scholarly journals Novel application of X-ray fluorescence microscopy (XFM) for the non-destructive micro-elemental analysis of natural mineral pigments on Aboriginal Australian objects

The Analyst ◽  
2016 ◽  
Vol 141 (12) ◽  
pp. 3657-3667 ◽  
Author(s):  
Rachel S. Popelka-Filcoff ◽  
Claire E. Lenehan ◽  
Enzo Lombi ◽  
Erica Donner ◽  
Daryl L. Howard ◽  
...  

This manuscript presents the first comprehensive non-destructive micro elemental characterisation of mineral pigments used on Aboriginal Australian objects.

2020 ◽  
Author(s):  
Avupati Venkata Surya Satyanarayana ◽  
Mokka Jagannadharao ◽  
Kemburu Chandra Mouli ◽  
Kollu Sai Satya Mounika

Abstract. Particle Induced X-ray Emission (PIXE) has been applied to a analytical tool for long range of major, minor and trace elemental analysis in Precambrian charnockites. PIXE is sensitive and non-destructive method for some elemental analysis in a variety of Precambrian charnockite rocks down to levels of a few parts per million and it is not valid for all remaining elements in the composition. The elements identified in the Precambrian charnokite rock are Cl, K, Ca, Ti, V, Cr, Mn, Fe, Ni, Cu, Zn, Se, Br, Rb, Sr, Y, Zr, Nb, Mo, Ru, Ag, Pb are identified without exact values by PIXE but the elements minor F, major elements Na, Mg, Al, Si, P and Ba and traces of Co, Th and U not detected due to various reasons even though there present in the charnockites, because of PIXE which is operation at 3 MeV energy and characterization material of charnockite mineral investigated. In mineral characterization of charnockite rocks, elemental errors in concentration of the compositions explained by comparing with present and previous studies.


2003 ◽  
Vol 13 (03n04) ◽  
pp. 149-161 ◽  
Author(s):  
N. K. PURI ◽  
M. HAJIVALIEI ◽  
S. C. BEDI ◽  
N. SINGH ◽  
I. M. GOVIL ◽  
...  

As part of the study of trace elemental analysis of ancient Indian coins, twenty-five coins belonging to medieval period (11th-14th century A.D) and fifty-nine coins belonging to Kusanas (78-250 A.D) from India have been analysed using Proton Induced X-ray Emission (PIXE) technique. The elements S , Ca , Fe , Cu , Ag , Sn , Pb were detected in 11th-14th century A.D. coins while elements namely S , Cl , K , Ca , Ti , Cr , Mn , Fe , Ni , Cu , As and Zn were detected in most of the Kusanas coins. Based on the elemental analysis different hypotheses put forward in the earlier literature were examined. The presence of Pb determined in medieval period coins does not rule out the utilization of local source of silver extracted from argentiferous galena instead of the Faranjal mines of Afghanistan as normally accepted. From the consistent concentration of Ag in these coins despite the change of Kingdoms it is confirmed that beside the rulers the commercial communities had a great influence in the currency of medieval period. This is the first attempt where reasonable number of ancient coins belonging to different periods were analysed by modern non destructive multi-elemental technique such as PIXE and has put the importance of the elemental analysis of ancient Indian coins in the proper perspective.


1983 ◽  
Vol 7 (2) ◽  
pp. 99-113 ◽  
Author(s):  
James L. Enyeart ◽  
Adelaide B. Anderson ◽  
Steven J. Perron ◽  
D. K. Rollins ◽  
Quintus Fernando

2014 ◽  
Vol 5 (1) ◽  
pp. 752-756
Author(s):  
Amir Pishkoo

In this study Proton Induced X-ray Emission (PIXE) and Rutherford Backscattering Spectrometry (RBS) as reliable and non-destructive techniques has been applied to compare thickness, major and trace elements of different brands of CD-R discs. Three elements, namely Ag, Ba, and Ti were found to be the major elements.


1974 ◽  
Vol 18 ◽  
pp. 598-605
Author(s):  
J. William Nelson ◽  
Dennis L. Meinert

AbstractProton scattering quantitative elemental analysis is examined as a complement to proton induced X-ray emission analysis for air particulate samples. Both methods are absolute, non-destructive, and are suitable for use on samples up to about 1 mg/cm2 in areal density. Characteristics of the method are discussed and examples of aerosol spectra are presented.


