To determine the major factor affecting the rate of groundwater recharge, we need to understand the process of groundwater recharge and the factors that influence it.
- Groundwater Recharge: The process by which water infiltrates from the surface into the saturated zone of an aquifer.
- Factors Affecting Recharge: Several factors influence how quickly and efficiently groundwater is replenished, including precipitation, soil type, land use, and depth to the water table.
- Precipitation intensity: High-intensity rainfall can lead to more runoff and less infiltration if the soil's infiltration capacity is exceeded. While important, it's not the sole determining factor.
- Soil permeability: The ability of soil to transmit water. High permeability allows for greater infiltration and recharge. This is a critical factor.
- Groundwater depth: While a shallow water table can increase recharge rates (less distance for water to travel), the soil properties above are still key. It is not as direct as soil permeability.
- Land use: Land use can significantly affect recharge. For example, urbanization can reduce infiltration due to impervious surfaces, while forests can enhance infiltration.
While all options play a role, soil permeability is the most direct control on the rate at which water can infiltrate the soil and reach the groundwater table. It determines how easily water can move through the unsaturated zone. Land use changes soil permeability; precipitation intensity is a factor, but permeability dictates how much of the precipitation will infiltrate.
The major factor affecting the rate of groundwater recharge is Soil permeability.
In the context of the effect of drainage density on the run-off generation and the hydrograph at the catchment outlet, all other factors remaining the same, pick one or more CORRECT statement(s):