In-situ high temperature XRD studies and crystallization behavior of a Ti-rich Ti-Ni-Cu ribbon

Author(s):  
Wenjun He ◽  
Guanghui Min ◽  
Oleg Tolochko
2008 ◽  
Vol 31 (3) ◽  
pp. 573-577 ◽  
Author(s):  
Preetam Singh ◽  
Ashvani Kumar ◽  
Ajay Kaushal ◽  
Davinder Kaur ◽  
Ashish Pandey ◽  
...  

2021 ◽  
pp. 101-104
Author(s):  
S. H. Lim ◽  
C. S. Chua ◽  
Brian T. M. Ong ◽  
Coryl Jing Jun Lee ◽  
Dennis Cheng Cheh Tan ◽  
...  

2005 ◽  
Vol 398 (1-2) ◽  
pp. 156-164 ◽  
Author(s):  
A. Teresiak ◽  
A. Gebert ◽  
M. Savyak ◽  
M. Uhlemann ◽  
Ch. Mickel ◽  
...  

2016 ◽  
Vol 840 ◽  
pp. 375-380
Author(s):  
Meor Yusoff Meor Sulaiman ◽  
Khaironie Mohamed Takip ◽  
Ahmad Khairulikram Zahari

The high temperature phase transition of zirconia produced from commercial zirconyl chloride chemical was compared with that produced from a Malaysian zircon mineral. Zirconyl chloride was produced from zircon by using the hydrothermal fusion method. Initial XRD diffractogram of these samples at room temperature show that they are of amorphous structure. High temperature XRD studies was then performed on these samples; heated up to 1500°C. The XRD diffractograms shows that the crystalline structure of tetragonal zirconia was first observed and the monoclinic zirconia becomes more visible at higher heating temperature.


1985 ◽  
pp. 331-338 ◽  
Author(s):  
S. S. Iyengar ◽  
P. Engler ◽  
M. W. Santana ◽  
E. R. Wong

1984 ◽  
Vol 28 ◽  
pp. 331-338 ◽  
Author(s):  
S. S. Iyengar ◽  
P. Engler ◽  
M. W. Santana ◽  
E. R. Wong

Thermal analysts have exploited the sensitivity of carbonate mineral decomposition to furnace atmosphere as a diagnostic tool for identifying and quantifying these minerals in mixtures and solid solutions (1-3). However, thermal analysis techniques alone cannot reveal information about the reaction products after each thermal event. In-situ high temperature x-ray diffraction is one technique that can identify these products. Using this technique, Kissinger et al. (4) identified the reaction products of the thermal decomposition of reagent grade FeCO3 (siderite) and MgCO3 (magnesite). However, the thermal behavior of analytical reagent grade carbonates differs from natural minerals (1). Milodowski and Morgan (5) used in-situ XRD to investigate the thermal behavior of the dolomite-ankerite series.


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