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Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies

Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies
Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies
Magnetic measurements of samples with precisely controlled magnetic mineralogy, grain size, and interparticle spacing are needed to provide crucial experimental rock magnetic underpinning for paleomagnetic studies. We report a novel nanofabrication method for producing two-dimensional arrays of cylindrical synthetic magnetite particles with well-defined composition, particle size, and interparticle spacing. The samples are fabricated by writing dot arrays with electron beam lithography, transferring these patterns into sputtered Fe thin films by reactive ion etching in a CO/NH3 plasma, and oxidizing the resulting Fe particles in a controlled atmosphere to form magnetite. Scanning electron microscopy and transmission electron microscopy have been used to monitor the fabrication process and to determine the particle geometry. The particle sizes of our samples range between 100 nm and 265 nm with center-to-center spacings between 180 nm and 310 nm. Low-temperature magnetic remanence data confirm the stoichiometry of the magnetite. We present magnetic hysteresis data and first-order reversal curve diagrams for our samples and compare these with previously published data from other synthetic and natural magnetite samples. The ability to independently control particle size and interparticle spacing of magnetite grains makes our synthetic samples ideal for studying the influence of magnetostatic interactions on the paleomagnetic recording fidelity of naturally occurring magnetite in rocks.
0148-0227
B02104
Krása, David
00b97559-03e0-473a-834d-880a497139f7
Wilkinson, Chris D. W.
7169cf33-5a80-4315-a4e6-b23685bd47d2
Gadegaard, Nikolaj
bf72c3d1-e6a7-48b4-a968-c496b655bd98
Kong, Xiang
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Zhou, Haiping
1d2a368e-34cf-44b3-a12a-0a2110db1cc7
Roberts, Andrew P.
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Muxworthy, Adrian R.
7fa5c819-b5ca-4354-83df-f9481b16ed1e
Williams, Wyn
d8b0d6be-3729-4126-a3ec-628638b75292
Krása, David
00b97559-03e0-473a-834d-880a497139f7
Wilkinson, Chris D. W.
7169cf33-5a80-4315-a4e6-b23685bd47d2
Gadegaard, Nikolaj
bf72c3d1-e6a7-48b4-a968-c496b655bd98
Kong, Xiang
f868e708-9360-4ac7-b8d0-84320b1efc87
Zhou, Haiping
1d2a368e-34cf-44b3-a12a-0a2110db1cc7
Roberts, Andrew P.
4f062491-5408-4edb-8dd1-140c6a42e93f
Muxworthy, Adrian R.
7fa5c819-b5ca-4354-83df-f9481b16ed1e
Williams, Wyn
d8b0d6be-3729-4126-a3ec-628638b75292

Krása, David, Wilkinson, Chris D. W., Gadegaard, Nikolaj, Kong, Xiang, Zhou, Haiping, Roberts, Andrew P., Muxworthy, Adrian R. and Williams, Wyn (2009) Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies. Journal of Geophysical Research, 114 (B2), B02104. (doi:10.1029/2008JB006017).

Record type: Article

Abstract

Magnetic measurements of samples with precisely controlled magnetic mineralogy, grain size, and interparticle spacing are needed to provide crucial experimental rock magnetic underpinning for paleomagnetic studies. We report a novel nanofabrication method for producing two-dimensional arrays of cylindrical synthetic magnetite particles with well-defined composition, particle size, and interparticle spacing. The samples are fabricated by writing dot arrays with electron beam lithography, transferring these patterns into sputtered Fe thin films by reactive ion etching in a CO/NH3 plasma, and oxidizing the resulting Fe particles in a controlled atmosphere to form magnetite. Scanning electron microscopy and transmission electron microscopy have been used to monitor the fabrication process and to determine the particle geometry. The particle sizes of our samples range between 100 nm and 265 nm with center-to-center spacings between 180 nm and 310 nm. Low-temperature magnetic remanence data confirm the stoichiometry of the magnetite. We present magnetic hysteresis data and first-order reversal curve diagrams for our samples and compare these with previously published data from other synthetic and natural magnetite samples. The ability to independently control particle size and interparticle spacing of magnetite grains makes our synthetic samples ideal for studying the influence of magnetostatic interactions on the paleomagnetic recording fidelity of naturally occurring magnetite in rocks.

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Published date: 17 February 2009

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Local EPrints ID: 65946
URI: http://eprints.soton.ac.uk/id/eprint/65946
ISSN: 0148-0227
PURE UUID: d68dd502-162b-44cf-b36b-2af2dba4fbd8

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Date deposited: 03 Apr 2009
Last modified: 13 Mar 2024 18:01

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Contributors

Author: David Krása
Author: Chris D. W. Wilkinson
Author: Nikolaj Gadegaard
Author: Xiang Kong
Author: Haiping Zhou
Author: Andrew P. Roberts
Author: Adrian R. Muxworthy
Author: Wyn Williams

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