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Darrell Jackson

Principal Engineer Emeritus; Research Professor Emeritus, Electrical Engineering

Email

drj@apl.washington.edu

Phone

206-543-1359

Biosketch

Darrell Jackson is engaged in theoretical and experimental research in ocean acoustics. This includes random scattering in the ocean, acoustic remote sensing of the ocean bottom, and related signal processing methods.

Department Affiliation

Acoustics

Education

B.S. Electrical Engineering, University of Washington, 1960

M.S. Electrical Engineering, University of Washington, 1963

Ph.D. Electrical Engineering, University of Washington, 1966

Ph.D. Physics, California Institute of Technology, 1977

Publications

2000-present and while at APL-UW

Mid-frequency geoacoustic inversion using bottom loss data from the Shallow Water 2006 Experiment

Yang, J., D.R. Jackson, and D. Tang, "Mid-frequency geoacoustic inversion using bottom loss data from the Shallow Water 2006 Experiment," J. Acoust. Soc. Am., 129, 2426, doi:10.1121/1.3587932, 2011.

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1 Apr 2011

Geoacoustic inversion work has typically been carried out at frequencies below 1 kHz, assuming flat, horizontally stratified bottom models. Despite the relevance to Navy sonar systems, many of which operate at mid-frequencies (1-10 kHz), limited inversion work has been carried out in this frequency band. This paper is an effort to demonstrate the viability of geoacoustic inversion using bottom loss data in the frequency band of 2-5 kHz. The acoustic measurements were taken during the Shallow Water 2006 Experiment off the coast of New Jersey. A half-space bottom model, with three parameters, density, compressional wave speed, and attenuation, was used for geoacoustic inversion by fitting the model to data in the least-squares sense. Inverted sediment sound speed was compared with direct measurements and inversion results using different techniques in the same area. The comparison shows that bottom loss can be used to infer sediment geoacoustic parameters at mid-frequencies. In addition, observations and modeling results demonstrate that forward scattering from topographical changes is important at mid-frequencies and should be taken into account in sound propagation predictions and geoacoustic inversion. To cope with fine-scale topographic variability, measurement technique such as averaging over tracks may be necessary.

Multibeam sonar observations of hydrothermal flows at the Main Endeavour Field

Rona, P.A., K.G. Benis, C.D. Jones, and D.R. Jackson, "Multibeam sonar observations of hydrothermal flows at the Main Endeavour Field," J. Acoust. Soc. Am., 129, 2373, doi:10.1121/1.3587686, 2011.

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1 Apr 2011

The Cabled Observatory Vent Imaging Sonar has been deployed at the Main Endeavour Node of the Canadian Neptune cabled observatory and has acquired data on plume and diffuse hydrothermal flows. Based on the Reson 7125 multibeam sonar and operating at 200 and 400 kHz, two-dimensional and three-dimensional time series are produced using plume backscattering, Doppler shift, and acoustic scintillation. Hydrothermal plumes and diffuse flow are important as agents of transfer of heat, chemicals, and biological material from the mantle and crust into the ocean in quantitatively significant amounts. High-frequency sonar measurements offer the possibility of inversion to obtain fluxes of central importance in these processes. Long-term time series, obtainable in cabled systems, allow observations of hydrothermal response to tidal, tectonic, and volcanic forcing. Examples will be given of plume bending due to currents, determination of entrainment of ambient water, time variation of diffuse flows, and Doppler determination of volume flux.

Simplified formulations for sea-surface scattering for use in modeling equalizer performance in underwater communications

Rouseff, D. and D.R. Jackson, "Simplified formulations for sea-surface scattering for use in modeling equalizer performance in underwater communications," J. Acoust. Soc. Am., 129, 2665, doi:10.1121/1.3588917, 2011.

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1 Apr 2011

Reflection off the rough sea surface typically introduces time spread in an acoustic signal. The details of channel response and hence the time spread will change as the sea surface evolves. Communications signals that are spread by the rough surface may still be recompressed and demodulated successfully by an equalizer providing that the channel response does not change too rapidly. To aid in designing an equalizer, it would be useful to know which acoustic paths should be treated as useful signal and which must be treated as noise because they change too rapidly. Viewed as a rough surface scattering problem, the classic Kirchhoff approximation should be appropriate for modeling reflected communications signals. Textbook descriptions of the Kirchhoff approximation are not promising, however, as they imply that the calculations depend on the details of the surface wave spectrum. In the present work, simplified expressions for the surface reflected communications signals are derived. The simplified results are tested in two ways: Predictions for the mutual coherence function are compared to numerically intense calculations, and predictions for communications performance are compared to experimental results.

