磁铁矿
磁性纳米颗粒
细菌
土生土长的
纳米颗粒
硫酸盐还原菌
化学
化学工程
材料科学
环境科学
环境化学
磁性纳米粒子
纳米技术
生物
冶金
生态学
工程类
遗传学
出处
期刊:Minerals
[MDPI AG]
日期:2018-05-14
卷期号:8 (5): 212-212
被引量:3
摘要
Recent researches have shown that microbe–metal interactions play an important role in metal cycling and biomineralization in subsurface environments. The objective of this research was to study the effects of microbial growth conditions for size control on the synthesis of magnetite nanoparticles using Fe(III)-reducing bacteria enriched from intertidal flat sediments in Korea. The microbial formation of the magnetite nanoparticles was examined under various incubation temperatures (8–35 °C), concentrations (20–60 mM) of magnetite precursor, medium pHs (6.5–8.5), and incubation times (0–3 weeks). The Fe(III)-reducing bacteria formed 2~10 nm-sized magnetite (Fe3O4) by reduction of 40 mM akaganeite, especially under the conditions at 25 °C and medium pH = 8.5 within a 1-week incubation time. The magnetite nanoparticles formed by microbial processes exhibited superparamagnetic behavior.
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