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AGU: Journal of Geophysical Research, Solid Earth

 

Keywords

  • rock magnetism
  • mineral magnetism
  • magnetite
  • nanofabrication
  • electron beam lithography
  • reactive ion etching

Index Terms

  • Geomagnetism and Paleomagnetism: Rock and mineral magnetism
  • Geomagnetism and Paleomagnetism: Magnetic mineralogy and petrology
  • Geomagnetism and Paleomagnetism: Instruments and techniques
Abstract
Cited By (1)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, B02104, 11 PP., 2009
doi:10.1029/2008JB006017

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

David Krása

School of GeoSciences, University of Edinburgh, Edinburgh, UK

Chris D. W. Wilkinson

James Watt Nanofabrication Centre, Department of Electronics and Electrical Engineering, University of Glasgow, Glasgow, UK

Nikolaj Gadegaard

James Watt Nanofabrication Centre, Department of Electronics and Electrical Engineering, University of Glasgow, Glasgow, UK

Xiang Kong

Department of Physics and Astronomy, University of Glasgow, Glasgow, UK

Haiping Zhou

James Watt Nanofabrication Centre, Department of Electronics and Electrical Engineering, University of Glasgow, Glasgow, UK

Andrew P. Roberts

National Oceanography Centre, University of Southampton, Southampton, UK

Adrian R. Muxworthy

Department of Earth Science and Engineering, Imperial College, London, UK

Wyn Williams

School of GeoSciences, University of Edinburgh, Edinburgh, UK

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.

Received 15 August 2008; accepted 18 December 2008; published 17 February 2009.

Citation: Krása, D., C. D. W. Wilkinson, N. Gadegaard, X. Kong, H. Zhou, A. P. Roberts, A. R. Muxworthy, and W. Williams (2009), Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies, J. Geophys. Res., 114, B02104, doi:10.1029/2008JB006017.

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