A Halo-Thermal Simulation of the Dead Sea for Application to Solar Energy Projects

1983 ◽  
Vol 105 (4) ◽  
pp. 348-355 ◽  
Author(s):  
P. Vadasz ◽  
D. Weiner ◽  
Y. Zvirin

A one-dimensional numerical model is developed to predict the long-range variations of vertical temperature, density, and salinity profiles in the Dead Sea, which is a highly saline large water body. The model utilizes the continuity, momentum, energy, and mass transfer equations, while taking into account the influence of the wind. The partial differential equations were solved numerically by means of explicit finite differences method. Simulation results were verified by comparison to measured data. In addition, the algorithm evaluates the evaporation rate from the Dead Sea which is an important parameter in several engineering projects under planning, such as the Mediterranean-Dead Sea conduit and the construction of floating salt gradient solar ponds for power generation.

Energy ◽  
2011 ◽  
Vol 36 (2) ◽  
pp. 922-931 ◽  
Author(s):  
A. Saleh ◽  
J.A. Qudeiri ◽  
M.A. Al-Nimr
Keyword(s):  
Dead Sea ◽  

1982 ◽  
Vol 104 (4) ◽  
pp. 293-298 ◽  
Author(s):  
Y. S. Cha ◽  
W. T. Sha ◽  
W. W. Schertz

A one-dimensional numerical model is developed to predict the diurnal variations of vertical temperature and concentration profiles in salt-gradient solar ponds. The model employs augmented thermal and mass diffusivities due to turbulent wind mixing and double-diffusive convection. Numerical results indicate that the thickness of the surface convective layer increases with wind speed (or the wavelength of the surface wave). Double-diffusive convection is, in the absence of wind, capable of sustaining a mixed layer at the surface when strong cooling occurs over the pond. In field ponds, the surface convective layer is probably maintained as a result of the combined action of wind-generated turbulent mixing and double-diffusive convection.


2018 ◽  
Vol 140 (10) ◽  
Author(s):  
Shahram Derakhshan ◽  
Seyedeh Elnaz Mirazimzadeh ◽  
Syamak Pazireh

Salt gradient solar ponds are the ponds in which due to existence of saline and salt gradient layers, lower layers are denser and avoid the natural convection phenomenon to occur so that solar radiation energy can be stored in the lowest zone. In this study, one-dimensional (1D) and two-dimensional (2D) numerical approaches have been implemented to simulate unsteady buoyancy-driven flow of solar ponds. In 1D method, the pond has been investigated in terms of the layers thicknesses so that the variation of temperature is calculated by energy conservation equation. The formulized radiation term was used as energy source term in energy equation. The results of 1D approach were validated with an experimental study and then optimization was carried out to determine the maximum thermal efficiency for an interval of layers height. Since the stability of the solar pond cannot be determined by 1D simulation, a 2D approach was considered to show the stability for different nonconvective zone (NCZ) heights and different salt gradients. In 2D study, in order to investigate hydrodynamic and thermal behavior of saltwater fluid, a numerical approach was used to simulate temperature gradients throughout the pond. The results of 2D numerical method are validated with an experimental data. The effect of linear and nonlinear salt gradient was considered.


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