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The result demonstrates that the sample prepared with a P123/TBOT mole ratio of 0.6 clearly shows a main peak at 0.2° to 0.25°, thus revealing the presence of a hexagonal phase mesostructure.
The SAED pattern demonstrates that the sample is also in polycrystal feature with α-Fe2O3 phase.
Figure 3 demonstrates that the sample synthesized in this work is not stable under cathode conditions.
No characteristic peak of any impurity is probed, which demonstrates that the sample fabricated by this method has high phase purity.
The standard Hall measurement demonstrates that the sample is n-type at room temperature, i.e. electrons are the main carriers contributing to transport.
Although the sample S3 and S4 have similar porous structure, the SAED patterns of the samples are changed and the ring patterns of S4 can be indexed as a cubic spinel phase of magnetite, which demonstrates that the sample S4 are in Fe3O4 phase.
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It demonstrates that the samples are composed of amorphous and crystalline forms.
Comparison of the materials with identical content, but based on the different matrices, demonstrates that the samples with the IPN PU/PHEMA are more hydrophilic than the samples based on PU.
Left triangle demonstrates that the samples are strongly occupied in Na+ + K+ field rather than Ca2+ + Mg2+ field, while the upper diagram indicates that almost all the samples fall near Cl− type, which explains the simple dissolution and evaporation dominance.
This demonstrates that the samples were distinguishable based on their overall gene expression profiles, that the samples were normalized consistently, and that there were no outlier samples (Figure 2A).
The plot demonstrates that the samples from each group clustered in different regions of three-dimensional space.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com