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Arctic Soil May Contain Nearly Twice Greenhouse-Gas Producing Material Than Previously Estimated

Date:
October 8, 2008
Source:
University of Alaska Fairbanks
Summary:
Frozen arctic soil contains nearly twice the greenhouse-gas-producing organic material as was previously estimated, according to new research. The research team discovered a previously undocumented layer of organic matter on top of and in the upper part of permafrost, ranging from 60 to 120 centimeters deep.

Chien-Lu Ping conducting soil tests.
Credit: Photo courtesy of UAF School of Natural Resources & Agricultural Sciences

Frozen arctic soil contains nearly twice the greenhouse-gas-producing organic material as was previously estimated, according to recently published research by University of Alaska Fairbanks scientists.

School of Natural Resources & Agricultural Sciences professor Chien-Lu Ping published his latest findings in Nature Geoscience. Wielding jackhammers, Ping and a team of scientists dug down more than one meter into the permafrost to take soil samples from more than 100 sites throughout Alaska. Previous research had sampled to about 40 centimeters deep.

After analyzing the samples, the research team discovered a previously undocumented layer of organic matter on top of and in the upper part of permafrost, ranging from 60 to 120 centimeters deep. This deep layer of organic matter first accumulates on the tundra surface and is buried during the churning freeze and thaw cycles that characterize the turbulent arctic landscape.

The resulting patterned ground plays a key role in the dynamics of carbon storage and release, Ping found. When temperatures warm and the arctic soil churns, less carbon from the surface gets to the deeper part of the soil. The carbon already stored in the deeper part of the soil is released into the atmosphere as carbon dioxide, methane and other gases.

Ping predicted that a two- to three-degree rise in air temperatures could cause the arctic tundra to switch from a carbon sink--an area that absorbs more carbon dioxide than it produces--to a carbon source--an area that produces more carbon dioxide than it absorbs. The more organic material stored in the tundra, the greater the potential effect of future releases, Ping stated.

“The distribution of the Arctic carbon pool with regard to the surface, active layer and permafrost has not been evaluated before, but is very relevant in assessing changes that will occur across the Arctic system,” Ping wrote in his study. “Where soil organic carbon is located in the soil profile is especially relevant and useful to climate warming assessments that need to evaluate effects on separate soil processes that vary with temperature and depth throughout the whole annual cycle of seasons.”

Colleagues on the project were Gary Michaelson, UAF Agricultural and Forestry Experiment Station; Mark Jorgenson, Alaska Biological Research; John Kimble, professional soil scientist; Howard Epstein, University of Virginia Department of Environmental Sciences; Vladimir Romanovsky, UAF Geophysical Institute; Donald Walker, UAF Institute of Arctic Biology. Ping’s study also included data from similarly conducted Canadian research.


Story Source:

The above story is based on materials provided by University of Alaska Fairbanks. Note: Materials may be edited for content and length.


Cite This Page:

University of Alaska Fairbanks. "Arctic Soil May Contain Nearly Twice Greenhouse-Gas Producing Material Than Previously Estimated." ScienceDaily. ScienceDaily, 8 October 2008. <www.sciencedaily.com/releases/2008/10/081008091129.htm>.
University of Alaska Fairbanks. (2008, October 8). Arctic Soil May Contain Nearly Twice Greenhouse-Gas Producing Material Than Previously Estimated. ScienceDaily. Retrieved October 21, 2014 from www.sciencedaily.com/releases/2008/10/081008091129.htm
University of Alaska Fairbanks. "Arctic Soil May Contain Nearly Twice Greenhouse-Gas Producing Material Than Previously Estimated." ScienceDaily. www.sciencedaily.com/releases/2008/10/081008091129.htm (accessed October 21, 2014).

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