scholarly journals Modifying interfacial interparticle forces to alter microstructure and viscoelasticity of densely packed particle laden interfaces

2019 ◽  
Vol 536 ◽  
pp. 30-41 ◽  
Author(s):  
Syed Ehsanur Rahman ◽  
Nader Laal-Dehghani ◽  
Sourav Barman ◽  
Gordon F. Christopher
2020 ◽  
Vol 05 ◽  
Author(s):  
Silas Santos ◽  
Orlando Rodrigues ◽  
Letícia Campos

Background: Innovation mission in materials science requires new approaches to form functional materials, wherein the concept of its formation begins in nano/micro scale. Rare earth oxides with general form (RE2O3; RE from La to Lu, including Sc and Y) exhibit particular proprieties, being used in a vast field of applications with high technological content since agriculture to astronomy. Despite of their applicability, there is a lack of studies on surface chemistry of rare earth oxides. Zeta potential determination provides key parameters to form smart materials by controlling interparticle forces, as well as their evolution during processing. This paper reports a study on zeta potential with emphasis for rare earth oxide nanoparticles. A brief overview on rare earths, as well as zeta potential, including sample preparation, measurement parameters, and the most common mistakes during this evaluation are reported. Methods: A brief overview on rare earths, including zeta potential, and interparticle forces are presented. A practical study on zeta potential of rare earth oxides - RE2O3 (RE as Y, Dy, Tm, Eu, and Ce) in aqueous media is reported. Moreover, sample preparation, measurement parameters, and common mistakes during this evaluation are discussed. Results: Potential zeta values depend on particle characteristics such as size, shape, density, and surface area. Besides, preparation of samples which involves electrolyte concentration and time for homogenization of suspensions are extremely valuable to get suitable results. Conclusion: Zeta potential evaluation provides key parameters to produce smart materials seeing that interparticle forces can be controlled. Even though zeta potential characterization is mature, investigations on rare earth oxides are very scarce. Therefore, this innovative paper is a valuable contribution on this field.


2016 ◽  
Vol 28 (7) ◽  
pp. 2348-2355 ◽  
Author(s):  
Anish Rao ◽  
Soumendu Roy ◽  
Mahima Unnikrishnan ◽  
Sumit S. Bhosale ◽  
Gayathri Devatha ◽  
...  

Langmuir ◽  
1997 ◽  
Vol 13 (21) ◽  
pp. 5528-5530 ◽  
Author(s):  
Tadao Sugimoto ◽  
Tetsuya Takahashi ◽  
Hiroyuki Itoh ◽  
Shun-ichi Sato ◽  
Atsushi Muramatsu

Nature ◽  
1959 ◽  
Vol 183 (4660) ◽  
pp. 538-539 ◽  
Author(s):  
R. H. G. PARRY
Keyword(s):  

2016 ◽  
Vol 291 ◽  
pp. 473-486 ◽  
Author(s):  
Simon Maurer ◽  
Sergio R. Durán ◽  
Martin Künstle ◽  
Serge M.A. Biollaz

Author(s):  
Jeongki Lee ◽  
Dante Fratta ◽  
Idil Deniz Akin

We developed an experimental program to monitor how interparticle forces control fine-grained soils' mechanical behavior when saturation changes from the tightly adsorbed regime to saturation. The testing program uses stiffness (i.e., S-wave velocity) and strength (i.e., Brazilian tensile strength) tests on kaolinite, silica flour, and diatomaceous earth soil samples at very low confining stresses (< 5 kPa). Three fine-grained soils yield a range of different properties, including particle size, specific surface area, negative charge density, and internal/external particle porosity. Results show that shear stiffness and tensile strength follow similar trends, emphasizing that the same interparticle forces control the mechanical responses. In particular, the interpretation of S-wave velocity measurements shows three different behavior ranges: a van der Waals attraction range, a capillary-dominated interparticle forces range, and the continuous decrease in the capillary forces from the saturation at the air-entry pressure until full saturation. We show that the interparticle forces respond to a complex function of water content, particle size, particle separations, surface charge density, and the presence of internal particle porosity.


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