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Prepare this assignment according to the guidelines found in the APA Style Guide


Prepare this assignment according to the guidelines found in the APA Style Guide. An abstract is required. Figure 1a shows the XRD patterns for pristine ME100, ME100-ODTMA and the corresponding patterns of Hy3078/ME100-ODTMA nanocomposites with various amounts of ME100-ODTMA in the diffraction angle range 2θ = 2–10°. Diffraction ranging from 2θ = 2–10° indicated an intercalated hybrid or an immiscible system. The 001 diffraction peak indicated for ME100 appeared at 2θ = 7–10°, of which the interlayer distance was 1.24nm. The presence of alkylammonium ions in the basal spacing reduced the attractive forces between the clay and enabled the polymer to be intercalated into the clay-polymer easing up clay distribution. an increase in intercalated structures with organoclay content and pristine clay caused smaller interlayer distances, which might have impeded the higher basal spacing or exfoliation of individual silicate layers.25 Figure 1b represents XRD patterns for pristine WXFN, WXFN-ODTMA and the corresponding patterns of

Hy3078/WXFN-ODTMA nanocomposites. The interlayer gallery height for the pristine WXFN, Distanced (001) between XRD and an individual layer of silicate thickness ( ? 1 nm), was 1.28 nm (2θ = 6.90°). The XRD profile of Hy3078 composites of the silicate reflected a disruption of silicate layers in the Hy3078/WXFN matrix, but in the case of Hy3078/WXFN-ODTMA with 4wt% clay content, it indicated an unorderly added structure with a (001) plane peak at 2θ = 2.40° (= 3.68 nm). In Figure 1c, the XRD profile of the pristine

WXFP and their respective composites showed the same trend as that of WXFN. This is an indication that as the clay content increases, the mobility of the nanofiller is decreased, providing the low driving force for the intercalated polymer to break the tactoids. However, 2ME100-ODTMA showed orderly diffraction peaks in comparison to ME100, associated with interlayer distances of k4.7, 2.2, and 1.6 nm, respectively. Extra peaks were as a result of longer-range registration and interstratified superstructure&nbsp.of the largest ME100 synthetic clay, which originates from a well-published inherent charge heterogeneity. This charge heterogeneity might have allowed various wetter chains to add to the fluoromics layers making monolayer-bilayer or bilayer pseudo-triple-layer arrangements possible.

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