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Wave scattering and interaction in elastic sea beds

Ivakin, A.N., and D.R. Jackson, "Wave scattering and interaction in elastic sea beds," J. Acoust. Soc. Am., 129, 2426, doi:10.1121/1.3587935, 2011.

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1 Apr 2011

A first-order perturbation model of scattering in an elastic medium is revisited and discussed. The material properties of the medium are defined by three spatially fluctuating variables, the density and two Lame parameters. The wave interaction process is described in terms of four mechanisms of scattering and energy conversion: two without change of the wave type, from compressional to compressional and from shear to shear, and two with the type conversion, from compressional to shear and vice versa. The model is applied to the case of acoustic scattering from and propagation in underwater sediments of different types, sand and rock. Wave interaction and attenuation due to various mechanisms of scattering in the sediment are considered. An improved method for calculation of the seabed scattering strength is proposed, which takes into account the so-called "windowing" effect. It allows more accurate accounting for the contribution of volume heterogeneities near the sediment surface and its comparison with the first-order roughness mechanism of scattering. The frequency-angular dependencies of the scattering strength for elastic sandy and rocky seafloors are calculated, and behaviors of the volume and roughness contributions are compared.

A geoacoustic bottom interaction model (GABIM)

Jackson, D.R., R.I. Odom, M.L. Boyd, and A.N. Ivakin, "A geoacoustic bottom interaction model (GABIM)," IEEE J. Ocean. Eng., 35, 603-617, 2010.

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29 Jul 2010

The geoacoustic bottom interaction model (GABIM) has been developed for application over the low-frequency and midfrequency range (100 Hz to 10 kHz). It yields values for bottom backscattering strength and bottom loss for stratified seafloors. The model input parameters are first defined, after which the zeroth-order, nonrandom problem is discussed. Standard codes are used to obtain bottom loss, uncorrected for scattering, and as the first step in computation of scattering. The kernel for interface scattering employs a combination of the Kirchhoff approximation, first-order perturbation theory, and an empirical expression for very rough seafloors. The kernel for sediment volume scattering can be chosen as empirical or physical, the latter based on first-order perturbation theory. Examples are provided to illustrate the various scattering kernels and to show the behavior predicted by the full model for layered seafloors. Suggestions are made for improvements and generalizations of the model.

Fine-scale volume heterogeneity in a mixed sand/mud sediment off Fort Walton Beach, FL

Briggs, K.B., A.H. Reed, D.R. Jackson, and D. Tang, "Fine-scale volume heterogeneity in a mixed sand/mud sediment off Fort Walton Beach, FL," IEEE J. Ocean. Eng., 35, 471-487, 2010.

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26 Jul 2010

As part of the effort to characterize the acoustic and physical properties of the seafloor during the high-frequency 2004 Sediment Acoustics Experiment (SAX04), fine-scale variability of sediment sound speed and density was measured in a medium quartz sand using diver cores and an in situ conductivity probe. This study has a goal of providing environmental input to high-frequency backscatter modeling efforts. Because the experiment was conducted immediately following exposure of the site to Hurricane Ivan, measurements revealed storm-generated sedimentary structure that included mud deposits and trapped sand pockets suspended in the mud.

Fluctuations of sediment sound speed and density were measured downcore at 1- and 2-cm increments, respectively, with standard laboratory techniques. Sediment density was also measured on a very fine scale with an in situ conductivity probe [in situ measurement of porosity (IMP2)] and by means of computed tomography (CT) imaging of a diver core. Overlap between the locations of the diver cores and the conductivity probe measurements allowed an examination of multiple scales of sediment heterogeneity and a comparison of techniques. Sediment heterogeneity was characterized using estimates of covariance corresponding to an algebraic form for the power spectrum of fluctuations obtained from core, conductivity, and CT measurements. Correcting for sampling brings the power spectra for density fluctuations determined from the various measurements into agreement, and supports description of heterogeneity at the site over a wide range of scales by a power spectrum having a simple algebraic form.

