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As shown in Figure S4a in the Supporting Information, the X-ray traces of as-cast films of 6,6′- and 5,5′-substituted isoindigo derivatives show a primary reflection at 0.42 Å–1 for 6,6′ -BT and 5,5′ -BT, and at 0.41 Å–1 for 6,6′ -BZ.
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The pattern displays a high intensity primary reflection at 2.37° of d spacing = 3.72 nm which confirms the hexagonal structure.
A very weak primary reflection at 0.41 Å–1 is observed in the X-ray trace of 5,5′ -BZ.
However, if reverberating events are appearing in the same depth and location as the primary reflection of a target of interest, this may be considered to degrade the ultrasound image quality.
This is an indication that these are primary reflection events.
Presenting the data for both crystals as a function of azimuth about the 2.05 2.05 2.05 primary reflection reveals the complex interaction between the DMS and the CTR.
They are mostly as a result of sedimentations at depth which yield reflection events with almost similar time of arrival as the primary reflection events, such that any time a seismic section becomes indistinct at greater depth, it is hypothesized that the data have become overwhelmed by short-path multiples and could be investigated (www.Stanford.edu/sep/prof/iei; Retailleau et al. 2002).
On the other hand, when a secondary reflection acts as the source for a tertiary reflection emerging in the direction of the primary reflection, the intensity can be modified by constructive or destructive interference.
Primary reflection examines its object by abstraction, by analytically breaking it down into its constituent parts.
The primary reflection mirror adopts paraboloidal mirror; the secondary mirror adopts hyperboloidal or ellipsoidal mirror.
Although secondary reflection is able to recoup the unity of experience that primary reflection dissects, it is possible that secondary reflection is frustrated.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com