Study Offers New Explanation for Siberia's Permafrost Cratershttps://phys.org/news/2024-09-explanation-siberia-permafrost-craters.htmlMysterious craters that first appeared in the Siberian permafrost a decade ago were caused by climate change-driven pressure changes that explosively released methane frozen underground, a new study reports. The research offers a fresh take on the origins of the craters first sighted on Russia's Yamal Peninsula in 2014.
The new study finds that the region's unusual geology, coupled with climate warming, kickstarted a process that led to the release of methane gas from methane hydrates in the permafrost.
"There are very, very specific conditions that allow for this phenomenon to happen," said Ana Morgado, a chemical engineer at the University of Cambridge and one of the study's authors. "We're talking about a very niche geological space."
The research was published in
Geophysical Research Letters.
... The Yamal Peninsula's thick, clayey permafrost acts as an osmotic barrier—and warming is changing it. This 180 to 300-meter (590 to 980-foot)-thick layer stays permanently frozen throughout the year. An "active layer" of topsoil above it thaws and re-freezes seasonally.
Interspersed throughout the tundra and sandwiched within the permafrost lie unusual, one-meter-thick layers of unfrozen, high-salinity water called crypogegs, kept liquid by a combination of pressure and salinity. Underneath the cryopegs sits a layer of crystallized methane-water solids, called methane hydrates, which are kept stable by high pressure and low temperature.
But warmer temperatures are destabilizing these layers. Climate change has caused the active layer to melt and expand downward until it reaches the cryopeg, releasing water that travels via osmotic pressure into the cryopeg, the researchers found.
But there isn't enough space in the cryopeg to hold the extra meltwater forced in by osmosis, so pressure builds. The increasing pressure creates cracks in the soil that travel upward from the cryopeg toward the surface. The pressure gradient then reverses: the cracked soil causes a sudden drop in pressure at depth. That pressure change damages the methane hydrates below the cryopeg, which causes a release of methane gas and a physical explosion.
The lead-up to the explosion can last for decades, the study found. That timeline aligns with increasing climate warming starting in the 1980s.
Ana M. O. Morgado et al,
Osmosis Drives Explosions and Methane Release in Siberian Permafrost,
Geophysical Research Letters (2024)
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GL108987