Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy

Useful paleomagnetic information is expected to be recorded by samples with moments up to three orders of magnitude below the detection limit of standard superconducting rock magnetometers. Such samples are now detectable using recently developed magnetic microscopes, which map the magnetic fields a...

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Main Authors: Lima, Eduardo A., Weiss, Benjamin P.
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: American Geophysical Union (AGU) 2017
Online Access:http://hdl.handle.net/1721.1/108020
https://orcid.org/0000-0003-3113-3415
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author Lima, Eduardo A.
Weiss, Benjamin P.
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Lima, Eduardo A.
Weiss, Benjamin P.
author_sort Lima, Eduardo A.
collection MIT
description Useful paleomagnetic information is expected to be recorded by samples with moments up to three orders of magnitude below the detection limit of standard superconducting rock magnetometers. Such samples are now detectable using recently developed magnetic microscopes, which map the magnetic fields above room-temperature samples with unprecedented spatial resolutions and field sensitivities. However, realizing this potential requires the development of techniques for retrieving sample moments from magnetic microscopy data. With this goal, we developed a technique for uniquely obtaining the net magnetic moment of geological samples from magnetic microscopy maps of unresolved or nearly unresolved magnetization. This technique is particularly powerful for analyzing small, weakly magnetized samples such as meteoritic chondrules and terrestrial silicate crystals like zircons. We validated this technique by applying it to field maps generated from synthetic sources and also to field maps measured using a superconducting quantum interference device (SQUID) microscope above geological samples with moments down to 10⁻¹⁵ Am². For the most magnetic rock samples, the net moments estimated from the SQUID microscope data are within error of independent moment measurements acquired using lower sensitivity standard rock magnetometers. In addition to its superior moment sensitivity, SQUID microscope net moment magnetometry also enables the identification and isolation of magnetic contamination and background sources, which is critical for improving accuracy in paleomagnetic studies of weakly magnetic samples.
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spelling mit-1721.1/1080202024-05-15T03:18:16Z Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy Lima, Eduardo A. Weiss, Benjamin P. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Weiss, Benjamin P Useful paleomagnetic information is expected to be recorded by samples with moments up to three orders of magnitude below the detection limit of standard superconducting rock magnetometers. Such samples are now detectable using recently developed magnetic microscopes, which map the magnetic fields above room-temperature samples with unprecedented spatial resolutions and field sensitivities. However, realizing this potential requires the development of techniques for retrieving sample moments from magnetic microscopy data. With this goal, we developed a technique for uniquely obtaining the net magnetic moment of geological samples from magnetic microscopy maps of unresolved or nearly unresolved magnetization. This technique is particularly powerful for analyzing small, weakly magnetized samples such as meteoritic chondrules and terrestrial silicate crystals like zircons. We validated this technique by applying it to field maps generated from synthetic sources and also to field maps measured using a superconducting quantum interference device (SQUID) microscope above geological samples with moments down to 10⁻¹⁵ Am². For the most magnetic rock samples, the net moments estimated from the SQUID microscope data are within error of independent moment measurements acquired using lower sensitivity standard rock magnetometers. In addition to its superior moment sensitivity, SQUID microscope net moment magnetometry also enables the identification and isolation of magnetic contamination and background sources, which is critical for improving accuracy in paleomagnetic studies of weakly magnetic samples. National Science Foundation (U.S.) (DMS-1521765) National Science Foundation (U.S.) (DMS-0934689) Peterson, Thomas F. 2017-04-10T18:09:39Z 2017-04-10T18:09:39Z 2016-10 2016-06 Article http://purl.org/eprint/type/JournalArticle 1525-2027 http://hdl.handle.net/1721.1/108020 Lima, Eduardo A. and Weiss, Benjamin P.“Ultra-High Sensitivity Moment Magnetometry of Geological Samples Using Magnetic Microscopy.” Geochemistry, Geophysics, Geosystems 17, no. 9 (September 2016): 3754–3774. https://orcid.org/0000-0003-3113-3415 en_US http://dx.doi.org/10.1002/2016GC006487 Geochemistry, Geophysics, Geosystems Creative Commons Attribution-Noncommercial-Share Alike http://creativecommons.org/licenses/by-nc-sa/4.0/ application/pdf American Geophysical Union (AGU) arXiv
spellingShingle Lima, Eduardo A.
Weiss, Benjamin P.
Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy
title Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy
title_full Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy
title_fullStr Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy
title_full_unstemmed Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy
title_short Ultra-high sensitivity moment magnetometry of geological samples using magnetic microscopy
title_sort ultra high sensitivity moment magnetometry of geological samples using magnetic microscopy
url http://hdl.handle.net/1721.1/108020
https://orcid.org/0000-0003-3113-3415
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