HIGH-ENERGY PROTON-BEAM ANALYSIS OF GEOLOGICAL-MATERIALS

Authors
Citation
Nm. Halden, HIGH-ENERGY PROTON-BEAM ANALYSIS OF GEOLOGICAL-MATERIALS, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 77(1-4), 1993, pp. 399-404
Citations number
22
Categorie Soggetti
Physics, Nuclear","Nuclear Sciences & Tecnology","Instument & Instrumentation
ISSN journal
0168583X
Volume
77
Issue
1-4
Year of publication
1993
Pages
399 - 404
Database
ISI
SICI code
0168-583X(1993)77:1-4<399:HPAOG>2.0.ZU;2-3
Abstract
Partitioning of trace elements between mineral phases reflects the phy sical, chemical and kinetic conditions of crystallization. Variations in environmental conditions during growth often result in complex and small-scale chemical zoning in minerals. The low abundance of trace el ements and their spatial inhomogeneity on a mum scale makes their anal ysis by a microprobe technique essential for addressing many petrologi cal problems. Mu-PIXE (2-3 MeV) has been successfully applied to many mineralogical problems and is rapidly becoming a routine analytical to ol for geologists. High-energy PIXE (40-60 MeV) provides a new dimensi on in mineralogical analysis. The K X-rays for many petrologically imp ortant trace elements occur in the 25-90 keV region, here the X-rays a re not affected by interference from the X-rays of more abundant geoch emically coherent elements. Furthermore, the K X-ray spectrum for an e lement is less complex than its corresponding L X-ray spectrum so data reduction is simplified. The use of high energy protons for elemental analysis makes high-energy PIGE accessible, here on-line emission of gamma-rays can be used to provide information on element (or in some c ases isotope) concentrations. For the analysis of chemically complex m aterials such as rocks and minerals it is necessary to thoroughly char acterize the material beforehand such that likely proton induced react ions can be predicted. Nuclear reactions produced by proton interactio n with mineral samples occur during on-line exposure of the sample. Th e by-products of such reactions may have significant half-lives which will make them amenable to off-line analysis. One such case is where P t undergoes (p, xn) reactions to form Au which then decays back to Pt via electron capture. The off-line spectrum after such a run contains Au X-rays and the background to such spectra is low, which raises the possibility that this form of analysis will provide low detection limi ts. This is the proton analogue of neutron activation analysis - proto n activation analysis (PAA).