Determination of water content in silica nanopowder using wavelength-dispersive X-ray fluorescence spectrometer

2011 ◽  
Vol 99 (2) ◽  
pp. 332-338 ◽  
Author(s):  
Yong Suk Choi ◽  
Jong-Yun Kim ◽  
Suk Bon Yoon ◽  
Kyuseok Song ◽  
Young Jin Kim
1981 ◽  
Vol 14 (6) ◽  
pp. 451-454 ◽  
Author(s):  
A. Yücel ◽  
M. Rautureau ◽  
D. Tchoubar ◽  
C. Tchoubar

A calculation method for the X-ray profiles from small, needle-like crystallites [Yücel, Rautureau, Tchoubar & Tchoubar (1980). J. Appl. Cryst. 13, 370–374] is applied to natural Eskisehir sepiolite mineral. By analysing the hk0 reflections, quantitative results are given on the average cross-sectional dimensions, their distribution, preferred directions of growth, lattice parameters, hydration state, and imperfections. Practical methods for the determination of the zeolitic water content and the importance of boundary effects are proposed.


2013 ◽  
Vol 544 ◽  
pp. 445-449
Author(s):  
Ran Yan ◽  
Yu Bing Liu ◽  
Ping Dai

When an X-ray photon which is generated by the sample enters into the detector, pulses can be produced and recorded. The detector is unable to respond to another photon that enters at the same time when a photon is being detected. The time that the detector takes to respond to a photon is regarded as dead time. For the x-ray fluorescence detector, the recorded count is less than the real count impulse due to dead time. Hence, to correct x-ray intensity of samples whose element content is vastly different, determination of dead time is necessary. In this paper, a new and complete way to determine dead time is proposed, which can be summarized as “intensity pair method”. Three “intensity pairs” were used for determining dead time, which were “intensity pair” of collimators (S2 and S4), “intensity pair” of spectral lines (Kα and Kβ) and “intensity pair” of beads with different flux-sample ratio (higher SH and lower SL analyte content in the beads). It comes to a conclusion that dead time obtained from “intensity pair” of beads is the most practical method for correcting X-ray fluorescence intensity. As for routine analysis, the dead time of proportional counter can be accurate to 1×10-9s, which can make intensity correction error less than 0.1%.


RSC Advances ◽  
2016 ◽  
Vol 6 (11) ◽  
pp. 9002-9006 ◽  
Author(s):  
Xiaofeng Lin ◽  
Shun-Xing Li ◽  
Feng-Ying Zheng

An integrative field analytical system was developed for the determination of Pb(ii) and Cd(ii).


2017 ◽  
Vol 726 ◽  
pp. 85-89
Author(s):  
Lei Zhang ◽  
Man Li ◽  
Hai Jian Li ◽  
Xin Song

Energy dispersive X-ray fluorescence spectrometry (EDXRF) allows a rapid determination of the concentration of elemental constituents or the thickness of thin film, it has been widely used in the industry of thin film thickness. But for multilayer film, especially the middle layer, with the absorption and enhance effect of other layers, the thickness and intensity of the middle layer is not a linear relationship. This paper reports a quantitative analysis of multilayer film thicknesses based on the use of EDXRF and fundamental parameters method. The thickness of multilayer film can be easily determined with the CTCFP software because it requires a minimum number of pure elementals only. Analysis of double-layer thin films using the CTCFP software shows that the inter-element and inter-layer X-ray absorptions and enhancements in a specimen have been determined properly. Results obtained on the standards confirmed the accuracy of the method.


2001 ◽  
Vol 16 (4) ◽  
pp. 224-226 ◽  
Author(s):  
G. Vanhoyland ◽  
M. K. Van Bael ◽  
J. Mullens ◽  
L. C. Van Poucke

The anhydrous acid strontium oxalate Sr(HC2O4)⋅½(C2O4) was obtained by thermal decomposition of the hydrated acid strontium oxalate Sr(HC2O4)⋅½(C2O4)⋅H2O. This non-hygroscopic compound crystallizes in the space group P 21/c (No. 14) with unit cell parameters: a=0.796 61(7) nm, b=0.9205(1) nm, c=0.731 98(8) nm, and β=102.104(8)°. Final refinement of the X-ray powder data yielded RB=3.2% and Rwp=11.1% (background-corrected data). In this structure, Sr is eight-fold coordinated by O. These polyhedra are connected together by edge-sharing to form two-dimensional (2D) layers along the bc-plane, which means that there is an increased dimensionality from 1D to 2D with decreasing water content of the acid oxalates.


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