Thawing permafrost on Peel Plateau releasing acid that's breaking down minerals: study

Mineral weathering intensified by thawing permafrost is likely increasing the amount of carbon dioxide released into the air and water, according to a study from the University of Alberta.

Mineral weathering likely increasing carbon dioxide released into the air and water, says study

A new study from the University of Alberta found that permafrost thaw on the Peel Plateau is accelerating the chemical breakdown of minerals which causes climate warming. (Submitted by Scott Zolkos )

Rapidly thawing permafrost on the N.W.T.'s Peel Plateau is releasing acid that breaks down minerals and could be further contributing to Arctic climate change, according to new research from the University of Alberta.

The study, published in Geophysical Research Letters, found that as permafrost thaw accelerates, a process called mineral weathering intensifies. This happens when minerals that were previously frozen are exposed and broken down into their chemical components by sulphuric or carbonic acid that can exist naturally in water.

It has also likely increased the amount of carbon dioxide released into the air and water, the study says, which causes climate warming.

'Like a giant mud pit'

Lead author Scott Zolkos is a PhD candidate with the University of Alberta. (Submitted by Scott Zolkos )

Lead author Scott Zolkos, who is a PhD candidate in the university's Department of Biological Sciences, said the Peel Plateau is an ideal place to study this phenomenon. During the last glacial cycle, he explained, as the ice sheet moved it ground up bedrock and then preserved minerals.

"It's an exciting place for this type of work because the permafrost there is more mineral and sediment rich," he said.

Zolkos said the researchers also worked with scientists from the N.W.T. Geological Survey to look at long-term records of the Peel River. The records showed that sulphuric-driven mineral weathering has intensified as permafrost thaw has accelerated.

He noted that permafrost thaw slumps in the Peel Plateau are "impressive" and said the largest one he saw was several hundred metres across and more than 30 metres deep.

"They're really pretty massive features and inside them there can be quite a lot of activity because the ground subsides … and the permafrost becomes exposed," he said, explaining that rainfall can increase this movement.

"It looks like a giant mud pit." 

Impacting local ecosystem

Zolkos said researchers also spent four years in the field and worked alongside local residents who helped guide them and collect samples.

"Just hearing their perspectives on how that region has changed over the past five decades or more, it's very interesting to hear," he said. "It also gives us a really deep appreciation for a lot of ecological change that we haven't seen in only the past few years that we've been here."

Zolkos said mineral weathering impacts the ecosystem, which has both local and global impacts.

Zolkos says mineral weathering is changing the chemical composition of streams in the Peel Plateau. (Submitted by Scott Zolkos )

"As permafrost thaws and this material that's been kind of locked away in the permafrost for so long enters streams, it can transform and change the chemical composition of streams," he said.

The growing research in this area shows the need to reduce the amount of carbon dioxide in the atmosphere, Zolkos said.

"Once these thaw slump features start, it's not really something you can stop, which I think is true of a lot of permafrost thaw in the Arctic."

Zolkos said he hopes to look at the larger picture of the effects of permafrost thaw slumps on carbon dioxide in streams and how minerals move through streams.


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