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Full page fax print - International Seabed Authority

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2. EXPLORATION TOOLS AND SYSTEMS<br />

Marine mineral exploration programs for massive sulphides and cobalt-rich<br />

ferromanganese crusts require state-of-the-art multi-purpose research vessels that allow<br />

time and cost efficient exploration of large areas. A prerequisite are permanently<br />

installed multibeam swath mapping systems (up to 121 beams) which are capable of<br />

mapping the seafloor down to several thousand meters depth. Modern systems are able<br />

to map a swath width of more than 3 times the water depth along the ships track. Onboard<br />

computer processing usually produces a coloured or even 3D bathymetric map<br />

with down to 5 m contour intervals. In addition, ship-mounted sediment echosounder<br />

are being routinely used to determine the thickness and nature of the upper part of the<br />

sedimentary column, whereas seismic reflection surveys reveal information about the<br />

deeper part of the sedimentary pile. Side-scan sonar systems, which are towed behind<br />

the ship, obtain information about tectonic features at the seafloor. Gravity, magnetic,<br />

and heat flow surveys are also routinely run.<br />

On-line real-time observation of the seafloor in the search for hydrothermal<br />

sulphides at oceanic spreading ridges or for cobalt-rich ferromanganese crusts at<br />

seamount flanks is achieved by using deep-towed camera-systems (rated up to 5.000 m<br />

depth) which are equipped with lamps and flashes in combination with high-resolution<br />

colour video cameras and still cameras for up to 700 colour slides. The data transfer from<br />

the seafloor to the ship is achieved via a fibre optic cable while the energy for cameras,<br />

lamps and flashes is transmitted via a co-axial cable.<br />

Basic sampling devices include various corers (spade, piston and gravity corer)<br />

and dredges (barrel, box and chain-bag dredge) as well as free-fall grabs known from<br />

manganese nodule exploration. An excellent development is TV-guided grab systems<br />

(rated up to 5.000 m depth) for precise large-scale (up to about 3 tonnes) sampling of<br />

rocks, massive sulphides or cobalt crusts. Due to a high-resolution video camera and<br />

several lights mounted in the centre of the grab, the system can be used for small scale<br />

mapping of the seafloor as well as for sample selection and finally sampling. If the<br />

sample is not sufficient, the grab can be reopened and closed several times before the<br />

batteries are exhausted and need to be recharged. TV-grabs are usually also operated on<br />

a fibre optic cable to enhance the camera signal and to trigger the closing and opening<br />

mechanism of the grab. The power necessary to close and open the claws, however, is<br />

provided by deep-sea batteries.<br />

For water sampling in the search for geochemical signals (methane, manganese,<br />

helium isotopes) of active hydrothermal vents, several CTD (conductivity-temperaturedepth)<br />

and rosette sampler systems with up to 24 bottles are in use. Each bottle can be<br />

closed remotely at a certain water depth. Chemical analyses of the water samples are<br />

usually performed on board ship with only limited time delays. In recent years,<br />

<strong>International</strong> <strong>Seabed</strong> <strong>Authority</strong> 93

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