Development of DONET2 — Off Kii chanel observatory network
Katsuyoshi KawaguchiEiichiro ArakiY. KogureNarumi TakahashiTakeshi KatayamaK. HishikiNoriyuki FujiwaraNaoki IIDAY. Kaneda
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DONET is a flexible and expandable submarine cabled seafloor observation infrastructure for mega-thrust earthquake research and disaster prevention. The system which consists of a backbone looped submarine cable system, five science nodes and 20 set of state of art earthquake and tsunami observatories was developed and constructed in the program started from 2006 and fully in operation from 2011 at the hypothesis region of To-Nankai earthquake. Simultaneously with the construction of original DONET, the development and deployment of second DONET system (DONET2) was planned and started in 2010 to subject for the hypothesis region of Nankai earthquake. Since this region spreads out in the wide area about 2 times rather than the region of the To-Nankai earthquake, deployment of a large-scale observation network system is required. Expansion of scale of observatory means the increase of power distribution capacity and the confliction of network topology, it will need to solve the several engineering subject to expand the design of original DONET to large scale system DONET2. This paper describe several indispensable technologies of submarine cabled seafloor observation system DONET (power consumption control, power blanching and time synchronization), then introduce the novel engineering approach for high voltage power distribution control and large scale network topology management for DONET2 off Kii channel observatory network.Keywords:
Seafloor Spreading
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: Introduction The Problem Fieldwork Measurements: The Approach The First Two Deployments Third Deployment, September 1989 to June 1990 Fourth Deployment, November 1993 to April 1994 Results from Third Deployment Results from Fourth Deployment Further Work Acknowledgements
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‘Seafloor spreading and magnetic anomalies’ begins with the Vine–Matthews Hypothesis, which proposed that strips of seafloor parallel to the mid-ocean ridges, where two plates diverge from one another, were magnetized in opposite directions because the Earth’s field had reversed itself many times. A test of the Vine–Matthews Hypothesis, which required determining the age of the seafloor, became a test of seafloor spreading. Dating the ocean floor using magnetic anomalies detected by magnetometers towed behind ships and core samples extracted during the Deep-Sea Drilling Project confirmed the hypothesis. With magnetic anomalies to date the seafloor and a curve relating seafloor depth and age, the difference between the Atlantic, with its ‘ridge’, and the Pacific and its ‘rise’ became comprehensible. With a theory for predicting the depths of oceans, it was also possible to understand the history of sea-level changes.
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