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General Overview of
Project
The coal tar that is currently
being removed from the former Oneonta Manufactured Gas Plant
site is being done so by certified professionals who
approach the clean up using certified and closely monitored
methods. The pits that are dug by the engineers are done so
after careful calculations are made based on where the left
over coal tar is and where it has moved to. In order to
decide where the pits are dug it is imperative to take the
geology and hydrology of the area into
consideration.

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The above
image displays where the remediation site is located within
Oneonta New York
The geology of an area does not just include the
rocks, but the unconsolidated overburden (soil and
unconsolidated sediments). Differences in geology can
drastically change the way viscous mediums, like water, oil
or in this case the coal tar, move though the ground. For
example, water will move more easily though gravel (larger
sediment) than it will clay or silt (smaller sediment). This
is because there are large spaces in between each gravel
grain and there are very small spaces in between clays and
silts. Imagine having a container of gumballs and a
container of baking flour. If you were to dump equal amounts
of water into the containers the one with the gumballs would
have water reach the bottom first. Using this information we
can calculate an estimate of approximately how fast liquids
are moving though the ground. We get geologic information of
what is below ground from well logs. When a well is put into
the ground a record is made of all the geology that the well
passes through.
The hydrology of the area includes all things
having to do with water. This includes rivers, streams,
lakes, rain and water wells. The hydrology of the area is
important, especially the ground water, because some of the
components of the coal tar dissolve in water. Water
infiltrates though the overburden (soils/sediment) and down
to a saturated zone in the soil, or the aquifer. The aquifer
stores water, but the water is constantly moving. The ground
water moves considerably slower than surface water in a
river or stream does. Water is known as the universal
solvent, meaning that almost everything dissolves in water,
so if there is dissolution taking place then is an important
factor in the proper clean-up. The water table (the top of
the area saturated with ground water) changes during the
year, so it is very important to know how deep the water
table is. For example, if you need to dig a hole 25 deep but
the water table is only 20 feet below the ground, you may
have some issues.
Another piece of the puzzle is the geography of
the area, or the topography and general shape of the land in
the area. This includes the hills, flat flood planes and
other terrain. The topography is based on the geology of the
area and the geologic processes that happened in the past.
For example glaciers carved out the U-shaped valleys that we
see today in Oneonta. The ground water will flow much like
surface water, from areas of high elevation to areas of low
elevation, only much slower.
Overall, digging the coal tar out of the ground
is a complex job that could not be done properly without an
understanding of the geology and hydrology of the area. For
example, what would happen if they started to dig a hole
with an excavator and encountered sandstone bedrock 5 feet
down? The excavator could not be used to take out bedrock,
so they would need to find a different way to clean up the
site. The contaminant and ground water would have traveled
though the ground differently if it was moving though
sandstone bedrock instead of unconsolidated sediments.
Engineers would not know how far the coal tar has traveled
over a period of time, where it has gone or what it has done
if they did not know what type of geology it is moving
though. They also would not know if ground water was
affecting its transport. The geology and the hydrology of an
area are interconnected and are impetrative information in
order to make the clean-up effort successful.
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