MARVI
04 / 12

Groundwater, demystified

An invisible resource with visible consequences.

Rain moves through soil and rock into an aquifer. Wells reveal only a small window into a connected underground system.

Village groundwater recharge structure
A covered community water and recharge structure
Researchers measuring groundwater in the field

Then / now

From 10–15 metres in the 1960s to 30–40 metres today.

In some places, farmers drill beyond 100 metres chasing a falling watertable. Recharge helps, but sustainable use also requires understanding demand.

G / 01

The aquifer is shared

Water pumped from one well can affect neighbours drawing from the same underground store.

G / 02

Rainfall is not recharge

Only part of rain reaches groundwater; soils, geology, land use and structures shape the journey.

G / 03

Trends need time

A single reading is a snapshot. Repeated measurements reveal depletion, recovery and seasonal rhythm.