By Bernd Jahne, Horst Hausseker
, Pages xi-xiii, Bernd Jähne, Horst Haußecker
, Pages xv-xxi
1 - Introduction
, Pages 1-8, Bernd Jähne
2 - Radiation and Illumination
, Pages 11-52, Horst Haußecker
3 - Imaging Optics
, Pages 53-84, Peter Geißler
4 - Radiometry of Imaging
, Pages 85-109, Horst Haußecker
5 - Solid-State picture Sensing
, Pages 111-151, Peter Seitz
6 - Geometric Calibration of electronic Imaging Systems
, Pages 153-175, Robert Godding
7 - third-dimensional Imaging Techniques
, Pages 177-208, Rudolf Schwarte, Gerd Häusler, Reinhard W. Malz
8 - illustration of Multidimensional Signals
, Pages 211-272, Bernd Jähne
9 - local Operators
, Pages 273-345, Bernd Jähne
10 - Motion
, Pages 347-395, Horst Haußecker, Hagen Spies
11 - 3-dimensional Imaging Algorithms
, Pages 397-438, Peter Geißler, Tobias Dierig, Hanspeter A. Mallot
12 - layout of Nonlinear Diffusion Filters
, Pages 439-458, Joachim Weickert
13 - Variational tools for Adaptive Smoothing and Segmentation
, Pages 459-482, Christoph Schnörr
14 - Morphological Operators
, Pages 483-515, Pierre Soille
15 - Probabilistic Modeling in laptop Vision
, Pages 517-540, Joachim Hornegger, Dietrich Paulus, Heinrich Niemann
16 - Fuzzy photograph Processing
, Pages 541-576, Horst Haußecker, Hamid R. Tizhoosh
17 - Neural web Computing for photograph Processing
, Pages 577-606, Anke Meyer-Bäse
A - software Gallery
, Pages 609-665
, Pages 667-679
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Extra info for Computer Vision and Applications. A Guide for Students and Practitioners
39) In order to maintain equilibrium, the emitted flux must equal the absorbed flux at each wavelength and in each direction. 3: Basic (idealized) object and surface types Object Properties Opaque e(A) + /5(A) = 1, body AR coating Ideal window Cannot be penetrated by radiation. All exitant radiation is either reflected or emitted. e(A) + f (A) = 1, No radiation is reflected at the surface. All exitant radiation is transmitted or emitted. p(A)=0 All radiation passes without attenuation. e(A) = p(\) = 0, The temperature is not accessible by IR f (A) = 1 thermography because no thermal emission takes place.
Most materials are either opaque or attenuate transmitted radiation to a certain degree. Let z be the direction of propagation along the optical path. Consider the medium being made up from a number of infinitesimal layers of thickness dz (Fig. 17). 17: Depth dependence of the volumetric absorption and emission of radiation. 49) with the extinction coefficient or attenuation coefficient K of the material (in environmental sciences, K is sometimes referred to as turbidity). The unit of K is a reciprocal length, such as m _ 1 .
3 the full complexity of multiple scattering becomes a factor . Examples of multiple scatter media are white clouds. Although each droplet may be considered an independent scatterer, no direct solar radiation can penetrate the cloud. All droplets only diffuse light that has been scattered by other drops. So far only the net attenuation of the transmitted beam due to scattering has been considered. 58) where dV = dS dz defines a volume element with a cross section of dS and an extension of dz along the optical path (Fig.