Dispersion and attenuation due to scattering from heterogeneities of the frame bulk modulus of a poroelastic medium

Hefner, B.T., and D.R. Jackson, "Dispersion and attenuation due to scattering from heterogeneities of the frame bulk modulus of a poroelastic medium," J. Acoust. Soc. Am., 127, 3372-3384, 2010.

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1 Jun 2010

While Biot theory can successfully account for the dispersion observed in sand sediments, the attenuation at high frequencies has been observed to increase more rapidly than Biot theory would predict. In an effort to account for this additional loss, perturbation theory is applied to Biot's poroelastic equations to model the loss due to the scattering of energy from heterogeneities in the sediment. A general theory for propagation loss is developed and applied to a medium with a randomly varying frame bulk modulus. The theory predicts that these heterogeneities produce an overall softening of the medium as well as scattering of energy from the mean fast compressional wave into incoherent fast and slow compressional waves. This theory is applied to two poroelastic media: a weakly consolidated sand sediment and a consolidated sintered glass bead pack. The random variations in the frame modulus do not have significant effects on the propagation through the sand sediment but do play an important role in the propagation through the consolidated medium.

Mid- to high-frequency acoustic penetration and propagation measurements in a sandy sediment

Hefner, B.T., D.R. Jackson, K.L. Williams, and E.I. Thorsos, "Mid- to high-frequency acoustic penetration and propagation measurements in a sandy sediment," IEEE J. Ocean. Eng., 34, 372-387, 2009.

30 Oct 2009

Scattering by sinusoidal pressure-release surfaces

Jackson, D.R., "Scattering by sinusoidal pressure-release surfaces," J. Acoust. Soc. Am., 126, 2166, 2009.

1 Oct 2009

The role of porosity fluctuations in scattering from sand sediments and in propagation losses within the sediment

Hefner, B.T., and D.R. Jackson, "The role of porosity fluctuations in scattering from sand sediments and in propagation losses within the sediment," J. Acoust. Soc. Am., 126, 2168, 2009.

1 Oct 2009

Acoustic observation of the time dependence of the roughness of sandy seafloors

Jackson, D.R., M.D. Richardson, K.L. Williams, A.P. Lyons, C.D. Jones, K.B. Briggs, and D. Tang, "Acoustic observation of the time dependence of the roughness of sandy seafloors," IEEE J. Ocean. Eng., 34, 407-422, 2009.

28 Aug 2009

Acoustic backscattering from a sand and a sand/mud environment: Experiments and data/model comparisons

Williams, K.L., D.R. Jackson, D. Tang, K.B. Briggs, and E.I. Thorsos, "Acoustic backscattering from a sand and a sand/mud environment: Experiments and data/model comparisons," IEEE J. Ocean. Eng., 34, 388-398, 2009.

4 Aug 2009

Measurement and modeling of broadband Bragg scattering from a sinusoidal surface

Tang, D., and D.R. Jackson, "Measurement and modeling of broadband Bragg scattering from a sinusoidal surface," J. Acoust. Soc. Am., 125, 2661, 2009.

1 Apr 2009

Midfrequency backscatter imaging of fish schools in a shallow water waveguide

Jones, C.D., and D.R. Jackson, "Midfrequency backscatter imaging of fish schools in a shallow water waveguide," J. Acoust. Soc. Am., 125, 2550, 2009.

1 Apr 2009

The effects of scattering from heterogeneities in porosity during sound propagation through sand sediments

Hefner, B.T., D.R. Jackson, and J. Calantoni, "The effects of scattering from heterogeneities in porosity during sound propagation through sand sediments," J. Acoust. Soc. Am., 125, 2746, 2009.

1 Apr 2009

Dispersion and attenuation due to scattering from heterogeneities in the frame bulk and shear moduli of sand sediments

Hefner, B.T., D.R. Jackson, and J. Calantoni, "Dispersion and attenuation due to scattering from heterogeneities in the frame bulk and shear moduli of sand sediments," J. Acoust. Soc. Am., 123, 3441, 2008

1 May 2008

Synthetic aperture sonar imaging of simple finite targets near a sediment-water interface

Kargl, St., K.L. Williams, E. Thorsos, D.R. Jackson, and D. Tang, "Synthetic aperture sonar imaging of simple finite targets near a sediment-water interface," J. Acoust. Soc. Am., 123, 3944, 2008.

