OCEANOGRAPHY TOOLS Some of the types of equipment



















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OCEANOGRAPHY TOOLS Some of the types of equipment oceanographers use to do research.
GRAVITY CORE • The most basic • sampling device used to collect core samples from the seafloor. It penetrates up to 10 meters into the sediment.
SECCHI DISK • Used to estimate the • transparency of seawater. Can give a relative measure of productivity or turbidity.
DIP NET • Useful for scooping up seaweed, jellyfish and other drifting organisms from docks or the side of a vessel.
SEDIMENT SIEVES • Used to analyze sediment grain size composition.
PLANKTON NETS • A fine mesh net. • Collects small plant • and animal plankton. Typically towed behind or to the side of a vessel.
NEUSTON NET • Used to collect organisms and other particulates from the surface to about 1 ½ feet down.
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NISKIN BOTTLE • Used to collect • water samples from specific depths. The “messenger” triggers the valves to close.
CAROUSEL • A device used for • deploying multiple sensory devices at one time. Devices may include: oxygen sensors, niskin bottles, salinometers, conductivity meters, depth sensors, etc…
HYDROPHONE • A microphone for acoustic measurements in fluids.
BOTTOM (SHIPEK) GRAB SAMPLER • Used to take samples • from off the ocean floor. Sediment, as well as any organisms on the substrate will be collected when it closes.
DREDGE • Used to catch • organisms living on the ocean floor and right above it. Towed behind the vessel.
HYDROMETER • Device used to • measure the densities of liquid and solutions. Salinity levels are determined with this instrument.
GLOBAL POSITIONING SYSTEM (GPS) • A worldwide radio- navigation system that uses satellites to triangulate your location on earth.
ROV’S (Remotely Operated Underwater Vehicles) • Unoccupied, highly maneuverable underwater robots operated by a person aboard a surface vessel.
TUCKER TRAWL • Used to collect • samples at various depths. Insures that only what is caught in the net is at the specified depth. • http: //www. youtub e. com/watch? v=qh 5 x. Oh. GBK 0 A