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Section 1: Publication
Publication Type
Journal Article
Authorship
Ferguson, G., McIntosh, J.C., Warr, O., Sherwood Lollar, B., Ballantine, C.J., Famiglietti, J.S., Kim, J.H., Michalski, J., Mustard, J.F., Tarnas, J. and McDonnell, J.J.
Title
Crustal Groundwater Volumes Greater than Previously Thought
Year
2021
Publication Outlet
Geophysical Research Letters, p.e2021GL093549
DOI
ISBN
ISSN
Citation
Ferguson, G., McIntosh, J.C., Warr, O., Sherwood Lollar, B., Ballantine, C.J., Famiglietti, J.S., Kim, J.H., Michalski, J., Mustard, J.F., Tarnas, J. and McDonnell, J.J., 2021. Crustal Groundwater Volumes Greater than Previously Thought. Geophysical Research Letters, p.e2021GL093549. American Geophysical Union Highlight Article.
Abstract
Global groundwater volumes in the upper 2 km of the Earth's continental crust—critical for water security—are well estimated. Beyond these depths, a vast body of largely saline and non-potable groundwater exists down to at least 10 km—a volume that has not yet been quantified reliably at the global scale. Here, we estimate the amount of groundwater present in the upper 10 km of the Earth's continental crust by examining the distribution of sedimentary and crystalline rocks with depth and applying porosity-depth relationships. We demonstrate that groundwater in the 2–10 km zone (what we call “deep groundwater”) has a volume comparable to that of groundwater in the upper 2 km of the Earth's crust. These new estimates make groundwater the largest continental reservoir of water, ahead of ice sheets, provide a basis to quantify geochemical cycles, and constrain the potential for large-scale isolation of waste fluids.
Key Points
-Groundwater is the largest continental store of water, liquid or otherwise
-The volume of deep saline groundwater is similar to shallow potable groundwater
-Deep groundwater systems remain largely unexplored
Plain Language Summary
Global groundwater volumes in the upper 2 km of the Earth's continental crust, which include important potable water supplies, are well estimated. At greater depths, a vast body of largely saline water exists down to at least 10 km and this volume that has not yet been quantified reliably at the global scale. Here, we estimate the amount of groundwater present in the upper 10 km of the Earth's continental crust. We demonstrate that groundwater between 2 and 10 km deep has a volume comparable to that of groundwater in the upper 2 km of the Earth's crust. These new estimates make groundwater the largest continental reservoir of water, ahead of ice sheets. This large volume of fluid, which is thought to be largely disconnected from the rest of the hydrologic cycle, is largely uncharacterized.
Plain Language Summary