Water
quality relates to both geology/nature, as well as human beings, in a multitude
of different ways. Geologists are interested in water quality, because of its relation
to nature within the critical zone, which inherently has different levels of effects
on humans in society. There are a number of issues, in terms of water quality,
related to geology, for example, geologists have been measuring water for
decades, conducting millions of measurements and analyses that have brought
endless data on water quality. These measurements often times find something
important about the water and the environment around it. For instance, these measurements
find out the water ways properties, and the implications that these properties
pose for the water way, as well as, the way these properties vary over time.
So, if for example, the levels of the PH, conductivity, temperature, dissolved oxygen,
nitrate or othro-phosphate begin to change from the results of the measurements
taken from samples, than one can deduct that that something is going on
somewhere that is affecting the water, and possibly, the water quality, which
naturally can have negative implications for humans, since our very survival
relies on water and its quality.
I graphed the parameter of
measurements of conductivity in the Mad River for the most recent 12-month
consecutive period. Conductivity is the amount of dissolved material in water
and is a measure of the ability of water to pass an electrical current.
Furthermore, conductivity is linked directly to the total dissolved solids that
are present in the water. As the webpage http://water.epa.gov/type/rsl/monitoring/vms59.cfm
states, “The conductivity of rivers in the United States generally ranges from
50 to 1500 µmhos/cm. Studies of inland fresh waters indicate that streams
supporting good mixed fisheries have a range between 150 and 500 µhos/cm.
Conductivity outside this range could indicate that the water is not suitable
for certain species of fish or macro invertebrates. Industrial waters can range
as high as 10,000 µmhos/cm.” The graph of the data from the measurements of
conductivity in the Mad River for the most recent 12 month consecutive periods
trends, or lack thereof, correspond with this research.
As one can see looking at the graph
and having the knowledge of the dates when this data was taken, which are, 1)
6/23/2009, 2) 6/30/2009, 3) 7/7/2009, 4) 7/14/2009, 5) 7/21/2009, 6) 7/29/2009,
7) 8/3/2009, 8) 8/11/2009, 9) 8/18/2009, 10) 8/24/2009, 11) 8/31/2009, 12)
9/28/2009. Since this data set was measured during the months of June, July,
August and September, the scatterplot isn’t exactly constant; however they do
follow the seasonal trends, meaning that they are all quite moderate, because
of the months that this data set is taken from. However, there are high levels
of conductivity in low flow during the summer months and low conductivity when
it rains, and pollution, as well as groundwater, can affect the conductivity in
a stream or river, like Mad River.
Stefan
Latham