The findings indicate that the drier conditions brought about by a warming climate will cause the soil to relinquish its hold on hundreds of years of mercury accumulation, sending that mercury back into the air at levels up to 15 times greater than originally calculated. "While peat lands are typically viewed as very wet and stagnant places, they do burn in continental regions, especially late in the season when water tables are depressed," explained Turetsky. "When peat lands burn, they can release a huge amount of mercury that overwhelms regional atmospheric emissions. Our study is new in that it looks to the soil record to tell us what happens when peat soil burns, soil that has been like a sponge for mercury for a long time."
Monday, August 28, 2006
Forget The Thermometer, The Mercury Really Is Rising
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