History | |
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Name | |
Owner | 2E Maritime, Istanbul, Turkey |
Builder | Sønderborg Skibsværft A/S, Sønderborg, Denmark |
Launched | January 12, 1974 |
Commissioned | May 1, 1974 |
Homeport | Istanbul, Turkey |
Identification | |
Status | Active |
General characteristics | |
Class and type | 100-A-1.1-Nav IL; Ap; ST |
Tonnage | |
Length | 78.80 m (258 ft 6 in) |
Beam | 13.25 m (43 ft 6 in) |
Draft | 4.16 m (13 ft 8 in) |
Depth | 6.00 m (19 ft 8 in) |
Installed power | 1,589 kW (2,131 hp) |
Propulsion | Alpha B&W 16V23HU - 4S 16cyl-Vee 225 x 300 Trp 750 rpm |
Speed |
|
Armament | None |
The RV Denar 2 is a Turkish research and survey vessel owned by TOMA Maritime S.A. Istanbul, Turkey and operated 2E Maritime in Istanbul, Turkey. [1]
She was built by Sønderborg Skibsværft A/S in Sønderborg, Denmark. Christened Leila Bech, she was launched on January 12, 1974, and was commissioned under the Danish flag on May 1, 1974. After sailing under the Panamas and Ilaian flags, she was finally purchased by the Turkish private maritime company in October 2013 as the first and so far the only non-governmental vessel of her kind. [1] [2] She was renamed "Denar", short for "Deniz Araştırmaları" (literally: sea surveys).
She made her first operation in the Mediterranean Sea for the Northern Cyprus Water Supply Project, an international water diversion project designed to supply water for drinking and irrigation from southern Turkey to Northern Cyprus via undersea pipeline. With the help of her two remotely operated underwater vehicles (ROV), she was put into service at the construction projects of Marmaray, İzmit Bay Bridge and Yavuz Sultan Selim Bridge in addition to deep sea surveys. [2]
Denar 2 is 78.80 m (258 ft 6 in) long, with a beam of 13.25 m (43 ft 6 in) and a max. draft of 4.16 m (13 ft 8 in). Assessed at 2,033 GT, 2,997 DWT and 610 NT, the ship is propelled by a 1,589 kW (2,131 hp) diesel engine of type Alpha Burmeister & Wain 16V23HU - 4S 16cyl-Vee 225 x 300 Trp 750 rpm. She has a top speed of 11 knots (20 km/h) with 10 knots (19 km/h) in service. [3] [4]
She has capabilities for bathymetric surveys, oceanographic surveys, geological surveys, geophysical surveys and geotechnical engineering. Furthermore, she can be used in coastal management and ocean engineering applications such as submarine pipeline applications and for dredging services. [3]
She has three cranes capable of lifting loads between 3.5–10 tonnes, and an A-frame for 20 tonnes. She is equipped with following instrumentation: [3]
She carries two ROVs: [5]
Work-class ROV (TRV-HD) capable of diving up to 1,000 m (3,300 ft) and carrying payloads up to 136 kg (300 lb):
Image-class ROV (Saab Seaeye Falcon) with diving capability of up to 300 m (980 ft):
She features the following equipment: [3]
Multibeam echosounder (Kongsberg EM 1002)
She has following capabilities: [3]
Positioning system: [3] (Kongsberg-Simrad SDP 11),
Hydrographic survey systems: [3]
Oceanographic/meteorological survey systems: [3]
Geophysical survey systems: [3]
Geological survey and geotechnical systems: [3]
Software: [3]
The Challenger Deep is the deepest known point of the seabed of Earth, located in the western Pacific Ocean at the southern end of the Mariana Trench, in the ocean territory of the Federated States of Micronesia. According to the GEBCO Gazetteer of Undersea Feature Names the depression's depth is 10,920 ± 10 m (35,827 ± 33 ft) at 11°22.4′N142°35.5′E, although its exact geodetic location remains inconclusive and its depth has been measured at 10,902–10,929 m (35,768–35,856 ft) by deep-diving submersibles, remotely operated underwater vehicles, benthic landers, and sonar bathymetry. The differences in depth estimates and their geodetic positions are scientifically explainable by the difficulty of researching such deep locations.
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Echo sounding or depth sounding is the use of sonar for ranging, normally to determine the depth of water (bathymetry). It involves transmitting acoustic waves into water and recording the time interval between emission and return of a pulse; the resulting time of flight, along with knowledge of the speed of sound in water, allows determining the distance between sonar and target. This information is then typically used for navigation purposes or in order to obtain depths for charting purposes.
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Sodar, an acronym of sonic detection and ranging, is a meteorological instrument used as a wind profiler based on the scattering of sound waves by atmospheric turbulence. Sodar equipment is used to measure wind speed at various heights above the ground, and the thermodynamic structure of the lower layer of the atmosphere.
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Dr. Fred Noel Spiess was a naval officer, oceanographer and marine explorer. His work created new advances in marine technology including the FLIP Floating Instrument Platform, the Deep Tow vehicle for study of the seafloor, and the use of acoustics for underwater navigation and geodetic positioning.
Underwater acoustics is the study of the propagation of sound in water and the interaction of the mechanical waves that constitute sound with the water, its contents and its boundaries. The water may be in the ocean, a lake, a river or a tank. Typical frequencies associated with underwater acoustics are between 10 Hz and 1 MHz. The propagation of sound in the ocean at frequencies lower than 10 Hz is usually not possible without penetrating deep into the seabed, whereas frequencies above 1 MHz are rarely used because they are absorbed very quickly.
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The Newtsuit is an atmospheric diving suit designed and originally built by Phil Nuytten.
Acoustic seabed classification is the partitioning of a seabed acoustic image into discrete physical entities or classes. This is a particularly active area of development in the field of seabed mapping, marine geophysics, underwater acoustics and benthic habitat mapping. Seabed classification is one route to characterizing the seabed and its habitats. Seabed characterization makes the link between the classified regions and the seabed physical, geological, chemical or biological properties. Acoustic seabed classification is possible using a wide range of acoustic imaging systems including multibeam echosounders, sidescan sonar, single-beam echosounders, interferometric systems and sub-bottom profilers. Seabed classification based on acoustic properties can be divided into two main categories; surficial seabed classification and sub-surface seabed classification. Sub-surface imaging technologies use lower frequency sound to provide higher penetration, whereas surficial imaging technologies provide higher resolution imagery by utilizing higher frequencies.
ABISMO is a remotely operated underwater vehicle (ROV) built by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) for exploration of the deep sea. It is the only remaining ROV rated to 11,000-meters, ABISMO is intended to be the permanent replacement for Kaikō, a ROV that was lost at sea in 2003.
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An underwater survey is a survey performed in an underwater environment or conducted remotely on an underwater object or region. Survey can have several meanings. The word originates in Medieval Latin with meanings of looking over and detailed study of a subject. One meaning is the accurate measurement of a geographical region, usually with the intention of plotting the positions of features as a scale map of the region. This meaning is often used in scientific contexts, and also in civil engineering and mineral extraction. Another meaning, often used in a civil, structural, or marine engineering context, is the inspection of a structure or vessel to compare actual condition with the specified nominal condition, usually with the purpose of reporting on the actual condition and compliance with, or deviations from, the nominal condition, for quality control, damage assessment, valuation, insurance, maintenance, and similar purposes. In other contexts it can mean inspection of a region to establish presence and distribution of specified content, such as living organisms, either to establish a baseline, or to compare with a baseline.
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