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Electron probe sub-micron analysis i...
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ProQuest Information and Learning Co.
Electron probe sub-micron analysis in geoscience : = Problems and potential solutions of low voltage electron microprobe analysis, as applied to reduced lunar phases and pyroxene lamellae.
Record Type:
Language materials, manuscript : Monograph/item
Title/Author:
Electron probe sub-micron analysis in geoscience :/
Reminder of title:
Problems and potential solutions of low voltage electron microprobe analysis, as applied to reduced lunar phases and pyroxene lamellae.
Author:
Gopon, Phillip N.
Description:
1 online resource (201 pages)
Notes:
Source: Dissertation Abstracts International, Volume: 78-01(E), Section: B.
Contained By:
Dissertation Abstracts International78-01B(E).
Subject:
Geology. -
Online resource:
click for full text (PQDT)
ISBN:
9781369098891
Electron probe sub-micron analysis in geoscience : = Problems and potential solutions of low voltage electron microprobe analysis, as applied to reduced lunar phases and pyroxene lamellae.
Gopon, Phillip N.
Electron probe sub-micron analysis in geoscience :
Problems and potential solutions of low voltage electron microprobe analysis, as applied to reduced lunar phases and pyroxene lamellae. - 1 online resource (201 pages)
Source: Dissertation Abstracts International, Volume: 78-01(E), Section: B.
Thesis (Ph.D.)
Includes bibliographical references
Conventional electron-probe microanalysis (EPMA) has an X-ray analytical spatial resolution on the order of 1-4 mum width/depth. Many of the naturally occurring Fe-Si compounds analyzed in this study are smaller than 1 im in size, requiring the use of lower accelerating potentials and non-standard X-ray lines for analysis. The problems with the use of low energy Xray lines (soft X-rays) of iron for quantitative analyses are discussed and a review is given of the alternative X-ray lines that may be used for iron at or below 5 keV (i.e., accelerating voltage that allows analysis of areas of interest smaller than 1 mum). Problems include the increased sensitivity to surface effects for soft X-rays, peak shifts (induced by chemical bonding, differential selfabsorption, and/or buildup of carbon contamination), uncertainties in the mass attenuation coefficient (MAC) for X-ray lines near absorption edges, and issues with spectral resolution and count rates from the available Bragg diffractors. In addition to the results from the traditionally used Fe Lalpha line, alternative approaches, utilizing Fe Lbeta, and Fe Ll-n lines, are discussed.
Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2018
Mode of access: World Wide Web
ISBN: 9781369098891Subjects--Topical Terms:
670379
Geology.
Index Terms--Genre/Form:
554714
Electronic books.
Electron probe sub-micron analysis in geoscience : = Problems and potential solutions of low voltage electron microprobe analysis, as applied to reduced lunar phases and pyroxene lamellae.
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Problems and potential solutions of low voltage electron microprobe analysis, as applied to reduced lunar phases and pyroxene lamellae.
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1 online resource (201 pages)
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Source: Dissertation Abstracts International, Volume: 78-01(E), Section: B.
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Advisers: John W. Valley; John H. Fournelle.
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Thesis (Ph.D.)
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The University of Wisconsin - Madison
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2016.
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Includes bibliographical references
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Conventional electron-probe microanalysis (EPMA) has an X-ray analytical spatial resolution on the order of 1-4 mum width/depth. Many of the naturally occurring Fe-Si compounds analyzed in this study are smaller than 1 im in size, requiring the use of lower accelerating potentials and non-standard X-ray lines for analysis. The problems with the use of low energy Xray lines (soft X-rays) of iron for quantitative analyses are discussed and a review is given of the alternative X-ray lines that may be used for iron at or below 5 keV (i.e., accelerating voltage that allows analysis of areas of interest smaller than 1 mum). Problems include the increased sensitivity to surface effects for soft X-rays, peak shifts (induced by chemical bonding, differential selfabsorption, and/or buildup of carbon contamination), uncertainties in the mass attenuation coefficient (MAC) for X-ray lines near absorption edges, and issues with spectral resolution and count rates from the available Bragg diffractors. In addition to the results from the traditionally used Fe Lalpha line, alternative approaches, utilizing Fe Lbeta, and Fe Ll-n lines, are discussed.
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Ann Arbor, Mich. :
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ProQuest,
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2018
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Mode of access: World Wide Web
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Geology.
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ProQuest Information and Learning Co.
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click for full text (PQDT)
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