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The hydrophobicity of the mineral particles is thus reduced and hence, their floatability [8].
(11) The mechanism for the formation of α particles is thus not yet clear.
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Palygorskite particles are thus likely to move preferentially over smectite and kaolinite downward in the soil profile, and eventually to clog soil pores.
Palygorskite particles are thus likely to move preferentially over smectite and kaolinite downwards in the soil profile, and eventually to clog soil pores.
The resulting particles are thus comprised of self-assembled monolayers of perfluorohexadecanoic acid (PFHD) (C15F31COOH) around the alumina (Al2O3) shell encapsulating the Al core.
Density and force are obtained by assuming that the particles have finite size, are tenuous, and may pass through one another; the particles are thus called clouds.
The experimentally observed two-phase microstructure for larger particles was thus primarily due to the growth of Ag-rich regions epitaxially on initially formed small fcc Ag Ni nanoparticles.
The particles are thus hydrophobically modified, resulting in phase inversion from w/o to w/o/w at higher water mass fraction, while for particles originating in ASA, the phase inverts from w/o to o/w at a lower water mass fraction.
The particles are thus stabilized by the capping agent like flavonoids and water soluble compounds present in the leaf extract [25].
These particles are thus seen to undergo an amorphous to crystalline transformation, the kinetics and completeness of which depend on the protein-to-mineral ratios, with low ratios favoring faster conversion to crystals.
These particles are thus obscured for SEM-EDX analysis and can only be analysed if the skin cells are destroyed or new systems such as backscattered electron imaging (BEI) are connected to the SEM.
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