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Titlebook: Inverse Problems in Wave Propagation; Guy Chavent,Paul Sacks,William W. Symes Conference proceedings 1997 Springer-Verlag New York, Inc. 1

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書目名稱Inverse Problems in Wave Propagation
編輯Guy Chavent,Paul Sacks,William W. Symes
視頻videohttp://file.papertrans.cn/475/474702/474702.mp4
叢書名稱The IMA Volumes in Mathematics and its Applications
圖書封面Titlebook: Inverse Problems in Wave Propagation;  Guy Chavent,Paul Sacks,William W. Symes Conference proceedings 1997 Springer-Verlag New York, Inc. 1
描述Inverse problems in wave propagation concern extraction of information about distant structural features from the measurements of scattered waves. Tasks of this nature arise in geophysics, ocean acoustics, civil and environmental engineering, ultrasonic nondestructive testing, biomedical ultrasonics, radar, astrophysics, and other areas of science and technology. The papers in this volume represent most of these scientific and technical topics, together with fundamental mathematical investigations of the relation between waves and scatterers.
出版日期Conference proceedings 1997
關(guān)鍵詞Eigenvalue; Potential; Radiologieinformationssystem; Vibration; differential equation; hyperbolic equatio
版次1
doihttps://doi.org/10.1007/978-1-4612-1878-4
isbn_softcover978-1-4612-7322-6
isbn_ebook978-1-4612-1878-4Series ISSN 0940-6573 Series E-ISSN 2198-3224
issn_series 0940-6573
copyrightSpringer-Verlag New York, Inc. 1997
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Partitioned Nonlinear Optimization for the Interpretation of Seismograms, optimization allows us to isolate those features of the 1D models that are uniquely determined. These features — integrals over depth along the wavepath—are then used as constraints in a linear inversion for three dimensional (3D) Earth structure. We illustrate the theory with a synthetic example.
地板
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Generalized Modes in an Acoustic Strip,(.) if . > .. We explain how to build generalized eigenfunctions (or modes) of the stationary operator (.(.), .) associated to this wave equation, i.e. solutions . of the equation—?... ?. = λ. which are locally in the domain .(.) and bounded in appropriate weighted spaces.
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On Reconstruction of the Diffusion and of the Principal Coefficient of a Hyperbolic Equation,oblem: find a,b given either for one . (single boundary measurement) or for all (regular) . supported in F × (0,T). Here Γ is a part of ?Ω which can coincide with ?Ω, but in most of geophysical applications it is relatively small part of it. In fact, F is the observation area.
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Results, Old and New, in Computed Tomography,um optics. As a consequence, many aspects of CT have been extensively studied and are now well understood, thus providing an interesting model case for the study of other inverse problems. Other aspects, notably three-dimensional reconstructions, still provide numerous open problems.
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Conference proceedings 1997, radar, astrophysics, and other areas of science and technology. The papers in this volume represent most of these scientific and technical topics, together with fundamental mathematical investigations of the relation between waves and scatterers.
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0940-6573 ltrasonics, radar, astrophysics, and other areas of science and technology. The papers in this volume represent most of these scientific and technical topics, together with fundamental mathematical investigations of the relation between waves and scatterers.978-1-4612-7322-6978-1-4612-1878-4Series ISSN 0940-6573 Series E-ISSN 2198-3224
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