Cellular alignment by grafted adhesion peptide surface density gradients

2004 ◽  
Vol 71A (3) ◽  
pp. 403-411 ◽  
Author(s):  
Catherine E. Kang ◽  
Ernest J. Gemeinhart ◽  
Richard A. Gemeinhart
Keyword(s):  
Surface Density ◽  
Density Gradients ◽  
Cellular Alignment

Sea surface density gradients in the Nordic Seas during the Holocene as revealed by paired microfossil and isotope proxies

2016 ◽  
Vol 31 (3) ◽  
pp. 380-398 ◽  
Author(s):  
Nicolas Van Nieuwenhove ◽  
Claude Hillaire-Marcel ◽  
Henning A. Bauch ◽  
Anne de Vernal
Keyword(s):  
Surface Density ◽  
Sea Surface ◽  
Density Gradients ◽  
Nordic Seas ◽  
The Holocene

Collective Conformations of DNA Polymers Assembled on Surface Density Gradients

2012 ◽  
Vol 134 (9) ◽  
pp. 3954-3956 ◽  
Author(s):  
Gabriel Shemer ◽  
Yahel Atsmon ◽  
Eyal Karzbrun ◽  
Roy H. Bar-Ziv
Keyword(s):  
Surface Density ◽  
Density Gradients

Endothelial Cell Migration on Surface-Density Gradients of Fibronectin, VEGF, or Both Proteins

Langmuir ◽  
2007 ◽  
Vol 23 (22) ◽  
pp. 11168-11173 ◽  
Author(s):  
Lingyun Liu ◽  
Buddy D. Ratner ◽  
E. Helene Sage ◽  
Shaoyi Jiang
Keyword(s):  
Cell Migration ◽  
Endothelial Cell ◽  
Surface Density ◽  
Endothelial Cell Migration ◽  
Density Gradients

Motions of neutral hydrogen at high latitudes

1967 ◽  
Vol 31 ◽  
pp. 265-278 ◽  
Author(s):  
A. Blaauw ◽  
I. Fejes ◽  
C. R. Tolbert ◽  
A. N. M. Hulsbosch ◽  
E. Raimond
Keyword(s):  
Surface Density ◽  
Velocity Dispersion ◽  
Neutral Hydrogen ◽  
Hydrogen Gas ◽  
High Latitudes ◽  
Low Velocity

Earlier investigations have shown that there is a preponderance of negative velocities in the hydrogen gas at high latitudes, and that in certain areas very little low-velocity gas occurs. In the region 100° <l< 250°, + 40° <b< + 85°, there appears to be a disturbance, with velocities between - 30 and - 80 km/sec. This ‘streaming’ involves about 3000 (r/100)2solar masses (rin pc). In the same region there is a low surface density at low velocities (|V| < 30 km/sec). About 40% of the gas in the disturbance is in the form of separate concentrations superimposed on a relatively smooth background. The number of these concentrations as a function of velocity remains constant from - 30 to - 60 km/sec but drops rapidly at higher negative velocities. The velocity dispersion in the concentrations varies little about 6·2 km/sec. Concentrations at positive velocities are much less abundant.

ATOMIZATION MODELLING OF LIQUID JETS USING A TWO-SURFACE-DENSITY APPROACH

2015 ◽  
Vol 25 (1) ◽  
pp. 47-80 ◽  
Author(s):  
Bejoy Mandumpala Devassy ◽  
Chawki Habchi ◽  
Eric Daniel
Keyword(s):  
Surface Density ◽  
Liquid Jets
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