土壤中常见的晶态铁氧化物有针铁矿(Goethite)、赤铁矿(Hematite)、磁 赤铁矿(Maghemite)、磁铁矿(Magnetite)、纤铁矿(Lepidocrocite)和水铁矿 (Ferrihydrite)等(熊毅,1983)。
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Anionic maghemite nanoparticles allow labeling of a wide cell variety and their recognition in cellular, organo typical, and animal models.
阴离子磁赤铁矿纳米颗粒能够标记多种细胞,并用于细胞、器官和动物模型的识别。
The analysis of the iron bearing mineral compositions indicates that the major iron bearing minerals in the rocks are magnetite, maghemite, hematite, pyrite and siderite.
矿物成分分析显示,岩石中主要含铁矿物为磁铁矿、磁赤铁矿、赤铁矿、黄铁矿和菱铁矿。
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