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Science
Report:
Today we are
getting our first look at the hydrothermal activity here at Axial Volcano.
We use two types of operations to map and sample hydrothermal plumes.
The simplest one is called a vertical cast. The ship holds position over
a location on the seafloor and we lower our instruments slowly down through
the water column to within a few meters of the seafloor. The principal
instrument package we use is called a "CTD." This acronym stands for "conductivity
(an indication of seawater salinity), temperature, and depth" for the
primary data that is measured. We also have instruments that measure the
turbidity of the water, which estimates the concentration of particulate
matter. In addition to these instruments the CTD holds 21 special plastic
bottles that each capture 20 liter (about 5 gallons) samples of seawater.
At the end of the cast, when the CTD is returned to the ship's deck, scientists
on board take samples from each bottle to analyze for a variety of chemicals
added to the water by hydrothermal venting.
The second operation is
called a tow-yo and uses the same equipment as on a vertical cast. But
instead of the ship holding a position, in a tow-yo we are slowly moving
through the water at a speed of about 1.5 knots. While the ship is moving
we are also raising and lowering the CTD using the winch, so that the
path of the CTD above the seafloor traces a sawtooth pattern. This technique
allows us to obtain more detailed information about the distribution of
hydrothermal plumes over a wide area. Some tows last up to 12 hours along
a track line almost 20 miles long.
Our first view of the plumes
here at Axial has shown that venting is still active, more than 2 and
a half years after the volcanic eruption in January 1998. However, even
by looking at just a few casts we can see that the intensity of the venting
is less than last year. This change agrees with our hypothesis that hydrothermal
activity is most intense immediately after an eruption, decreases quickly
afterwards, and then continues to decline at a slower rate for several
years. We will continue to map the distribution of the plumes in the coming
days.
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Deployment
of the CTD to monitor hydrothermal plume emmissions.
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