A Graph Matching and Energy Minimization Based Algorithm for Lunar Surface Image Mosaic

2015 ◽  
pp. 46-55 ◽  
Author(s):  
Chuan Li ◽  
Zhi-Yong Liu ◽  
Xu Yang ◽  
Hong Qiao ◽  
Chuan-Kai Liu
Keyword(s):  
Lunar Surface ◽  
Energy Minimization ◽  
Graph Matching ◽  
Image Mosaic ◽  
Surface Image

Graph-Based Registration and Blending for Undersea Image Stitching

Robotica ◽  
2019 ◽  
Vol 38 (3) ◽  
pp. 396-409 ◽  
Author(s):  
Xu Yang ◽  
Zhi-Yong Liu ◽  
Hong Qiao ◽  
Jian-Hua Su ◽  
Da-Xiong Ji ◽  
...  
Keyword(s):  
Energy Minimization ◽  
Moving Objects ◽  
Graph Matching ◽  
Structural Information ◽  
Ocean Current ◽  
Image Stitching ◽  
Local Disturbance ◽  
Markov Random ◽  
Integer Quadratic Programming ◽  
Quadratic Programming Problems

SummaryImage stitching is important for the perception and manipulation of undersea robots. In spite of a well-developed technique, it is still challenging for undersea images because of their inevitable appearance ambiguity caused by the limited light in the undersea environment, and local disturbance caused by moving objects, ocean current, etc. To get a clean and stable background panorama in the undersea environment, this paper proposes an undersea image-stitching method by introducing graph-based registration and blending procedures. Specifically, in the registration procedure, matching the features in each undersea image pair is formulated and solved by graph matching, to incorporate the structural information between features. In the blending procedure, an energy function on the indirect graph Markov random field is proposed, which takes both image consistency and neighboring consistency into consideration. Coincidentally, both graph matching and energy minimization can be mathematically formulated by integer quadratic programming problems with different constraints; the recently proposed graduated nonconvexity and concavity procedure is used to optimize both problems. Experiments on both synthetic images and real-world undersea images witness the effectiveness of the proposed method.

scholarly journals Novel Image Mosaic Algorithm for Concrete Pavement Surface Image Reconstruction

2013 ◽  
Vol 96 ◽  
pp. 2692-2697 ◽  
Author(s):  
Hua Wang ◽  
Xin Liu ◽  
Shen Zhang ◽  
Wei Quan
Keyword(s):  
Image Reconstruction ◽  
Concrete Pavement ◽  
Image Mosaic ◽  
Pavement Surface ◽  
Surface Image

scholarly journals Introducing locally affine-invariance constraints into lunar surface image correspondence

2016 ◽  
Vol 186 ◽  
pp. 258-270 ◽  
Author(s):  
Yu-Ren Zhang ◽  
Xu Yang ◽  
Hong Qiao ◽  
Zhi-Yong Liu ◽  
Chuan-Kai Liu
Keyword(s):  
Lunar Surface ◽  
Affine Invariance ◽  
Image Correspondence ◽  
Surface Image

The Geosciences Applied to Lunar Exploration

1962 ◽  
Vol 14 ◽  
pp. 169-257 ◽  
Author(s):  
J. Green
Keyword(s):  
Lunar Surface ◽  
Probable Mechanism ◽  
Point Of View ◽  
Lunar Exploration ◽  
Geological Model ◽  
Apply Geophysics ◽  
Surface Features ◽  
The Impact

The term geo-sciences has been used here to include the disciplines geology, geophysics and geochemistry. However, in order to apply geophysics and geochemistry effectively one must begin with a geological model. Therefore, the science of geology should be used as the basis for lunar exploration. From an astronomical point of view, a lunar terrain heavily impacted with meteors appears the more reasonable; although from a geological standpoint, volcanism seems the more probable mechanism. A surface liberally marked with volcanic features has been advocated by such geologists as Bülow, Dana, Suess, von Wolff, Shaler, Spurr, and Kuno. In this paper, both the impact and volcanic hypotheses are considered in the application of the geo-sciences to manned lunar exploration. However, more emphasis is placed on the volcanic, or more correctly the defluidization, hypothesis to account for lunar surface features.

A Photographic Map of the Moon

1962 ◽  
Vol 14 ◽  
pp. 113-115
Author(s):  
D. W. G. Arthur ◽  
E. A. Whitaker
Keyword(s):  
Lunar Surface ◽  
The Moon ◽  
Map Projection

The cartography of the lunar surface can be split into two operations which can be carried on quite independently. The first, which is also the most laborious, is the interpretation of the lunar photographs into the symbolism of the map, with the addition of fine details from telescopic sketches. An example of this kind of work is contained in Johann Krieger'sMond Atlaswhich consists of photographic enlargements in which Krieger has sharpened up the detail to accord with his telescopic impressions. Krieger did not go on either to convert the photographic picture into the line symbolism of a map, or to place this picture on any definite map projection.

The effects of surface absorbed monolayer microdiffraction patterns

1988 ◽  
Vol 46 ◽  
pp. 680-681
Author(s):  
M. Pan ◽  
J.M. Cowley
Keyword(s):  
Surface Potential ◽  
Electron Probe ◽  
Potential Distribution ◽  
Crystal Surface ◽  
Normal Direction ◽  
Surface Image ◽  
Extended Surface ◽  
Gas Molecules ◽  
Surface Nature ◽  
Electron Microdiffraction

Electron microdiffraction patterns, obtained when a small electron probe with diameter of 10-15 Å is directed to run parallel to and outside a flat crystal surface, are sensitive to the surface nature of the crystals. Dynamical diffraction calculations have shown that most of the experimental observations for a flat (100) face of a MgO crystal, such as the streaking of the central spot in the surface normal direction and (100)-type forbidden reflections etc., could be explained satisfactorily by assuming a modified image potential field outside the crystal surface. However the origin of this extended surface potential remains uncertain. A theoretical analysis by Howie et al suggests that the surface image potential should have a form different from above-mentioned image potential and also be smaller by several orders of magnitude. Nevertheless the surface potential distribution may in practice be modified in various ways, such as by the adsorption of a monolayer of gas molecules.

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