A Full-region Model for Ultra-Scaled MoS2 MOSFET Covering Direct Source-Drain Tunneling

Author(s):  
Weiran Cai ◽  
Wenrui Lan ◽  
Zichao Ma ◽  
Lining Zhang ◽  
Mansun Chan
Keyword(s):  
2005 ◽  
Vol 35 (3) ◽  
pp. 359-382 ◽  
Author(s):  
L. Anderson ◽  
G. Stansfield
Keyword(s):  

PLoS ONE ◽  
2015 ◽  
Vol 10 (10) ◽  
pp. e0140606
Author(s):  
Zengru Cui ◽  
Gonglin Yuan ◽  
Zhou Sheng ◽  
Wenjie Liu ◽  
Xiaoliang Wang ◽  
...  
Keyword(s):  

1967 ◽  
Vol 1 (1) ◽  
pp. 33-45
Author(s):  
Harold T. Moody ◽  
Frank W. Puffer ◽  
Robert M. Williams

1996 ◽  
Vol 118 (1) ◽  
pp. 37-44 ◽  
Author(s):  
G. A. Eghneim ◽  
S. J. Kleis

A combined experimental and numerical study was conducted to support the development of a new gradient maintenance technique for salt-gradient solar ponds. Two numerical models were developed and verified by laboratory experiments. The first is an axisymmetric (near-field) model which determines mixing and entrainment in the near-field of the injecting diffuser by solving the conservation equations of mass, momentum, energy, and salt. The model assumes variable properties and uses a simple turbulence model based on the mixing length hypothesis to account for the turbulence effects. A series of experimental measurements were conducted in the laboratory for the initial adjustment of the turbulence model and verification of the code. The second model is a one-dimensional far-field model which determines the change of the salt distribution in the pond gradient zone as a result of injection by coupling the near-field injection conditions to the pond geometry. This is implemented by distributing the volume fluxes obtained at the domain boundary of the near-field model, to the gradient layers of the same densities. The numerical predictions obtained by the two-region model was found to be in reasonable agreement with the experimental data.


2007 ◽  
Vol 36 (4) ◽  
Author(s):  
Małgorzata Robakiewicz

Seasonal variability of hydrodynamics in the Vistula Estuary in 1994The Vistula Estuary is a coastal water body boasting free connection with the open sea, where mixing processes of marine and fluvial waters are maintained by local conditions. Based on results from a hydrodynamic model, applied to represent conditions in the year 1994, and using salinity as a tracer, it was found that fluvial water has a tendency to spread westward from the river mouth. This is in contradiction with the dominant wind direction in the region. Model results confirmed field observations of specific hydrological and meteorological conditions required to transport fluvial water northward, towards the Hel Peninsula.


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