To calculate the pressure difference in a convective loop for water with two temperature points, we can use the hydrostatic pressure equation along with the properties of water.
The density of water varies with temperature. At approximately 20°C, the density is about 998 kg/m³, and at 60°C, it decreases to about 983 kg/m³. For our calculation, we can average the two densities, but let's take the values as they are for simplicity in this case.
The hydrostatic pressure difference can be expressed as: