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A morphological transition is observed as film thickness increases from the first few foundational layers to films containing five or more layers.
As the value of U is increased, a progressive morphological transition is observed from the dendritic-plume structure to discrete spherical plumes, accompanied with thickening of the plumes and an increase in the plume spacing.
This morphological transition is fully reversible as determined by TEM and rheology studies and occurs because of a subtle change in the packing parameter for the copolymer chains.
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The rheological measurements indicated that a special rheological percolation (named as morphology rheological percolation) which closely relate to the morphological transition was very differ from the rheological percolation which closely relate to the formation of the rheological network.
The mechanism of the morphological transition was due to the LiCl loaded in different ion-dissolving blocks.
This morphological transition was reversible, as demonstrated by several water-to-acetone and acetone-to-water solvent changes.
This morphological transition was confirmed by TEM studies of the dried diluted aqueous dispersions (see Figure 2 a and 2 b).
Since the early aggregate stage is critical for multicellular development and apparently for differential gene regulation during chimeric development, we examined how candidate genes important in this morphological transition are regulated in chimera vs. clone.
raddiana (also considered as a separate species: A. raddiana Savi); but since gradual morphological transitions are found and desert dwellers shape the very morphology of trees and bushes by their management strategies [6], we refer to A. tortilis at the species level.
However, we refer to A. tortilis at the species level because gradual morphological transitions are found and desert dwellers shape the very morphology of trees (see below). A. tortilis is the dominant tree species in the mountainous landscape of the ED and is confined to seasonally dry river-valleys, wadis, where soil moisture conditions permits its establishment and continued growth.
Theoretical calculations on critical thicknesses of the morphological transitions are reported in[5 7] and experimental data in[8 10]; numerous data were summarized in review papers[11 13].
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