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1<br />

Civil Engineering, University of Victoria, Victoria, British Columbia, Canada<br />

2<br />

Department of Civil Engineering, McGill University, Montreal, Québec, Canada<br />

3<br />

Department of Geological Sciences, The University of Texas at Austin, Austin, Texas, USA<br />

4<br />

Department of Geography, University of Calgary, Calgary, Alberta, Canada<br />

5<br />

Geoscience Centre, Georg-August-Universität Göttingen, Göttingen, Germany<br />

Groundwater is important for energy and food security, human health, and ecosystems.<br />

Unfortunately, groundwater is being depleted globally impacting agriculture and the environment,<br />

and even causing regional crustal deformation. Groundwater is also part of diverse<br />

earth processes from chemical weathering to ocean eutrophication but groundwater<br />

dynamics are not part of most earth system models. The time since groundwater recharge,<br />

or groundwater age, ranges hugely from days to millions of years, which is important for<br />

groundwater management and the role of groundwater in various earth processes. Yet,<br />

the volume, distribution and lifespan of young groundwater remain unknown. Here we<br />

show that only ~6% of global volume of groundwater is less than fifty years old (0.26 - 4.2<br />

million km 3 ) and that current pumping rates can deplete this young groundwater in less<br />

than fifty years in half the areas heavily irrigated with groundwater. We combine extensive<br />

geochemical, geological, hydrologic and geospatial datasets with numerical groundwater<br />

simulations to derive two consistent and independent estimates of the young groundwater<br />

volume as well as provide the first data-driven estimate of total groundwater volume<br />

(~22.6 million km 3 in the upper 2 km of the crust). Most young groundwater is found in<br />

the first 250 meters underground but is very unevenly distributed across the Earth. The<br />

regions with heavy groundwater irrigation and a

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