[ Back to EurekAlert! ] Public release date: 2-Mar-2009
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Maria-José Viñas
mjvinas@agu.org
202-777-7530

Peter Weiss
pweiss@agu.org
202-777-7507
American Geophysical Union

Marc Airhart
mairhart@jsg.utexas.edu
512-471-2241
University of Texas


Wenchuan earthquake mudslides emit greenhouse gas

Mudslides that followed the 12 May 2008 Wenchuan, China earthquake, ranked by the US Geological Survey as the 11th deadliest earthquake ever recorded, may cause a carbon-dioxide release in upcoming decades equivalent to two percent of current annual global carbon emissions from fossil fuel combustion, a new study shows.

Mudslides wipe away plants and topsoil, depleting terrain of nutrients for plant regrowth and burying swaths of vegetation. Buried vegetable matter decomposes and releases carbon dioxide and other gases to the atmosphere.

The expected carbon dioxide release from the mudslides following the Wenchuan earthquake is similar to that caused by Hurricane Katrina's plant damage, report Diandong Ren, of the University of Texas at Austin, and his colleagues, who used a computer model to predict the ecosystem impacts of the mudslides.

What's more, the vegetation destruction will lead to a loss of nitrogen from the quake-devastated region's ecosystem twice as large as the loss of that nutrient from California ecosystems because of the October 2007 wildfires there, Ren says. And, as the biomass buried by the China quake rots, 14 percent of the nitrogen will be spewed into the atmosphere as nitrous oxide, a pollutant typically released from agricultural operations, automobiles, and other sources.

The team will publish its findings on 4 March 2009 in Geophysical Research Letters, a journal of the American Geophysical Union (AGU).

Although landscapes devastated by the Chinese earthquake may re-green soon, the recovery will be cosmetic, says Ren. "From above, the area will look green in a few years, because grass grows back quickly, but the soil nutrients recover very slowly, and other kinds of plants won't grow," he says.

The magnitude-7.9 Wenchuan quake was followed by many aftershocks in the Sichuan Basin, an area that, because of its geological features – deep valleys enclosed by high mountains with steep slopes – is already prone to landslides. May is also the rainy season in Sichuan, and the combination of aftershocks and major precipitation events in the days following the earthquake caused severe mudslides. The avalanches killed thousands, destroyed roads and blocked rivers and access to relief, and shredded water and power stations, among other facilities. To predict ecosystem impacts of the mudslides, Ren and his collaborators applied a comprehensive computer model of landslides that incorporates several physical parameters, such as soil mechanics, root mechanical reinforcement (the root's grip of the dirt, which mitigates erosion), and precipitation.

Ren's model also shows that the primary mudslides following the earthquake removed large areas of nutrient-rich topsoil, leaving behind deep scars in the land that will take decades to recover, preventing the re-growth of vegetation.

The researchers write in their paper that, although being able to predict the location and timing of a mudslide is essential to mitigate its impacts, current mudslide models are not accurate enough.

"Previous approaches, which are mainly based on statistical approaches and empirical measures, have no predictive ability of where mudslides are going to happen," Ren says. His model, he claims, could be applied to forecast under what circumstances a landslide would occur at a specific location. He points out this would be particularly useful for places such as Southern California, where global warming predictions call for an increase in the frequency of these events.

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Notes for Journalists

As of the date of this press release, this study by Ren and his colleagues is still "in press" (i.e. not yet published).

Journalists and public information officers (PIOs) of educational and scientific institutions who have registered with AGU can download a PDF copy of a manuscript of this paper by clicking on this link: http://www.agu.org/journals/pip/gl/2008GL036702-pip.pdf.

Or, you may order a copy of the final, copy-edited and formatted PDF of the paper by emailing your request to Maria-José Viñas at mjvinas@agu.org or to Marc Airhart of University of Texas at Austin at mairhart@jsg.utexas.edu.

Please provide your name, the name of your publication, and your phone number.

(Beginning Wednesday, 4 March, registered news media and PIOs may directly download the final, copy-edited and formatted PDF of the paper by clicking on the following link: http://dx.doi.org/10.1029/2008GL036702)

If you need instructions for downloading, please see: http://www.agu.org/jinstructions.shtml.

Neither the paper nor this press release are under embargo.

Images:

A photograph showing a Chinese town affected by a mudslide is available by emailing Maria-José Viñas at mjvinas@agu.org

Title: "Mudslide-caused ecosystem degradation following Wenchuan earthquake 2008"

Authors: Diandong Ren and Rong Fu; Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas, USA;

Jiahu Wang: State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing, China. Also at School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, Oklahoma, USA;

David J. Karoly: School of Earth Sciences, University of Melbourne, Melbourne, Victoria, Australia;

Yang Hong: School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, Oklahoma, USA;

Lance M. Leslie: School of Meteorology, University of Oklahoma, Norman, Oklahoma, USA;

Congbin Fu and Gang Huang: Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.

Citation: Ren, D., J. Wang, R. Fu, D. J. Karoly, Y.Hong, L. M. Leslie, C. Fu, andG.Huang (2009), Mudslide-caused ecosystem degradation following Wenchuan earthquake 2008, Geophys. Res. Lett., 36, L05401, doi:10.1029/2008GL036702.

Contact information for author: Diandong Ren: +1 (512) 232-6273, DiandongRen1972@mail.utexas.edu



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