1 May 2008

High-Frequency Seafloor Acoustics

Jackson, D.R., and M.D. Richardson, "High-Frequency Seafloor Acoustics," New York, Springer, 616 pp., 2007. (See Dr. Jacksons page under PEOPLE to find errata for High-Frequency Seafloor Acoustics.)

30 Jan 2007

Overview of SAX99 and SAX04 measurements of sediment sound speed and attenuation

Thorsos, E.I., K.L. Williams, D.R. Jackson, and D. Tang, "Overview of SAX99 and SAX04 measurements of sediment sound speed and attenuation," J. Acoust. Soc. Am., 117, 2494, 2005.

1 Aug 2005

A method for Doppler acoustic measurement of black smoker flow fields

Jackson, D.R., C.D. Jones, P.A. Rona, and K.G Bemis, "A method for Doppler acoustic measurement of black smoker flow fields," Geochem. Geophys., Geosyst., 4, 10.1029/2003GC000509, 2003.

14 Nov 2003

Acoustic backscattering experiments in a well characterized sand sediment: Data/model comparisons using sediment fluid and Biot models

Williams, K.L., D.R. Jackson, E.I. Thorsos, D. Tang, and K.B. Briggs, "Acoustic backscattering experiments in a well characterized sand sediment: Data/model comparisons using sediment fluid and Biot models," IEEE J. Ocean. Eng., 27, 376-387, DOI: 10.1109/JOE.2002.1040925, 2002.

1 Jul 2002

Comparison of sound speed and attenuation measured in a sandy sediment to predictions based on the Biot theory of porous media

Williams, K.L., D.R. Jackson, E.I. Thorsos, and D. Tang, Schock, S.G., "Comparison of sound speed and attenuation measured in a sandy sediment to predictions based on the Biot theory of porous media," IEEE J. Ocean. Eng., 27, 413-428, DOI: 10.1109/JOE.2002.1040928, 2002.

1 Jul 2002

Fine-scale volume heterogeneity measurements in sand

Tang, D., K.B. Briggs, K.L. Williams, D.R. Jackson, E.I. Thorsos, and D.B. Percival, "Fine-scale volume heterogeneity measurements in sand," IEEE J. Ocean. Eng., 27, 546-560, DOI: 10.1109/JOE.2002.1040937, 2002.

1 Jul 2002

High-frequency subcritical acoustic penetration into a sandy sediment

Jackson, D.R., K.L. Williams, E.I. Thorsos, and S.G. Kargl, "High-frequency subcritical acoustic penetration into a sandy sediment," IEEE J. Ocean. Eng., 27, 346-361, doi:10.1109/JOE.2002.1040923, 2002.

1 Jul 2002

Ocean acoustics, matched-field processing and phase conjugation

Kuperman, W.A., and D.R. Jackson, "Ocean acoustics, matched-field processing and phase conjugation," in Imaging of Complex Media with Acoustic and Seismic Waves, edited by Fink et al., 43-96 (Spinger-Verlag, Berlin, 2002).

15 Jan 2002

Decision-directed passive phase conjugation: Equalisation performance in shallow water

Flynn, J.A., J.A. Ritcey, W.L.J. Fox, D.R. Jackson, and D. Rouseff, "Decision-directed passive phase conjugation: Equalisation performance in shallow water," Electronics Lett., 37(25), 1551-1553, 2001.

6 Dec 2001

Underwater acoustic communication using passive phase conjugation

Rouseff, D., W.L.J. Fox, D.R. Jackson, and C.D. Jones, "Underwater acoustic communication using passive phase conjugation," MTS/IEEE Oceans 2001, 5-8 November, Honolulu, HI, doi:10.1109/OCEANS.2001.968344 (IEEE, 2001).

5 Nov 2001

Decision-directed passive phase conjugation for underwater acoustic communications with results from a shallow-water trial

Flynn, J.A., J.A. Ritcey, W.L.J. Fox, D.R. Jackson, and D. Rouseff, "Decision-directed passive phase conjugation for underwater acoustic communications with results from a shallow-water trial," Conf. Record of the 35th Asilomar Conference on Signals, Systems, and Computers, 4-7 November 2001, edited by M.B. Matthews, 1420-1427, doi:10.1109/ACSSC.2001.987724 (IEEE, 2001).

