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instructions set forth in this manual before attempting to operate the equipment and conduct any maintenance. Your navigational echo sounder will perform to the utmost of its ability only if it is operated and maintained in accordance with the correct procedures. This equipment is designed, produced and documented by FURUNO ELECTRIC CO., LTD.,
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The FE-800 is a colour navigation echo sounder which operates with 50 or 200 kHz frequency. The FE-800 is comprised of a control unit, tran sceiver, matching box and transducer. Echoes are output on an 8.4-inch LCD screen. The main features of the FE-800 are: • Complies with the following regulations:
(50 kHz, 200 kHz) monochrome LCD echo sounder. Comprised of a display unit and a transducer, the LS-6100 displays underwater conditions on a bright 6-inch monochrome LCD. The main features of the LS-6100 are • Compact design permits installation where space is limited. • Bright 6-inch monochrome LCD gives excellent readability even in broad
The JFE-680 Echo-Sounder consists of a transducer mounted on the bottom of the ship's hull and a main unit that displays information on the depth and formation of the seabed. This information is gained by using ultrasonic waves sent from the transducer that are then reflected off the sea bottom and picked up again by the transducer.
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1. Introduction 1.1 Function The JFE-582 Echo-Sounder consists of a transducer mounted on the bottom of the ship's hull and a main unit that displays information on the depth and formation of the sea bottom.
monochrome LCD echo sounder. Comprised of a display unit and a transducer, the LS-4100 displays underwater conditions on a bright 5-inch monochrome LCD. The main features of the LS-4100 are • Bright 5-inch monochrome LCD gives excellent readability even in broad daylight. • Automatic function permits unattended adjustment of range and gain.
19 de out. de 2023 · The JFE-680 Echo-Sounder consists of a transducer mounted on the bottom of the ship's hull and a main unit that displays information on the depth and formation of the seabed. This information is gained by using ultrasonic waves sent from the transducer that are then reflected off the sea bottom and picked up again by the transducer.
