1993
DOI: 10.1006/ciun.1993.1007
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Geometry-Limited Diffusion in the Characterization of Geometric Patches in Images

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Cited by 34 publications
(11 citation statements)
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“…This is accomplished by letting the scale for boundariness be defined not according to the time of a uniform diffusion equation (the variance of a Gaussian envelope) but according to the time of a variable-conductance diffusion equation. [25], where the conductance is monotonic decreasing with the medialnessbased boundariness. This behaves as though the space near object boundaries is stretched before the medialness measures are made.…”
Section: Boundariness-medialness Interactionsmentioning
confidence: 99%
See 1 more Smart Citation
“…This is accomplished by letting the scale for boundariness be defined not according to the time of a uniform diffusion equation (the variance of a Gaussian envelope) but according to the time of a variable-conductance diffusion equation. [25], where the conductance is monotonic decreasing with the medialnessbased boundariness. This behaves as though the space near object boundaries is stretched before the medialness measures are made.…”
Section: Boundariness-medialness Interactionsmentioning
confidence: 99%
“…Boundariness at a particular location x and scale a has typically been associated with variations in luminance about that location, i.e., with combinations of first or second partial derivatives in some direction u of the intensity function after convolution with a Gaussian with standard deviation o-(see [4], Sobel's method in [7], and [25]). However, there are many other possible cues to boundariness.…”
Section: Multiscale Geometry Detectorsmentioning
confidence: 99%
“…Several features indicate the boundaries of planar patches: step edges (gradient magnitude) of amplitude, step edges of range, and step edges in the surface normal. The smoothing process is a vector-valued, anisotropic diffusion [39] as described in [40,41]. The processing consists of solving a system of nonlinear, partial differential equations with each equation being a variable-conductance diffusion where the conductance is what ensures coupling with other equations.…”
Section: Geometric Diffusion and Watershedsmentioning
confidence: 99%
“…The k j 's are free parameters expressed in units of the root-mean-squared gradients of the terms with which they are associated [40,42]; for this work, we have used k 1 = 2, k 2 = 3, and k 3 = k 4 = k 5 = 10. Equation (7) is solved on the discrete image grid using finiteforward differences as described in the literature [39,40].…”
Section: Geometric Diffusion and Watershedsmentioning
confidence: 99%
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