The world's deserts may be storing some of the climate-changing carbon dioxide emitted by human activities, a new study suggests. Massive aquifers¹ underneath² deserts could hold more carbon than all the plants on land, according to the new research. Humans add carbon dioxide to the atmosphere through fossil fuel combustion³ and deforestation. About 40 percent of this carbon stays in the atmosphere and roughly 30 percent enters the ocean, according to the University Corporation for Atmospheric⁴ Research. Scientists thought the remaining carbon was taken up by plants on land, but measurements show plants don't absorb all of the leftover⁵ carbon. Scientists have been searching for a place on land where the additional carbon is being stored--the so-called "missing carbon sink."

 

The new study suggests some of this carbon may be disappearing underneath the world's deserts - a process exacerbated⁶ by irrigation. Scientists examining the flow of water through a Chinese desert found that carbon from the atmosphere is being absorbed by crops, released into the soil and transported underground in groundwater--a process that picked up when farming entered the region 2,000 years ago. 

 

Underground aquifers store the dissolved carbon deep below the desert where it can't escape back to the atmosphere, according to the new study. 

 

The new study estimates that because of agriculture roughly 14 times more carbon than previously⁷ thought could be entering these underground desert aquifers every year. These underground pools that taken together cover an area the size of North America may account for at least a portion of the "missing carbon sink" for which scientists have been searching.

 

"The carbon is stored in these geological structures covered by thick layers of sand, and it may never return to the atmosphere," said Yan Li, a desert biogeochemist with the Chinese Academy of Sciences in Urumqi, Xinjiang, and lead author of the study accepted for publication in Geophysical Research Letters, a journal of the American Geophysical Union. "It is basically a one-way trip."

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