SAXS study of ion tracks in San Carlos olivine and Durango apatite

B. Afra; M. D. Rodriguez; M. Lang; R. C. Ewing; N. Kirby; C. Trautmann; P. Kluth

doi:10.1016/j.nimb.2012.03.007

SAXS study of ion tracks in San Carlos olivine and Durango apatite

B. Afra^*, M. D. Rodriguez, M. Lang, R. C. Ewing, N. Kirby, C. Trautmann, P. Kluth

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

15 Citations (Scopus)

Abstract

Ion tracks were generated in crystalline San Carlos olivine (Mg,Fe) ₂SiO ₄ and Durango apatite Ca ₁₀(PO ₄) ₆F ₂ using different heavy ions ( ⁵⁸Ni, ¹⁰¹Ru, ¹²⁹Xe, ¹⁹⁷Au, and ²³⁸U) with energies ranging between 185 MeV and 2.6 GeV. The tracks and their annealing behavior were studied by means of synchrotron based small angle X-ray scattering in combination with in situ annealing. Track radii vary as a function of electronic energy loss but are very similar in both minerals. Furthermore, the annealing behavior of the track radii has been investigated and preliminary results reveal a lower recovery rate of the damaged area in olivine compared with apatite.

Original language	English
Pages (from-to)	243-246
Number of pages	4
Journal	Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms
Volume	286
DOIs	https://doi.org/10.1016/j.nimb.2012.03.007
Publication status	Published - 1 Sept 2012

Access to Document

10.1016/j.nimb.2012.03.007

Cite this

@article{a68acdc979604419afeaf97944072538,

title = "SAXS study of ion tracks in San Carlos olivine and Durango apatite",

abstract = "Ion tracks were generated in crystalline San Carlos olivine (Mg,Fe) 2SiO 4 and Durango apatite Ca 10(PO 4) 6F 2 using different heavy ions ( 58Ni, 101Ru, 129Xe, 197Au, and 238U) with energies ranging between 185 MeV and 2.6 GeV. The tracks and their annealing behavior were studied by means of synchrotron based small angle X-ray scattering in combination with in situ annealing. Track radii vary as a function of electronic energy loss but are very similar in both minerals. Furthermore, the annealing behavior of the track radii has been investigated and preliminary results reveal a lower recovery rate of the damaged area in olivine compared with apatite.",

keywords = "Apatite, Ion track annealing, Ion tracks, Minerals, Olivine, SAXS",

author = "B. Afra and Rodriguez, \{M. D.\} and M. Lang and Ewing, \{R. C.\} and N. Kirby and C. Trautmann and P. Kluth",

year = "2012",

month = sep,

day = "1",

doi = "10.1016/j.nimb.2012.03.007",

language = "English",

volume = "286",

pages = "243--246",

journal = "Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms",

issn = "0168-583X",

publisher = "Elsevier B.V.",

}

TY - JOUR

T1 - SAXS study of ion tracks in San Carlos olivine and Durango apatite

AU - Afra, B.

AU - Rodriguez, M. D.

AU - Lang, M.

AU - Ewing, R. C.

AU - Kirby, N.

AU - Trautmann, C.

AU - Kluth, P.

PY - 2012/9/1

Y1 - 2012/9/1

N2 - Ion tracks were generated in crystalline San Carlos olivine (Mg,Fe) 2SiO 4 and Durango apatite Ca 10(PO 4) 6F 2 using different heavy ions ( 58Ni, 101Ru, 129Xe, 197Au, and 238U) with energies ranging between 185 MeV and 2.6 GeV. The tracks and their annealing behavior were studied by means of synchrotron based small angle X-ray scattering in combination with in situ annealing. Track radii vary as a function of electronic energy loss but are very similar in both minerals. Furthermore, the annealing behavior of the track radii has been investigated and preliminary results reveal a lower recovery rate of the damaged area in olivine compared with apatite.

AB - Ion tracks were generated in crystalline San Carlos olivine (Mg,Fe) 2SiO 4 and Durango apatite Ca 10(PO 4) 6F 2 using different heavy ions ( 58Ni, 101Ru, 129Xe, 197Au, and 238U) with energies ranging between 185 MeV and 2.6 GeV. The tracks and their annealing behavior were studied by means of synchrotron based small angle X-ray scattering in combination with in situ annealing. Track radii vary as a function of electronic energy loss but are very similar in both minerals. Furthermore, the annealing behavior of the track radii has been investigated and preliminary results reveal a lower recovery rate of the damaged area in olivine compared with apatite.

KW - Apatite

KW - Ion track annealing

KW - Ion tracks

KW - Minerals

KW - Olivine

KW - SAXS

UR - http://www.scopus.com/inward/record.url?scp=84865507375&partnerID=8YFLogxK

U2 - 10.1016/j.nimb.2012.03.007

DO - 10.1016/j.nimb.2012.03.007

M3 - Article

SN - 0168-583X

VL - 286

SP - 243

EP - 246

JO - Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms

JF - Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms

ER -

SAXS study of ion tracks in San Carlos olivine and Durango apatite

Abstract

Access to Document

Other files and links

Fingerprint

Cite this