4 Nov 2001

Passive phase conjugation for underwater communication

Rouseff, D., W.L.J. Fox, and D.R. Jackson, "Passive phase conjugation for underwater communication," J. Acoust. Soc. Am., 110, 2632, 2001.

1 Nov 2001

Underwater acoustic communication by passive phase conjugation: Theory and experimental results

Rouseff, D., D.R. Jackson, W.L.J. Fox, C.D. Jones, J.A. Ritcey, and D.R. Dowling, "Underwater acoustic communication by passive phase conjugation: Theory and experimental results," IEEE J. Ocean. Eng., 26(4), 821-831, 2001.

1 Oct 2001

An overview of SAX99: Acoustic Measurements

Thorsos, E.I., K.L. Williams, N.P. Chotrios, J.T. Christoff, K.W. Commander, C.F. Greenlaw, D.V. Holliday, D.R. Jackson, J.L. Lopes, D.E. McGehee, J.E. Piper, M.D. Richardson, and D. Tang, "An overview of SAX99: Acoustic Measurements," IEEE J. Ocean. Eng., 26, 4-25, 2001.

1 Jan 2001

Acoustic penetration at subcritical grazing angles: Measurements and comparison with simulations based on perturbation theory

Jackson, D.R., K.L. Williams, D. Tang, and E.I. Thorsos, "Acoustic penetration at subcritical grazing angles: Measurements and comparison with simulations based on perturbation theory," J. Acoust. Soc. Am., 108, 2510, doi:10.1121/1.1289207, 2000.

1 Nov 2000

APL-UW environmental measurements during SAX99: Sediment conductivity and tomography

Tang, D., K.L. Williams, D.R. Jackson, and E.I. Thorsos, "APL-UW environmental measurements during SAX99: Sediment conductivity and tomography," J. Acoust. Soc. Am., 108, 2535, 2000.

1 Nov 2000

Applied Physics Laboratory participation in SAX99: Experiment design and execution

Williams, K.L., D.R. Jackson, D. Tang, and E.I. Thorsos, "Applied Physics Laboratory participation in SAX99: Experiment design and execution," J. Acoust. Soc. Am., 108, 2510, 2000.

1 Nov 2000

High-frequency measurements of absorption and dispersion in a a sandy sediment

Jackson, D.R., K.L. Williams, D. Tang, and E.I. Thorsos, "High-frequency measurements of absorption and dispersion in a a sandy sediment," J. Acoust. Soc. Am., 108, 2511, doi:10.1121/1.1289207, 2000.

1 Nov 2000

Sediment acoustic backscattering during SAX99: Measurements and models

Williams, K.L., D.R. Jackson, D. Tang, and E.I. Thorsos, "Sediment acoustic backscattering during SAX99: Measurements and models," J. Acoust. Soc. Am., 108, 2511, 2000.

1 Nov 2000

Underwater acoustic communication by passive phase conjugation: Theory and experiment

Jackson, D.R., D. Rouseff, W.L.J. Fox, C.D. Jones, J.A. Ritcey, and D.R. Dowling, "Underwater acoustic communication by passive phase conjugation: Theory and experiment," J. Acoust. Soc. Am., 108, 2607, doi:10.1121/1.1289207, 2000.

1 Nov 2000

High-Frequency Bistatic Scattering Models for Elastic Seafloors

Jackson, D.R., "High-Frequency Bistatic Scattering Models for Elastic Seafloors," APL-UW TM 2-00, February 2000.

1 Feb 2000

Modeling of subcritical penetration into sediments due to interface roughness

Thorsos, E.I., D.R. Jackson, and K.L. Williams, "Modeling of subcritical penetration into sediments due to interface roughness," J. Acoust. Soc. Am., 107, 263-277, 2000.

1 Jan 2000

Acoustics Air-Sea Interaction & Remote Sensing Center for Environmental & Information Systems Center for Industrial & Medical Ultrasound Electronic & Photonic Systems Ocean Engineering Ocean Physics Polar Science Center