Which process allows groundwater to recharge through interconnected soil pores?

Infiltration is the process that allows groundwater to recharge through interconnected soil pores. This process refers to the movement of water from the surface into the soil, where it can then fill the spaces or pores within the soil profile. Infiltration is a crucial part of the water cycle as it enables precipitation to seep into the ground, replenishing aquifers and maintaining groundwater levels.

When water from rainfall or irrigation reaches the soil surface, it begins to percolate downward through these interconnected pores. This movement not only helps in recharging groundwater but also plays a significant role in sustaining plant life and maintaining soil moisture. Factors such as soil texture, structure, and vegetation cover can influence the rate and extent of infiltration.

The other processes listed do not address groundwater recharge directly. Evaporation involves the transformation of liquid water into vapor, transpiration refers to the release of water vapor from plants, and condensation is the conversion of vapor back into liquid, typically forming clouds. None of these processes facilitate the movement of water into soil and the aquifers beneath it, which makes infiltration the correct answer in the context of groundwater recharge.