Javascript must be enabled to continue!
Application of the Gelfand–Levitan method to geoacoustic inversion in shallow water
View through CrossRef
The Gelfand–Levitan inverse technique is an exact inversion method originating in quantum scattering theory [I. M. Gelfand and B. M. Levitan, Am. Math. Soc. Transl. 1, 253–304 (1955)]. At a single frequency, the required input data are the Fourier transform of the plane wave reflection coefficient as a function of incident vertical wave number. The method was originally employed in underwater acoustics for a deep-water environment where a simple relationship exists between the reflection coefficient and the depth-dependent Green’s function, which is obtained by Hankel transforming measurements of the point source pressure field [A. A. Merab, Sc.D. thesis, MIT/WHOI Joint Program, Woods Hole, MA (January 1987)]. In shallow water, the Green’s function is characterized by poles corresponding to the eigenvalues of the perfectly trapped modes in the waveguide. These poles complicate the relationship between the Green’s function and the reflection coefficient, and therefore the application of the Gelfand–Levitan technique. However, through application of the Darboux transform to the governing wave equation and the reflection coefficient, the Gelfand–Levitan method can be employed for shallow-water geoacoustic inversion [J. R. McLaughlin and S. Wang, in Mathematical and Numerical Aspects of Wave Propagation, edited by J. A. DeSanto (SIAM, Philadelphia, 1998), pp. 232–236]. In this talk, the Darboux transform will be illustrated and examples of geoacoustic inversion for synthetic shallow-water acoustic data will be presented. [Work supported by ONR.]
Acoustical Society of America (ASA)
Title: Application of the Gelfand–Levitan method to geoacoustic inversion in shallow water
Description:
The Gelfand–Levitan inverse technique is an exact inversion method originating in quantum scattering theory [I.
M.
Gelfand and B.
M.
Levitan, Am.
Math.
Soc.
Transl.
1, 253–304 (1955)].
At a single frequency, the required input data are the Fourier transform of the plane wave reflection coefficient as a function of incident vertical wave number.
The method was originally employed in underwater acoustics for a deep-water environment where a simple relationship exists between the reflection coefficient and the depth-dependent Green’s function, which is obtained by Hankel transforming measurements of the point source pressure field [A.
A.
Merab, Sc.
D.
thesis, MIT/WHOI Joint Program, Woods Hole, MA (January 1987)].
In shallow water, the Green’s function is characterized by poles corresponding to the eigenvalues of the perfectly trapped modes in the waveguide.
These poles complicate the relationship between the Green’s function and the reflection coefficient, and therefore the application of the Gelfand–Levitan technique.
However, through application of the Darboux transform to the governing wave equation and the reflection coefficient, the Gelfand–Levitan method can be employed for shallow-water geoacoustic inversion [J.
R.
McLaughlin and S.
Wang, in Mathematical and Numerical Aspects of Wave Propagation, edited by J.
A.
DeSanto (SIAM, Philadelphia, 1998), pp.
232–236].
In this talk, the Darboux transform will be illustrated and examples of geoacoustic inversion for synthetic shallow-water acoustic data will be presented.
[Work supported by ONR.
].
Related Results
Water, water everywhere but not a drop to drink: The false promise of virtual water
Water, water everywhere but not a drop to drink: The false promise of virtual water
The concept of “virtual water,” which represents the volume of water needed to produce a particular quantity of agricultural commodity, has become popular among international water...
A Novel Approach for Bathymetry Estimation through Bayesian Gravity Inversion
A Novel Approach for Bathymetry Estimation through Bayesian Gravity Inversion
The bathymetry is the most superficial layer of the Earth’s crust on which it is possible to perform direct measurements. However, it is also well known that water covers more than...
eXperimental jOint inveRsioN (XORN) project: first results of a 3D joint gravity and magnetic inversion
eXperimental jOint inveRsioN (XORN) project: first results of a 3D joint gravity and magnetic inversion
<div>
<p><span>The Earth crust represents less than 1% of the volume of our planet but is exceptionally important as it preserves the sign...
Revisiting Kundi Bhandara: Understanding the Ancient Water Management Systems from the Mughal Period - Case of Burhanpur City, Madhya Pradesh
Revisiting Kundi Bhandara: Understanding the Ancient Water Management Systems from the Mughal Period - Case of Burhanpur City, Madhya Pradesh
Since ancient times, managing water has been significant in human civilization. Sophistic water management systems were built in India's Mughal era, which is remembered for its arc...
Two New Methods for Obtaining Water Samples from Shallow Aquifers and Littoral Sediments
Two New Methods for Obtaining Water Samples from Shallow Aquifers and Littoral Sediments
AbstractTwo sampling techniques have been developed which enable ground water samples to be obtained from various depths within shallow aquifers and littoral sediments. Both techni...
Practical Tips for 3D Regional Gravity Inversion
Practical Tips for 3D Regional Gravity Inversion
To solve the inverse gravimetric problem, i.e., to estimate the mass density distribution that generates a certain gravitational field, at local or regional scale, several paramete...
Groundwater Consumption, Quality and Economics in a Higher Education Institution: A Water Sustainability Initiative
Groundwater Consumption, Quality and Economics in a Higher Education Institution: A Water Sustainability Initiative
The demand for groundwater in a Higher Education Institution is very imperative since it’s the only source of water, all were drawn from its deep wells and shallow wells. The land ...
Acoustic studies of submarine gas hydrates on the Cascadia Margin.
Acoustic studies of submarine gas hydrates on the Cascadia Margin.
Submarine gas hydrates were detected over large areas in the Cascadia margin off the west coast of British Columbia by the presence of bottom simulating reflectors in seismic surve...
Recent Results
Low-high-low or high-low-high? Pattern effects on sequential auditory scene analysis
Low-high-low or high-low-high? Pattern effects on sequential auditory scene analysis
Sequential auditory scene analysis (ASA) is often studied using sequences of two alternating tones, such as ABAB or ABA_, with “_” denoting a silent gap, and “A” and “B” sine tones...
The great rebuilding of Amsterdam (1521–1578)
The great rebuilding of Amsterdam (1521–1578)
ABSTRACTIn 1452, approximately three-quarters of Amsterdam was destroyed by fire. Despite attempts by the city government to encourage citizens to build using brick and pan tiles, ...
Late Holocene Paleoclimatic Changes in Western Central Africa Inferred from Mineral Abundance in Dated Sediments from Lake Ossa (Southwest Cameroon)
Late Holocene Paleoclimatic Changes in Western Central Africa Inferred from Mineral Abundance in Dated Sediments from Lake Ossa (Southwest Cameroon)
AbstractMinerals derived from catchment soils were determined using FTIR spectroscopy in the well-dated core OW4 from Lake Ossa, a lowland rainforest area in Cameroon. This quantif...
Chronology of Laurentide glaciation in New Jersey and the New York City area, United States
Chronology of Laurentide glaciation in New Jersey and the New York City area, United States
AbstractDeposits of at least three glaciations are present in New Jersey and the New York City area. The oldest deposits are magnetically reversed. Pollen and stratigraphic relatio...