What happens to groundwater when the rate of infilration is less than the rate water being pumpedout of the ground?

When the rate of infiltration is less than the rate at which groundwater is being pumped out, the water table will begin to decline. This depletion can lead to reduced availability of water for wells and springs, potentially causing them to dry up. Additionally, prolonged groundwater depletion can result in land subsidence and negative impacts on ecosystems that rely on groundwater.