Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies
| dc.contributor.author | Krasa, David | |
| dc.contributor.author | Wilkinson, Chris D W | |
| dc.contributor.author | Gadegaard, Nikolaj | |
| dc.contributor.author | Kong, Xiang | |
| dc.contributor.author | Zhou, Haiping | |
| dc.contributor.author | Roberts, Andrew | |
| dc.contributor.author | Muxworthy, Adrian R | |
| dc.contributor.author | Williams, Wyn | |
| dc.date.accessioned | 2015-12-10T21:55:50Z | |
| dc.date.issued | 2009 | |
| dc.date.updated | 2016-02-24T11:05:40Z | |
| dc.description.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. | |
| dc.identifier.issn | 0148-0227 | |
| dc.identifier.uri | http://hdl.handle.net/1885/39157 | |
| dc.publisher | American Geophysical Union | |
| dc.source | Journal of Geophysical Research | |
| dc.subject | Keywords: etching; grain size; magnetic mineral; magnetic survey; magnetite; natural remanent magnetization; oxidation; paleomagnetism; particle size; scanning electron microscopy; stoichiometry; transmission electron microscopy | |
| dc.title | Nanofabrication of two-dimensional arrays of magnetite particles for fundamental rock magnetic studies | |
| dc.type | Journal article | |
| local.bibliographicCitation.lastpage | B02113 | |
| local.bibliographicCitation.startpage | B02104 | |
| local.contributor.affiliation | Krasa, David, University of Edinburgh | |
| local.contributor.affiliation | Wilkinson, Chris D W, Univeristy of Glasgow | |
| local.contributor.affiliation | Gadegaard, Nikolaj, Univeristy of Glasgow | |
| local.contributor.affiliation | Kong, Xiang, University of Southampton | |
| local.contributor.affiliation | Zhou, Haiping, Univeristy of Glasgow | |
| local.contributor.affiliation | Roberts, Andrew, College of Physical and Mathematical Sciences, ANU | |
| local.contributor.affiliation | Muxworthy, Adrian R, Imperial College London | |
| local.contributor.affiliation | Williams, Wyn, Univeristy of Glasgow | |
| local.contributor.authoruid | Roberts, Andrew, u4817957 | |
| local.description.embargo | 2037-12-31 | |
| local.description.notes | Imported from ARIES | |
| local.identifier.absfor | 040406 - Magnetism and Palaeomagnetism | |
| local.identifier.ariespublication | U4353633xPUB172 | |
| local.identifier.citationvolume | 114 | |
| local.identifier.doi | 10.1029/2008JB006017 | |
| local.identifier.scopusID | 2-s2.0-66149163117 | |
| local.type.status | Published Version |
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