Yesterday we retrieved the sediment traps that have been tethered
to the ocean floor for roughly four
months. This diagram illustrates the
rigging. There are a series of bottles
located under the large yellow funnels.
The bottles are on a timer that advances each of the many empty bottles
to the base of the funnel after a specified period of time. This
is the main reason we are out here. Dr.
Maureen Conte is the primary investigator of the Oceanic Flux Program (OFP)
time-series and has been for over 30 years.
The sediments collected in these traps tell us about the influence of the
ocean surface on the physical and biological processes over time scales of
weeks to decades and how particles flux in the water column. This hydrography
provides unprecedented opportunities to study the biology, chemistry, and ocean
physics especially over a long period of time.
Why is it important? Because this study helps us understand the reprocessing
of these particles, like carbon emissions, ocean acidification, or suspended plastics. The OFP is the longest running open-ocean
research of its kind dating back to 1978 and made possible through funding by
the National Science Foundation (NSF). Thank
you NSF!
Anika Aarons and Angela Tomassina prepare sediment trap. |
Today, we are 75 km SE of Bermuda. We returned the sediment traps to the sea with
fresh bottles. Anika Aarons, a grad
student at Mount Holyoke, assisted Maureen in the process. But it took all deck hands and marine techs
to launch these gigantic sinkable “rubber duckys” that require thousands of pounds
of steel, galvanized line, glass spheres the size of beach balls, and
waterproof instrumentation accompanied by a 2,400 lb. anchor. With all of this
heavy machinery and equipment on the aft deck, hardhats are a necessity. Anika will be ghost-blogging her experience
working on the OFP later today and I will share what we found in our surface sampling late last night.
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