Cobalt Nanocrystals Organized in Mesoscopic Scale

Author(s):  
Marie-Paule Pileni
2004 ◽  
Vol 108 (52) ◽  
pp. 20050-20055 ◽  
Author(s):  
Isabelle Lisiecki ◽  
Pierre-Antoine Albouy ◽  
Marie-Paule Pileni

2021 ◽  
Vol 103 (1) ◽  
Author(s):  
Leonardo R. Cadorim ◽  
Antonio R. de C. Romaguera ◽  
Isaías G. de Oliveira ◽  
Rodolpho R. Gomes ◽  
Mauro M. Doria ◽  
...  

Nano Letters ◽  
2021 ◽  
Author(s):  
Alberto Trentino ◽  
Jacob Madsen ◽  
Andreas Mittelberger ◽  
Clemens Mangler ◽  
Toma Susi ◽  
...  

2015 ◽  
Vol 27 (2) ◽  
pp. 544-549 ◽  
Author(s):  
Li-Bing Lv ◽  
Tian-Nan Ye ◽  
Ling-Hong Gong ◽  
Kai-Xue Wang ◽  
Juan Su ◽  
...  

Author(s):  
Florestan Schindler ◽  
Richard Brocker ◽  
Fritz Klocke ◽  
Patrick Mattfeld

Polycrystalline diamond (PCD) grinding takes an important role in the field of tool manufacture. Regardless, there is still lack of process knowledge about the occurring material removal mechanisms in PCD grinding. In order to get a better understanding of the process characteristics, the surface integrity zone of PCD inserts has been analyzed in detail after grinding for the first time. The drawn conclusion questions solely ductile or brittle behavior as removal mechanisms. Both thermal and mechanical process loads during the grinding process lead to thermophysical and chemical effects on a micro- and mesoscopic-scale and might thus have a significant impact on the material removal mechanism.


2021 ◽  
Vol 11 (11) ◽  
pp. 4817
Author(s):  
Filippos Vallianatos ◽  
Vassilis Sakkas

In the present work, a multiscale post-seismic relaxation mechanism, based on the existence of a distribution in relaxation time, is presented. Assuming an Arrhenius dependence of the relaxation time with uniform distributed activation energy in a mesoscopic scale, a generic logarithmic-type relaxation in a macroscopic scale results. The model was applied in the case of the strong 2015 Lefkas Mw6.5 (W. Greece) earthquake, where continuous GNSS (cGNSS) time series were recorded in a station located in the near vicinity of the epicentral area. The application of the present approach to the Lefkas event fits the observed displacements implied by a distribution of relaxation times in the range τmin ≈3.5 days to τmax ≈350 days.


Sign in / Sign up

Export Citation Format

Share Document