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Vol. 11 (2008 year), No. 3
Suslov A.N., Men'shikov V.I., Koval'chuk V.V.
Comparative analysis of efficiency of vessel radio-locators and thermal locators for safety navigation
The analysis of statistical data processing of quantitative thermography (thermovision) diagnostics of contact connections of electric equipment has been considered. The operational parameters of reliability have been obtained as a result of the appropriate statistical processing
(in Russian, стр.2, fig. 0, tables. 0, ref 0, Adobe PDF, Adobe PDF 0 Kb)
Vol. 12 (2009 year), No. 2
Kalityonkov A.N., Suslov A.N., Kalityonkov N.V., Milkin V.I., Kuchura A.N., Ivanyugin M.S.
On optimum navigation in ice conditions. Using of thermal radar
In this paper software agents' communication models and algorithms in the virtual business environment have been proposed. They allow to reduce response time on any changes of environment imitating the innovation field due to increase of data exchange between the agents and reduction of general network load. Two mechanisms for conversion of inter-node agent communications to intra-node agent communications and dynamic agent distribution have been represented. Various implementation approaches for agent communication and interaction mechanisms have been considered. Methods for effectiveness increase of data exchange between mobile agents in the distributed system for information support of innovations have been proposed. Data exchange mechanisms between software agents in the virtual business environment based on agent address structure extension and using of middle-agents brokering and matchmaking services have been minutely described.
(in Russian, стр.4, fig. 0, tables. 0, ref 0, Adobe PDF, Adobe PDF 0 Kb)
Vol. 12 (2009 year), No. 2
Suslov A.N., Pyatsi A.H., Kalityonkov N.V.
Prospects of thermal radars' application on vessels in modern conditions of navigation
In this paper the authors have analyzed the problem of finding the minimum of time for passing through the ice area of the navigation route provided that the density of ice is a function of both coordinates.
(in Russian, стр.11, fig. 24, tables. 1, ref 2, Adobe PDF, Adobe PDF 0 Kb)