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  • Chaos  (1)
  • Gravity, Geodesy and Tides  (1)
  • Key words statics  (1)
  • 1
    Electronic Resource
    Electronic Resource
    Static analysis of a two-member linkage interacting with a given surface (1999)
    Springer
    Archive of applied mechanics 69 (1999), S. 429-442 
    Details
    ISSN: 1432-0681
    Keywords: Key words statics ; two-member linkage ; Coulomb friction ; robotics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Summary The static interaction of a two-member linkage with a given surface is investigated. Dry friction acts at the point of contact of the linkage with the surface. The linkage has two drives generating torques at its joints. The optimal distribution of the joint torques is determined to maximize the friction force at the point of contact. The dependence of this maximal force on the lengths of the links and on the linkage configuration is investigated. The results obtained can be applied to the analysis and optimization of various robotic systems, in particular, manipulators interacting with rough surfaces and walking machines, especially tube-crawling robots.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s004190050232
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    Description of chaotic motion by an invariant probability density (1991)
    Springer
    Nonlinear dynamics 2 (1991), S. 291-304 
    Details
    ISSN: 1573-269X
    Keywords: Chaos ; Fokker-Planck-Equation ; probability density ; global description of motion
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mathematics
    Notes: Abstract An observation of single trajectories exhibiting chaotic motion turns out to be disadvantageous because even smallest variations of the initial conditions grow exponentially in time and result in an unpredictable long-time behaviour. The paper gives a different approach based on a probability distribution of the state space variables which is invariant on the area of attraction and results in a global description of chaotic motion.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00045298
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  • 3
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    Generalized model for a Moho inversion from gravity and vertical gravity-gradient data (2016)
    Oxford University Press
    Details
    Publication Date: 2016-08-14
    Description: Seismic data are primarily used in studies of the Earth's lithospheric structure including the Moho geometry. In regions, where seismic data are sparse or completely absent, gravimetric or combined gravimetric-seismic methods could be applied to determine the Moho depth. In this study, we derive and present generalized expressions for solving the Vening Meinesz–Moritz's (VMM) inverse problem of isostasy for a Moho depth determination from gravity and vertical gravity-gradient data. By solving the (non-linear) Fredholm's integral equation of the first kind, the linearized observation equations, which functionally relate the (given) gravity/gravity-gradient data to the (unknown) Moho depth, are derived in the spectral domain. The VMM gravimetric results are validated by using available seismic and gravimetric Moho models. Our results show that the VMM Moho solutions obtained by solving the VMM problem for gravity and gravity-gradient data are almost the same. This finding indicates that in global applications, using the global gravity/gravity-gradient data coverage, the spherical harmonic expressions for the gravimetric forward and inverse modelling yield (theoretically) the same results. Globally, these gravimetric solutions have also a relatively good agreement with the CRUST1.0 and GEMMA GOCE models in terms of their rms Moho differences (4.7 km and 4.1 km, respectively).
    Keywords: Gravity, Geodesy and Tides
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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