In a novel scientific article published inwards the magazine Nature Communications a grouping of scientists led yesteryear University of Copenhagen authors shows that thawing permafrost releases a high amount as well as diverseness of volatile organic compounds (VOCs). These compounds are non greenhouse gases similar carbon dioxide as well as methane.
Professor Riikka Rinnan from Department of Biology as well as Center for Permafrost, University of Copenhagen explains, 'Surprisingly, our novel experiments present that VOCs tin strength out last released from soil permafrost layers, which oftentimes stand upwards for organic textile stored for decades or longer. Even to a greater extent than surprisingly, VOCs from thawing permafrost may non last released to the atmosphere, equally our results present that the annual thaw layers higher upwards the permafrost seem to filter the VOCs beingness released from the permafrost.'
Soil microbes inwards a crucial role
Using advanced tracing techniques the inquiry squad shows, that the VOCs are consumed yesteryear microorganisms living inwards the soil layers. It appears, therefore, that the actual free of VOCs from thawing permafrost is determined yesteryear what happens to them on the means from the deeper soil layers to the atmosphere. If the permafrost is exposed to the surface e.g. due to erosion, or if the microbial uptake is hampered for illustration due to waterlogging, this could last a new, unaccounted Arctic VOC source alongside potential implications on the regional climate.
Source: University of Copenhagen [August 24, 2018]
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