Air Wells

Air Wells produce water from the air just as clouds do.  When warm moist air is cooled to what is called, the Due Point, it will condense provided it has something upon which to condense.  Condensation occurs in clouds when microscopic particles of dust are present.  When the air rises and is subsequently cooled to the due point water forms around the particles in the air.  In an Air Well cooling of the air to the due point occurs as the air contacts cool underground stones and water. the water in the air condenses on the rough edges of a suitable material (such as brick, concrete, stone) when the temperature of the air reaches the due point.  The condensation surfaces must be protected from the sun and cooled by the convective cooling effect of the earth. In our model it is conceivable that the proposed site could be designed to capture the prevailing warm moist air from the Western Sea, the Mediterranean Sea, and direct it under ground through the porous fill behind the sites retaining walls used to level the uneven landscape.  Therein the ground cooling effect would cool the air to the Due Point, the water in the air will condense on the stones and drip to the water table in the fill.  This effect has been known and used for thousands of years in the desert regions.  This system can conceivably produce millions of gallons of water within AKD. (Ref: Ezekiel 47:1+)


For more information and a drawing CLICK HERE.