"We went to fourteen small patches of remnant native prairie that still exist in Iowa, Minnesota, South Dakota, Nebraska and Kansas, and used a hand auger to collect deep soil cores, in material that dates back to the last Ice Age," says Isaac Larsen, professor of geosciences at UMass Amherst and the paper's senior author.
"We brought this soil back to our lab at UMass, sifted it to isolate individual sand grains, removed everything that wasn't quartz, and then ran these few spoonfuls through a chemical purification process to separate out the 10Be —which was just enough to fit on the head of a pin."
This sample was then sent to a lab which counted the individual 10Be atoms, from which Larsen and his colleagues calculated a precise rate of erosion, stretching from the present day all the way back to the last Ice Age, about 12,000 years ago.
"For the first time, we know what the natural rates of erosion are in the Midwest," says Caroline Quarrier, the paper's lead author and who completed this research as part of her master's thesis at UMass Amherst. "And because we now know the rate of erosion before Euro-American settlement, we can see exactly how much modern agriculture has accelerated the process."
The numbers are not encouraging. "Our median pre-agricultural erosion rate across all the sites we sampled is 0.04 mm per year," says Larsen. Any modern-day erosion rate higher than that number means that soil is disappearing faster than it is accumulating.
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