1991
DOI: 10.1016/0168-583x(91)95015-6
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Non-Rutherford 4He cross sections for ion beam analysis

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Cited by 30 publications
(4 citation statements)
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“…Measurements were performed at the Centro Nacional de Aceleradores (CNA) using a He + beam at the energy of 4250 KeV. At this energy, the cross section for Cr is "Rutherford" but that for C is "Non-Rutherford" [28] which would allow to have a better accuracy in the determination of the C content in the films. The backscattered ions were detected by a standard Si-barrier detector located at an angle of 165º to the beam direction.…”
Section: Elemental Composition and Structural Characterizationmentioning
confidence: 99%
“…Measurements were performed at the Centro Nacional de Aceleradores (CNA) using a He + beam at the energy of 4250 KeV. At this energy, the cross section for Cr is "Rutherford" but that for C is "Non-Rutherford" [28] which would allow to have a better accuracy in the determination of the C content in the films. The backscattered ions were detected by a standard Si-barrier detector located at an angle of 165º to the beam direction.…”
Section: Elemental Composition and Structural Characterizationmentioning
confidence: 99%
“…10 Although a boron ridge is not manifestly apparent from the experimental points of Fig. 10 Although a boron ridge is not manifestly apparent from the experimental points of Fig.…”
Section: Results and Analysesmentioning
confidence: 93%
“…For a standard backscattering energy for 4 He of 2 MeV, cross-sections for elements with Z greater than ~6 will be Rutherford, while for 2 MeV protons this value will be Z ~20; for 4 He of 4 MeV energy non-Rutherford behavior will be observed for elements with Z less than ~15. Departure from Rutherford scattering behavior often results in large increases in scattering cross-sections; a good example is the non-Rutherford scattering cross section of 4 He from 16 O for a 4 He energy just above 3 MeV (e.g., Cheng et al 1993;Leavitt and McIntyre 1991;Demarche and Terwagne 2006) where scattering cross-sections are more than an order of magnitude greater than Rutherford values. While these enhanced cross-sections have not yet found significant direct use in diffusion studies in minerals, they have been exploited to supplement other measurements, as in the study of Cherniak (2000), where non-Rutherford a scattering from 28 Si at 6.6 MeV was used to explore substitutional processes involved in REE diffusion in fluorapatite.…”
Section: Depth and Mass Resolutionmentioning
confidence: 99%