Artificial recharge from pits, trenches, or basins ordinarily is not considered feasible in situations where a thick layer of slowly permeable material exists near the surface. Results of a field investigation of recharge from an irrigation tail‐water pit indicate that pit or trench recharge is feasible under this condition provided that a much more permeable stratum exists above the less permeable one. The more highly conductive layer acts as a subsurface spreading basin which greatly enhances the opportunity for recharge.
The potential for recharge from pits penetrating a highly conductive layer underlain by a slowly permeable stratum can be calculated from the results of a simple theoretical analysis which is presented. The importance of subsurface spreading is demonstrated by a numerical example using conditions similar to those encountered during the field investigation. Under these conditions a narrow pit or trench 525 feet long and 10 feet deep has the potential for recharging at a rate of 1 million gpd or about 700 gpm. Subsurface spreading occurs over nearly 10 acres for this case. Evaporation is reduced because the need for spreading the water over large areas on the land surface is eliminated. Since the length of pit perimeter and not the surface area is the important factor for design, the volume excavated can be minimized by constructing long narrow pits or trenches.