A new study has, for the first time, estimated the total volume ofgroundwater present on the Earth. The results show that we're usingup the water supply quicker than it can be naturally replaced, whilefuture research will seek to determine exactly how long it will be until moderngroundwater runs dry.
Groundwater is an extremely preciousresource, being a key source of sustenance for humanity and the ecosystems we inhabit. It resides beneath the Earth's surface, ranges frommillions of years to just months old, and exists in huge quantities –quite literally millions of cubic kilometers. While calculations backin the 1970s roughly estimated the global volume of groundwater, this newstudy represents the first detailed calculation of the exactquantity, and it could have big implications.
Researchers from the University of Victoria, the University of Texas at Austin, the University of Calgary and the University of Göttingen created a map ofgroundwater distribution by carefully analyzing numerous datasets, and making use of more than40,000 scientific models. In all, the study estimates a total volumeof almost 23 million cubic kilometers (5.5 million cubic miles) of groundwater.
Two kinds of groundwater were detailed– old and modern. Old groundwater is located deep in the Earth, issalty and often contains uranium or arsenic. In contrast, moderngroundwater is closer to the surface, and moves more quickly.Unfortunately, it's also far more susceptible to climate change thanthe deeper, ancient water.
The map shows the majorityof the modern supply to be located in mountainous and tropicalregions, such as the Amazon Basin, the Congo and the Rockies.Unsurprisingly, very little groundwater was detected in arid regions like the Sahara desert and Central Australia, which is something that has long been suspected.
"Intuitively, we expect drier areasto have less young groundwater and more humid areas to have more, butbefore this study, all we had was intuition," said team member Dr Kevin Befus. "Now, we have aquantitative estimate that we compared to geochemical observations."
Of the calculated 23 million km3 ofgroundwater, 350,000 km3 (84,000 mi3) of it is less than 50years old. Futhermore, the study found that less than six percent ofthe groundwater located up to two kilometers (1.2 mi) deep in the earth isrenewable within a single human lifetime. In essence, we're using upgroundwater far quicker than it can be replaced.
Moving forward, the team plans tofurther analyze the data with the goal of furthering ourunderstanding of exactly how quickly the modern and old groundwateris being depleted by human activity. Once those calculations arecomplete, we'll have a strong idea of exactly how long we have before the supplyruns out.
In the meantime, the researchersbelieve that the results of the study will help inform variousstudies and individuals, from policy developers and water managers toscientists focusing on geochemistry, oceanography and more.
The researchers published the findingsin the journal Nature Geoscience.
Source: University of Victoria
A new study has, for the first time, estimated the total volume ofgroundwater present on the Earth. The results show that we're usingup the water supply quicker than it can be naturally replaced, whilefuture research will seek to determine exactly how long it will be until moderngroundwater runs dry.
Groundwater is an extremely preciousresource, being a key source of sustenance for humanity and the ecosystems we inhabit. It resides beneath the Earth's surface, ranges frommillions of years to just months old, and exists in huge quantities –quite literally millions of cubic kilometers. While calculations backin the 1970s roughly estimated the global volume of groundwater, this newstudy represents the first detailed calculation of the exactquantity, and it could have big implications.
Researchers from the University of Victoria, the University of Texas at Austin, the University of Calgary and the University of Göttingen created a map ofgroundwater distribution by carefully analyzing numerous datasets, and making use of more than40,000 scientific models. In all, the study estimates a total volumeof almost 23 million cubic kilometers (5.5 million cubic miles) of groundwater.
Two kinds of groundwater were detailed– old and modern. Old groundwater is located deep in the Earth, issalty and often contains uranium or arsenic. In contrast, moderngroundwater is closer to the surface, and moves more quickly.Unfortunately, it's also far more susceptible to climate change thanthe deeper, ancient water.
The map shows the majorityof the modern supply to be located in mountainous and tropicalregions, such as the Amazon Basin, the Congo and the Rockies.Unsurprisingly, very little groundwater was detected in arid regions like the Sahara desert and Central Australia, which is something that has long been suspected.
"Intuitively, we expect drier areasto have less young groundwater and more humid areas to have more, butbefore this study, all we had was intuition," said team member Dr Kevin Befus. "Now, we have aquantitative estimate that we compared to geochemical observations."
Of the calculated 23 million km3 ofgroundwater, 350,000 km3 (84,000 mi3) of it is less than 50years old. Futhermore, the study found that less than six percent ofthe groundwater located up to two kilometers (1.2 mi) deep in the earth isrenewable within a single human lifetime. In essence, we're using upgroundwater far quicker than it can be replaced.
Moving forward, the team plans tofurther analyze the data with the goal of furthering ourunderstanding of exactly how quickly the modern and old groundwateris being depleted by human activity. Once those calculations arecomplete, we'll have a strong idea of exactly how long we have before the supplyruns out.
In the meantime, the researchersbelieve that the results of the study will help inform variousstudies and individuals, from policy developers and water managers toscientists focusing on geochemistry, oceanography and more.
The researchers published the findingsin the journal Nature Geoscience.
Source: University of Victoria