2016
DOI: 10.1080/01691864.2015.1093428
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Map segmentation for simultaneous localization and mapping in ruins

Abstract: The distribution of environmental features of the internal ruins which are formed by a randomly seismic disaster is unpredictable. Therefore, the existing methods of map segmentation, which need to preset parameters, cannot be directly used. Considering the lack of prior knowledge, a map segmentation method based on the spectral clustering is proposed in the framework of hierarchical simultaneous localization and mapping (SLAM) algorithm. The method solves the problem of incremental complexity of SLAM algorith… Show more

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Cited by 3 publications
(1 citation statement)
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“…Quite interestingly, this is a demonstration of the surface reduction of V from V 5+ to V 4+ as reported by Rossell et al 123 , which was attributed to the presence of intrinsic surface defects in the form of oxygen vacancies that directly impact the electronic structure of monoclinic scheelite BiVO4. Meanwhile, a deconvolution procedure applied to the O 1s spectrum reveals that the O species are divided into oxygen due to the lattice structure, the non-lattice oxygen, and oxygen due to adsorbed molecules 122,124 . The deconvoluted O 1s peak at 529.2 eV is assigned to oxygen in a BiVO4 lattice environment, while the peaks at 530.3 eV and 532.0 eV are assigned to non-lattice and adsorbed oxygen species 125 , respectively.…”
Section: Effect Of Various Factors On Physico-chemical Propertiesmentioning
confidence: 99%
“…Quite interestingly, this is a demonstration of the surface reduction of V from V 5+ to V 4+ as reported by Rossell et al 123 , which was attributed to the presence of intrinsic surface defects in the form of oxygen vacancies that directly impact the electronic structure of monoclinic scheelite BiVO4. Meanwhile, a deconvolution procedure applied to the O 1s spectrum reveals that the O species are divided into oxygen due to the lattice structure, the non-lattice oxygen, and oxygen due to adsorbed molecules 122,124 . The deconvoluted O 1s peak at 529.2 eV is assigned to oxygen in a BiVO4 lattice environment, while the peaks at 530.3 eV and 532.0 eV are assigned to non-lattice and adsorbed oxygen species 125 , respectively.…”
Section: Effect Of Various Factors On Physico-chemical Propertiesmentioning
confidence: 99%