06/05/2026
This is an informative post from our watershed neighbors the the west. Drought conditions are no joke!!! Neshaminy Watershed Association
Groundwater Recharge - We Need It!
You may have seen in the news that Chester County is dealing with wells running dry. This is due to the underground aquifer, which supplies the well water, not being recharged (remember that drought warning last month).
Groundwater recharge happens when water moves downward from the surface into the soil and rock layers, reaching the water table over time. Aquifers are not large empty spaces holding water underground. If you dig a hole and there is water at the top you are seeing the water table. Below this is rock and sediment with a bunch of tiny spaces in between that hold water, this is the aquifer.
When rain or snow falls to the ground it seeps into the ground and through the tiny spaces until it reaches that top layer, the water table. Once the water meets the water table the aquifer is recharged. There are many factors that can stop the water getting into these spaces, such as:
• Surfaces that do not absorb water: such as paved or compacted surfaces and structures.
• Runoff: flows that are not slowed down enough to seep into the ground.
• Deforestation: forests capture rainfall and slows it down so it can seep into the ground.
• Stone & Soil Type: some types allow the water in better than others.
If you'd like to learn more about this topic leave us a comment!