To determine the primary recharge mechanism of a dug well, we need to understand how dug wells are constructed and how they receive water.
- Dug Well: A type of water well constructed by excavating or digging into the ground, typically by hand or with simple tools. They are usually shallow and penetrate the water table.
- Recharge Mechanism: The process by which a well receives water, replenishing its supply.
- Seepage: The slow percolation of water through soil and rock.
- Direct rainfall into the well openings: While some direct rainfall might enter the well, it is not the primary source of recharge, especially if the well is covered or has a small opening.
- By the lateral flow from nearby surface water bodies: If a dug well is located very close to a surface water body, some lateral flow might contribute, but this is not the general mechanism.
- Through seepage from the surrounding areas after rainfall: The primary recharge mechanism for a dug well is the infiltration of rainwater into the soil and its subsequent seepage through the surrounding areas to the well. The well acts as a collection point for the groundwater in its vicinity.
- By artificial means such as recharge pits and collection from rooftops of houses: While artificial recharge methods can supplement groundwater recharge, they are not the inherent recharge mechanism of a traditional dug well.
The recharge mechanism of the dug well is Through seepage from the surrounding areas after rain fall.
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):