2018 ◽  
Vol 32 (2) ◽  
Author(s):  
Pungky Sampurno ◽  
Rina Zuraida ◽  
Nazar Nurdin ◽  
Luli Gustiantini ◽  
Noor Cahyo Dwi Aryanto

Study of elemental composition in sediment has been proven useful in interpreting the depositional environmental changes. Multi Sensor Core Logger (MSCL) is a non-destructive analysis that measures several parameters in sediment core including magnetic susceptibility and elemental composition. Magnetic susceptibility and elemental analysis were measured in four selected marine sediment cores from western part of Bangka Strait (MBB-67. MBB-119, MBB-120 and MBB-173) by using magnetic susceptibility and X-ray Fluorescence (XRF) sensors attached to the MSCL. The data was collected within 2 cm interval. Scatter plots of Y/Zr and Zr/Ti show singular trend demonstrated by sediments from MBB-173 and two groups that composed of MBB-67 (Group 1) and MBB-119 + MBB-120 (Group 2). MBB-67 that is located adjacent to Klabat Granite shows upward changes in mineralogy, slight increase of grain size and negligible change in Y concentration. Cores MBB-119 and MBB-120 are inferred to be deposited during regression that resulted in the accummulation of Y-bearing zircon in MBB-119 before the mineral could reach MBB-120. Core MBB-173 is interpreted to be the product of plagioclase weathering that is submerged by rising sea level. This core contains a horizon of rich Y-bearing zircon at 60 cm.Keywords: Multi Sensor Core Logger, X-Ray Fluorescence, magnetic susceptibility, depositional environment, Bangka Island Studi tentang komposisi unsur kimia dalam sedimen telah terbukti bermanfaat dalam interpretasi perubahan lingkungan pengendapan. Multi Sensor Core Logger (MSCL) adalah sebuah analisis yang non-destructive, untuk mengukur beberapa parameter dalam bor sedimen termasuk suseptibilitas magnetik dan kandungan unsur. Suseptibilitas magnetik dan kandungan unsur diukur dari 4 bor sedimen laut yang terpilih di bagian barat Selat Bangka (MBB-67. MBB-119, MBB-120 and MBB-173) dengan menggunakan sensor suseptibilitas magnetik (MS) dan X-ray Fluorescence (XRF) yang terpasang pada MSCL. Pengukuran dilaksanakan dengan interval 2 cm. Plot Y/Zr dan Zr/Ti menunjukkan satu trend yang diperlihatkan oleh sedimen bor MBB-173 dan dua grup yang terdiri atas MBB-67 (Grup 1) dan MBB-119 + MBB-120 (Grup 2). Bor MBB-173 ditafsirkan sebagai hasil pelapukan plagioklas yang kemudian terendam air laut. Bor ini memperlihatkan horizon yang kaya akan zirkon pembawa yttrium pada kedalaman 60 cm.Kata kunci : Multi Sensor Core Logger, X-Ray Fluorescence, suseptibilitas magnetik, lingkungan pengendapan, Pulau Bangka


Metallomics ◽  
2019 ◽  
Vol 11 (1) ◽  
pp. 151-165 ◽  
Author(s):  
M. J. Hackett ◽  
A. Hollings ◽  
S. Caine ◽  
B. E. Bewer ◽  
M. Alaverdashvili ◽  
...  

X-ray fluorescence microscopy reveals unique elemental signatures within sub-populations of hippocampal pyramidal neurons.


2019 ◽  
Vol 21 ◽  
pp. 145
Author(s):  
E. Tsompopoulou ◽  
K. Mergia

Energy dispersive X-ray fluorescence spectroscopy (EDXRF) is a powerful non-destructive technique used to determine the elemental composition of materials. The current work focuses on the installation and optimization of the operation of the EDXRF system developed by Amptek Inc. Furthermore, XRF elemental analysis results of alloys candidate for fusion reactor applications are presented


Author(s):  
R. F. Egerton

An important parameter governing the sensitivity and accuracy of elemental analysis by electron energy-loss spectroscopy (EELS) or by X-ray emission spectroscopy is the signal/noise ratio of the characteristic signal.


Author(s):  
Brian Cross

A relatively new entry, in the field of microscopy, is the Scanning X-Ray Fluorescence Microscope (SXRFM). Using this type of instrument (e.g. Kevex Omicron X-ray Microprobe), one can obtain multiple elemental x-ray images, from the analysis of materials which show heterogeneity. The SXRFM obtains images by collimating an x-ray beam (e.g. 100 μm diameter), and then scanning the sample with a high-speed x-y stage. To speed up the image acquisition, data is acquired "on-the-fly" by slew-scanning the stage along the x-axis, like a TV or SEM scan. To reduce the overhead from "fly-back," the images can be acquired by bi-directional scanning of the x-axis. This results in very little overhead with the re-positioning of the sample stage. The image acquisition rate is dominated by the x-ray acquisition rate. Therefore, the total x-ray image acquisition rate, using the SXRFM, is very comparable to an SEM. Although the x-ray spatial resolution of the SXRFM is worse than an SEM (say 100 vs. 2 μm), there are several other advantages.


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