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Left: Transmission electron microscopy (TEM) images
of the Fe(III)-reducing bacterium, Geobacter sulfurreducens.
Right: TEM images of magnetite nanoparticles produced by the
bacteria. Note the difference in the scale bars.
21st-Century Medicinal Magnetism
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A relatively unexplored resource for magnetic nanomaterial production is a
type of subsurface microorganism capable of producing large quantities
of nanoscale magnetite (Fe3O4) at ambient temperatures. Metal-reducing
bacteria live in soils deficient in oxygen and conserve energy for
growth through the oxidation of hydrogen or organic electron donors,
coupled to the reduction of oxidized metals such as Fe(III)-bearing
minerals. This can result in the formation of magnetite via the extracellular
reduction of amorphous Fe(III)-oxyhydroxides, releasing soluble Fe(II)
and completely recrystallizing the amorphous mineral into a new phase.
The Manchester team developed a method for producing large quantities of
highly crystalline magnetite and cobalt ferrite (CoFe2O4) nanoparticles
using the Fe(III)-reducing bacterium, Geobacter sulfurreducens.
In particular, they demonstrated that cobalt ferrite nanoparticles with
the high coercivity (i.e., resistance to demagnetization) important for
applications can be manufactured through this biotechnological route. Three
samples containing increasing amounts of Co in the biogenic magnetite structure
were analyzed. X-ray diffraction and transmission electron microscopy showed
that the material is nanocrystalline. Moreover, the coercivity of the samples
increases with increasing Co content, so that it can be tuned for specific
applications.
The cation distribution in the ferrite nanoparticles was investigated using
x ray absorption (XA) and x-ray magnetic circular dichroism (XMCD)
at the Fe L2,3 and Co L2,3 edges,
measured at ALS Beamline 4.0.2. An XMCD spectrum is obtained as
the difference between two XA spectra measured in opposite external
magnetic fields. Magnetite has an inverse spinel crystal structure,
which contains tetrahedral (Td)
and octahedral (Oh) sites
accommodating Fe2+ and Fe3+ cations. Each specific
cation in the spinel structure generates a unique XMCD signature
determined by its valence state (number of d electrons), site symmetry
(i.e., Td or Oh),
and moment direction, which can be computed using atomic multiplet
calculations. By fitting a weighted sum of these calculated spectra
to the measured XMCD spectra, the site occupations of the Fe cations
can be obtained.
The biogenic materials show a striking change with increasing Co amount,
namely a decrease in intensity of the leading negative peak in
the Fe L3
edge, which implies that Co is predominantly replacing Fe2+ cations
in octahedral sites. Similarly, the site occupancy and oxidation state of
the Co can be directly assessed by examining the Co L2,3 XA
and XMCD spectra. The close similarity with the spectra for synthetically
produced CoFe2O4 thin films confirmed that
the bacteria were able to suitably accommodate Co in the ferrite structure
with the Co2+ residing primarily on Oh sites.

Top left: Crystal structure of cobalt ferrite
(CoFe2O4). Bottom left: Magnetic hysteresis
loops measured at T = 5 K for biogenic magnetite (red) and cobalt
ferrite (blue). A wider hysteresis loop indicates a higher resistance
to demagnetization. Center: Experimental (black) and best-fit
(red) Fe L2,3 XMCD spectra for biogenic magnetite
(top), cobalt-ferrite with 6 atom % Co (middle) and 23 atom %
Co (bottom). Right: The decomposition of the XMCD spectra into
the Fe2+ Oh (purple), Fe3+ Td (blue),
and Fe3+ Oh (green) components.
The color-coded numbers indicate the proportions of the components
in the XMCD spectrum.
The XMCD measurements indicate a dramatic enhancement in the magnetic
properties of biogenically produced nanoparticles when large quantities of
Co are introduced into the spinel structure, a major advance over previous
biomineralization studies. Inclusion of other transition metals into the spinel
structure by Fe(III)-reducing bacteria to tailor the magnetic properties of
nanoferrites could lead to a suite of materials required for different technological
uses. The successful production of highly ordered crystalline nanoparticulate
ferrites demonstrates the potential for scaled-up industrial manufacture of
nanoparticles using environmentally benign and energy-efficient methodologies.
Research conducted by V.S. Coker, N.D. Telling, R.A.D. Pattrick,
C.I. Pearce, J.R. Lloyd, F. Tuna, and R.E.P. Winpenny (University
of Manchester, UK); G. van der Laan (Diamond Light Source, UK);
and E. Arenholz (ALS).
Research funding: UK Engineering and Physical Sciences Research
Council and UK Biotechnology and Biological Sciences Research Council. Operation
of the ALS is supported by the U.S. Department of Energy, Office
of Basic Energy Sciences.
Publication about this research: V.S. Coker, N.D. Telling, G.
van der Laan, R.A.D. Pattrick, C.I. Pearce, E. Arenholz, F. Tuna,
R. Winpenny, and J.R. Lloyd, "Harnessing the extracellular
bacterial production of nanoscale cobalt ferrite with exploitable
magnetic properties," ACS Nano 3,
1922 (2009). |