A science journalist is writing about a groundwater aquifer spanning 15 kilometers in length and averaging 2.5 kilometers in width, with a uniform depth of 40 meters and a porosity of 20%. If the aquifer is fully saturated, how many cubic meters of water does it hold?

Mon, 04 May 2026 22:21:01 +0000

**How Do Scientists Estimate the Water Held in an Underground Aquifer?**
*A science journalist is writing about a groundwater aquifer spanning 15 kilometers in length and averaging 2.5 kilometers in width, with a uniform depth of 40 meters and a porosity of 20%. If the aquifer is fully saturated, how many cubic meters of water does it hold?* Beneath the surface of much-discussed climate challenges, groundwater aquifers quietly play a crucial role in water security across the United States. These vast underground reservoirs, often stretching for miles, store freshwater that communities rely on for drinking, agriculture, and industry. One such aquifer—spanning 15 kilometers long and 2.5 kilometers wide, plunging to a depth of 40 meters with 20% of its volume filled with water—raises an essential question: just how much water does it hold? This science journalist is exploring this figure not just as a number, but as a key indicator of sustainable water resources in a changing climate. Understanding how water volumes are calculated helps readers grasp the true scale of subsurface conservation and informs conversations about long-term water management. Why is this aquifer attracting attention now? Rising awareness of groundwater sustainability mirrors broader national trends linking clean water access to resilience against drought and climate variability. In the U.S., groundwater supports nearly half of all drinking water and a significant portion of agricultural irrigation. As reports of aquifer depletion grow, so does public and scientific focus on quantifying what’s truly available beneath our feet. This aquifer—fully saturated, uniform in structure—becomes a textbook example of how scientists translate physical dimensions and geological properties into usable water volume estimates. When considering a saturated unit volume of rock or sediment, porosity measures the percentage of pore space available to hold water. With a 20% porosity, 80% of the aquifer’s total volume consists of open spaces where water fills gaps between rock grains. To estimate total water volume, scientists multiply the aquifer’s total solid volume by its porosity and saturation rate. The aquifer spans 15,000 meters in length and 2,500 meters in width, creating a footprint of 37.5 million square meters—roughly 18 times the size of Central Park. Dropping to a depth of 40 meters, the total volume reaches 1.5 billion cubic meters. With a uniform porosity of 20%, this translates to approximately **300 million cubic meters** of water when fully saturated.