scholarly journals AN AUTOMATIC DELIVERY APPARATUS FOR FLUID MEDIA.

The Lancet ◽  
1916 ◽  
Vol 188 (4860) ◽  
pp. 716-717
Author(s):  
SydneyW. Cole
Keyword(s):  
1996 ◽  
Vol 260 (3-4) ◽  
pp. 441-446 ◽  
Author(s):  
A.J. Bain ◽  
P. Chandna ◽  
G. Butcher

Author(s):  
Arman Khalighi ◽  
Matthew Blomquist ◽  
Abhijit Mukherjee

In recent years, heat dissipation in micro-electronic systems has become a significant design limitation for many component manufactures. As electronic devices become smaller, the amount of heat generation per unit area increases significantly. Current heat dissipation systems have implemented forced convection with both air and fluid media. However, nanofluids may present an advantageous and ideal cooling solution. In the present study, a model has been developed to estimate the enhancement of the heat transfer when nanoparticles are added to a base fluid, in a single microchannel. The model assumes a homogeneous nanofluid mixture, with thermo-physical properties based on previous experimental and simulation based data. The effect of nanofluid concentration on the dynamics of the bubble has been simulated. The results show the change in bubble contact angles due to deposition of the nanoparticles has more effect on the wall heat transfer compared to the effect of thermo-physical properties change by using nanofluid.


Ultrasonics ◽  
1971 ◽  
Vol 9 (2) ◽  
pp. 124
Author(s):  
W. Mohring

2019 ◽  
Vol 34 ◽  
pp. 505-523 ◽  
Author(s):  
Maurizio Ribera d’Alcalà

Comparisons between terrestrial and marine ecosystems are generally not in the main stream of scientific literature even though Webb (2012) listed several points for which the transfer of knowledge and concepts related to one or to the other system would benefit our understanding of both. Even sharing this view, the leading hypothesis behind this contribution is that the pelagic system, where the dominant biotic component by number and biomass is microscopic, has specific features which strongly differentiate it from the above-the-surface terrestrial systems. Due to this, climate change, i.e. changes in temperature, precipitation and most importantly in the dynamics of the two fluid media, atmosphere and ocean, act with different mechanisms which prevents proceeding with analogies in many cases. In addition, the non-linearity of most of the processes and responses to perturbations requires, in order to obtain reliable forecasts or hindcasts, a detailed analysis of the path followed by the system which is normally overlooked in the step-change simulations or projections.


Science ◽  
1976 ◽  
Vol 192 (4239) ◽  
pp. 546-547
Author(s):  
S. VOGEL
Keyword(s):  

1970 ◽  
Vol 289 (5) ◽  
pp. 369-377
Author(s):  
John F. Carney ◽  
Bijoy K. Bhattacharya
Keyword(s):  

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