Airplane De-Icing Agents Linked To Reduced Oxygen In
Groundwater
Spring is here and that means fewer airplanes need to be
de-iced. That may be good, according to a new study which finds that de-icing
agents accumulated during the winter, which end up on unpaved areas and
infiltrate into the soils during snowmelt, could end up in
groundwater.
This is not news. Airports in the developed world are
required to keep groundwater levels safe and the de-icing agents are filtered by
the natural self cleaning capacities of soil. Chemicals such as propylene glycol
and potassium formate are degraded by micro-organisms and don't get into the
groundwater.
But a new paper finds they could still have an impact,
because the microbes use oxygen to degrade the pollutants. As a consequence iron
and manganese oxides, which stabilize the intergranular cement of the structure
of the soil, dissolve.
For the study, researchers analyzed the soil
around the airport of the Norwegian capital Oslo. There, every winter about
1,000-1,500 tons of de-icing agents are used.
"At the same time, the
airport is situated directly next to the largest superficial aquifer in Norway,
the Romerike-Aquifer," explains PD Dr. Markus Wehrer from the Friedrich Schiller
University Jena.
The geoscientists took soil core samples close to the
runway of the airport and examined them and graduate student Heidi Lissner
explains loaded soil cores with water that contained de-icing chemicals and thus
simulated a "thawing event". She collected the seepage water after it passed
through the soil cores, followed by an examination for de-icing chemicals as
well as the oxygen content and additional parameters.
It's not a panic
situation and there are a number of solutions. Airports could install specific
areas which allow the thawing water to seep away in a controlled manner, making
for more controlled use of bacteria in the soil that degrade the chemicals.
Also, alternative substances, which can be used for the degradation of
pollutants similar to the way in which oxygen works, may be supplied. And the
texture of the soil could be shaped in a way that delays the seepage of the
polluted soil water. By using a longer interval, which is then available for the
degradation of the substances, a lack of oxygen could be avoided, because
atmospheric oxygen is transferred slowly but continuously into the soil.
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