Roh Yul, Jang Hee-Dong, Suh Yongjae
Faculty of Earth Systems and Environmental Sciences, Chonnam National University, Gwangju 500-757, Korea.
J Nanosci Nanotechnol. 2007 Nov;7(11):3938-43. doi: 10.1166/jnn.2007.076.
Microbial synthesis of magnetite and metal (Co, Cr, Ni)-substituted magnetites has only recently been reported. The objective of this study was to examine the influence of Mn ion on the microbial synthesis of magnetite nanoparticles. The reductive biotransformation of an akaganeite (beta-FeOOH) or a Mn-substituted (2-20 mol%) akaganeite (Fe(1-x)Mn(x)OOH) by Shewanella loiha (PV-4, 25 degrees C) and Thermoanaerobacter ethanolicus (TOR-39, 60 degrees C) was investigated under anaerobic conditions at circumneutral pH (pH = 7-8). Both bacteria formed magnetite nanoparticles using akaganeite as a magnetite precursor. By comparison of iron minerals formed by PV-4 and TOR-39 using Mn-mixed akaganeite as the precursor, it was shown that PV-4 formed siderite (FeCO3), green rust [Fe2+Fe3+(OH)16CO3 x 4H2O], and magnetite at 25 degrees C, whereas TOR-39 formed mainly nm-sized magnetite at 60 degrees C. The presence of Mn in the magnetite formed by TOR-39 was revealed by energy dispersive X-ray analysis (EDX) is indicative of Mn substitution into magnetite crystals. EDX analysis of iron minerals formed by PV-4 showed that Mn was preferentially concentrated in the siderite and green rust. These results demonstrate that coprecipitated/sorbed Mn induced microbial formation of siderite and green rust by PV-4 at 25 degrees C, but the synthesis of Mn-substituted magnetite nanoparticles proceeded by TOR-39 at 60 degrees C. These results indicate that the bacteria have the ability to synthesize magnetite and Mn-substituted magnetite nano-crystals. Microbially facilitated synthesis of magnetite and metal-substituted magnetites at near ambient temperatures may expand the possible use of specialized ferromagnetic nano-particles.
微生物合成磁铁矿以及金属(钴、铬、镍)取代的磁铁矿直到最近才见报道。本研究的目的是考察锰离子对微生物合成磁铁矿纳米颗粒的影响。研究了嗜冷希瓦氏菌(PV-4,25℃)和嗜热栖热菌(TOR-39,60℃)在厌氧条件下、中性pH值(pH = 7 - 8)时对赤铁矿(β-FeOOH)或锰取代(2 - 20摩尔%)赤铁矿(Fe(1-x)Mn(x)OOH)的还原生物转化。两种细菌均以赤铁矿作为磁铁矿前体形成磁铁矿纳米颗粒。通过比较PV-4和TOR-39以锰混合赤铁矿为前体形成的铁矿物,结果表明PV-4在25℃时形成菱铁矿(FeCO3)、绿锈[Fe2+Fe3+(OH)16CO3·4H2O]和磁铁矿,而TOR-39在60℃时主要形成纳米尺寸的磁铁矿。通过能量色散X射线分析(EDX)揭示了TOR-39形成的磁铁矿中存在锰,这表明锰取代进入了磁铁矿晶体。对PV-4形成的铁矿物进行的EDX分析表明,锰优先富集在菱铁矿和绿锈中。这些结果表明,共沉淀/吸附的锰在25℃时诱导PV-4微生物形成菱铁矿和绿锈,但TOR-39在60℃时进行锰取代磁铁矿纳米颗粒的合成。这些结果表明细菌有能力合成磁铁矿和锰取代的磁铁矿纳米晶体。在接近环境温度下微生物促进合成磁铁矿和金属取代的磁铁矿可能会扩大特种铁磁纳米颗粒的潜在用途。