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Salt gradient solar pond is a water body in which a significant temperature rise
is caused by the absorption of solar radiation by the prevention of convection. In
other words, solar ponds are solar radiation collector-cum-storage devices. These are
capable enough to supply low grade heat at large scale. There are three distinct zones in a
solar pond, namely an Upper Convective Zone (UCZ), a Non-Convective Zone or
Non-Convective Gradient Zone (NCZ or NGZ) and a Storage or Lower
Convective Zone (STZ or LCZ).
The top convective layer absorbs a large portion of the solar radiation.
However, less than 50% penetrates to a depth of 0.2 m (Wang and Akbarzadeh, 1983) as
half the solar spectrum is in the infra red region, for which water is almost opaque
(Cengel and Ozissik, 1984). In other words, water is a selective absorber. In the
same context, Mehmet et al. (2006) have also reported a maximum absorption of
28.1% in the heat storage zone. Various losses of this stored energy result in further
reduced efficiency. Different methods and models have been proposed to improve the
efficiency of the solar pond (Rajagopan et
al., 2008; and Sharma et al., 2009). |