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Abstract

This paper demonstrates a non-destructive technique to evaluate the internal microstructure in the Sn-Ag-Cu (SAC) solder joint through synchrotron X-ray radiation tomography. Synchrotron X-ray tomography is increasingly utilized for characterizing the internal microstructure of materials in 3D images. A 3D model is reconstructed from a set of 2D projection images taken from different angles and angular position during the sample rotation, thus it could provide a more comprehensive description of the microstructure of an alloy compared to 2D images. In this paper, it is successfully observed and evaluated the internal microstructure of a 900 μm solder joint sample. The key principles and methods of synchrotron X-ray tomography are briefly described. Examples of quantitative and qualitative assessments on the grain refinement effect of Mg addition to SAC35 solder joint are also presented in this paper.
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Authors and Affiliations

C.Y. Tan
1
ORCID: ORCID
M.A.A. Mohd Salleh
1
N. Saud
1
ORCID: ORCID
M. Nabialek
2
ORCID: ORCID
A. Rylski
3
ORCID: ORCID

  1. Universiti Malaysia Perlis, Centre of Excellent on Geopolymer and Green Technology (CEGeoGTech), 02600 Perlis, Malaysia
  2. Czestochowa University of Technology, Department of Physics, Faculty of Production Engineering and Materials Technology,42-200 Czestochowa, Poland
  3. Lodz University of Technology, Institute of Materials Science and Engineering, 90-924 Lodz, Poland
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Abstract

Dolomite can be used as a source of aluminosilicate to produce geopolymers; however, this approach is limited by its low reactivity. This study analyzes the viability of producing geopolymers using dolomite/fly-ash with sodium silicate and NaOH solutions (at multiple concentrations) by determining the resultant geopolymers’ compressive strengths. The dolomite/fly-ash-based geopolymers at a NaOH concentration of ~22 M resulted in an optimum compressive strength of 46.38 MPa after being cured for 28 days, and the SEM and FTIR analyses confirmed the denser surface of the geopolymer matrix. The synchrotron micro-XRF analyses confirmed that the Ca concentration exceeded that of Si and Mg, leading to the formation of calcium silicate hydrate, which strengthens the resulting geopolymers.
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Authors and Affiliations

Emy Aizat Azimi
1
M.A.A. Mohd Salleh
1
Mohd Mustafa Al Bakri Abdullah
1
ORCID: ORCID
Ikmal Hakem A. Aziz
1
ORCID: ORCID
Kamarudin Hussin
1
ORCID: ORCID
Jitrin Chaiprapa
2
ORCID: ORCID
Petrica Vizureanu
3
ORCID: ORCID
Sorachon Yoriya
4
ORCID: ORCID
Marcin Nabiałek
5
ORCID: ORCID
Jerzy J. Wyslocki
5
ORCID: ORCID

  1. Universiti Malaysia Perlis (Unimap), Centre of Excellence Geopolymer and Green Technology (CeGeoGTech), Perlis, Malaysia
  2. Synchrotron Light Research Institute (SLRI), 111 University Avenue, Muang District, Nakhon Ratchasima 30000, Thailand
  3. ”Gheorghe Asachi” Technical University, Faculty of Materials Science and Engineering, Blvd. D. Mangeron 71, 700050 Lasi, Romania
  4. National Metal and Materials Technology Center (MTEC), 114 Thailand Science Park, Phaholyothin Road, Klong 1, Klongluang, Pathumthani 12120, Thailand
  5. Czestochowa University of Technology, Department of Physics, 42-200, Czestochowa, Poland

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