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Crystallite size was estimated from XRD peak broadening using the Scherrer calculation [64]: where d is crystallite diameter, λ is the wavelength of the X-rays, B is the peak breadth of the XRD peak, and θ B is the Bragg angle (in radians).
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However, the Williamson–Hall (W H) analysis is a simplified integral breadth method employed for estimating crystallite size and lattice strain, considering the peak width as a function of 2θ [15].
Williamson–Hall analysis is a simplified integral breadth method employed for estimating crystal, crystallite size and lattice strain, considering the peak width as a function of 2θ [39].
Williamson–Hall analysis is a simplified integral breadth method employed for estimating crystal, crystallite size and lattice strain, considering the peak width as a function of 2θ (Sundeep et al. 2016).
Williamson-Hall (W-H) analysis is a simplified integral breadth method where both size-induced and strain-induced broadening are deconvoluted by considering the peak width as a function of 2[14].
The size of the crystal grain was obtained from the peak width of X-ray diffraction using the two major models known and employed in bulk materials: the integral breadth and the Warren Averbach methods.
The peaks position and half peak breadth of XRD are in concordance with those measured in GCs, which indicates that nano-particles are released from glass matrix to aqueous solution.
In general, the increases in tan δ peak temperature, tan δ peak breadth, and room temperature modulus with increasing TEOS content are similar to those observed with POSS and VSQ.
The edge of a continent, it is the largest outcrop on the west coast of North America; the biggest Pacific island east of New Zealand – 290 miles long, 50 miles wide at peak breadth.
Coherent domain size is extracted from crystalline peak breadths obtained from the refinement [ 29] and is the average distance over which the crystalline cellulose is free of structural defects.
It was also found that particle size was quite small from the relatively wide half-peak breadth.
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