响时,其中的单畴磁铁矿难以得到保存.
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| 关 键 词： | 有机质 磁小体磁铁矿 热稳定性 |
| 收稿时间： | 2010-03-03 |
Effects of organic matter on thermal stability of nanometer-sized magnetite |
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| WU Wen-Fang,LI Jin-Hua,ZHANG Chun-Xia,PAN Yong-Xin.Effects of organic matter on thermal stability of nanometer-sized magnetite[J].Chinese Journal of Geophysics,2010,53(10):2427-2434. |
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| Authors: | WU Wen-Fang LI Jin-Hua ZHANG Chun-Xia PAN Yong-Xin |
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| Institution: | 1. Key Laboratory of the Earth's Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;
2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China;
3. Franco-Chinese Biomineralization and Nano-structures Laboratory, Beijing 100029, China;
4. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
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| Abstract: | Single domain (SD) magnetite particles are significant magnetic carriers in geologic samples. However, its stability remains a major concern due to their fine-grain sizes. To probe the effects of organic matter on thermal stability of magnetite nanoparticles, we comparatively studied the thermo-magnetic properties, hysteresis parameters and low-temperature magnetic behaviors of isolated magnetosome magnetites of Magnetospirillum magneticum AMB-1 and whole cell samples. The isolated SD magnetosome magentites with few amount of organic matter showed extremely good thermal stability, while the SD magnetites in whole cells changed strikingly during thermal treatment. The latter began to convert by ~270℃,and were almost entirely reduced to paramagnetic substance by 400℃. The coercivity (Bc), remanent coercivity (Bcr) and the ratio of saturation remanence to saturation magnetization (Mrs/Ms) decreased, while the ratio of remanence coercivity to coercivity (Bcr/Bc) increased when heating up to 400℃, owing to the reduction and decomposition of organic matter in whole cell. Our results indicated that SD magnetite in geologic samples carrying substantial organic matter can be hardly preserved if the samples were once heated to 300℃~400℃. |
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| Keywords: | Organic matter Magnetosome magnetite Thermal stability |
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