Can
you identify what's in this photo?
Each Wednesday morning
on Camp Lutherlyn's Facebook page
the Lutherlyn Environmental
Education Program posts a photo.
Readers
have all morning and afternoon
to
make their best guess about what the photo is.
Around
6 pm LEEP provides the answer and a brief explanation.
Each
week's What is it Wednesday post
will
also be posted on the Nature of Lutherlyn blog,
after it is posted on Facebook,
sometimes
with additional bonus information.
In
addition to bringing you current editions of What is it Wednesday
on the
Nature of Lutherlyn blog,
we
will be reposting old editions,
creating
a What is it Wednesday archive.
This
photo was posted as a What is it Wednesday on
February 19, 2020.
And
the answer is....
This is a spring polluted by abandoned coal mine drainage.
Lutherlyn’s property includes part of an abandoned coal mine
whose entrance tunnels, which ran horizontally into the hillside, have long
since collapsed. For many years this caused no problems, until orange water
started gushing out of the ground near the old mine entrance in the 1980’s.
When water collects underground in abandoned coal mines, it
sometimes dissolves minerals from those mines into the water. One of the minerals often found alongside coal in mines is iron sulfide, also known as pyrite or fool’s gold. When the water
seeps out of the mine, a chemical reaction happens between the water, the minerals
dissolved in it, and the oxygen in the air. That reaction consumes all of the
oxygen in the water and creates sulfuric acid and iron hydroxide. The iron hydroxide is the orange sediment visible in the water
(sometimes called “yellowboy”).
Low oxygen, high acidity, and thick iron
sediment make it impossible for aquatic animals to survive in such water.
Luckily, Lutherlyn has been able to treat this polluted
water with a passive wetland treatment system.
First, the water flows into a settling pond, either directly
from the mine through a pipe, or from streams created by springs like the one
pictured. Collecting the water in a large still pond allows much of the
sediment to settle and drop out of the water before it flows into the next part
of the treatment system.
After the settling pond, the water flows over a slope lined with
limestone, known as a limestone cascade. Here the water gets churned up as it
falls down the slope over the stones, which add oxygen to the water. The
limestone, which is alkaline – the opposite of acidic – reduces the acidity of
the water.
After the limestone cascade the water meanders through a
wetland filled with plants like cattails, which are natural filters. These
continue to remove excess iron and other minerals from the water as it flows
slowly through the wetland.
Finally, the water exits the wetland and joins the Semiconon
Creek, almost as clean as the unpolluted stream water. Treating the polluted
mine water with this system made it possible for the Semiconon Creek to be
removed from the list of impaired waters in Pennsylvania in 2008.
A story of pollution and damage to the earth
becomes a story of healing and restoration. This site also provides a great opportunity
for LEEP to teach students and others about water quality testing, the chemistry of abandoned mine pollution, and passive water treatment systems.
To learn how LEEP can help you discover more about ways we can care for the
earth and even help heal its wounds, through school field trips, summer camp, Saturday
Safaris and more, check out www.Lutherlyn.com/ee. Like and follow Camp Lutherlyn on
Facebook, to see What is it Wednesday posts when
they come out and have the opportunity to share your guesses in the comments!
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