A multiple-effect diffusion still was theoretically analyzed with a one-dimensional steady-state model. The still was tilted, and heated on the bottom and cooled on the top by natural-convection evaporation. The findings are summarized as; (1) The total evaporation rate,
Uv has a peak at 5 effects and then gradually decreases with an increasing number of effects,
n. The coefficient of performance,
COP increases rapidly at first and then gradually with an increasing
n. (2) The evaporative cooling enhanced by forced convection causes small increases in
Uv, and little changes in
COP. (3) Seawater heated beforehand causes great increases in
COP, and small changes in
Uv. (4) The
COP increases rapidly at first and then gradually with an increasing concentration of the effluent seawater. (5) An decrease in temperature of the still's bottom causes a great increase in
COP, accompanied with a drastic decrease in
Uv. (6) The pre-heating of seawater, the increase in the effluent concentration and the decrease in the bottom temperature cause decreases in heat for seawater temperature rise in the still, resulting in the increases in
COP.
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