Contains research objectives and summary of research on four research projects.Joint Services Electronics Program (Contract DAAB07-75-C-1346)Woods Hole Oceanographic Institution Purchase Order 455

Baggeroer, Arthur B.

Gallemore, J. Bruce

Kline, Richard B.

Leverette, Steven J.

Marzetta, Thomas L.

Metzger, Louis S.

Moura, José M. F.

Pusey, Leroy C.

Theriault, Kenneth B.

Zavadil, Steven W.

DSpace@MIT

XIV. DETECTION, ESTIMATION, AND MODULATION THEORYAcademic Research StaffProf. Arthur B. BaggeroerGraduate StudentsJ. Bruce GallemoreRichard B. KlineSteven J. LeveretteThomas MarzettaLouis S. MetzgerKenneth B. TheriaultSteven W. Zavadil1. SPACE/TIME TRACKING OF NARROW-BAND PASSIVE SOURCEJoint Services Electronics Program (Contract DAAB07-75-C-1346)Arthur B. Baggeroer, Louis S. Metzger, Jos6 M. F. MouraPassive tracking systems, with active radar or sonar signals not used, are appli-cable to a variety of fields, such as oceanography, meteorology, passive sonar, andnavigation. This research is directed toward understanding the fundamental limitationson the performance of these systems that exploit the curvature of a wave front acrossan array in conjunction with constraints on the source motion in order to estimate itsposition and velocity.Jos6 M. F. Moura has completed doctoral thesis research in which he examined thesituation of a narrow-band signal with linear constraints on the source motion. 1 HeSASS02totR°Ld C7LU IHwbLd 0- 10CR(I)> 105 \_U<> 10100 10Fig. XIV-1. Total range mean-square error vs X. (XL = array length, R = target range.)o= . 5 L/R o, where0PR No. 117JSEPJSEPJSEPI-4.402.400.40-1 600 .2 .3 .4 .53.60S160-0.40-2400 1 .2 .3 .4 .5f (Hz)(c)Fig. XIV-2.JSEP5.003.001 001.003.701.70-0.30-2.30 0I ~I I I I I I I I II .2 .3 .4 .5(b)SI .... I I. i I i I I I I1 .2 .3 .4 .5f(Hz)(d)Estimated spectra for a first-order process: (a) True extension.(b) Exponential extension (X = . 1). (c) Autoregressive (AR) exten-sion. (d) Damped sinusoid extension (X = . 1, f = . 05).oPR No. 117(XIV. DETECTION, ESTIMATION, AND MODULATION THEORY)identified two important considerations in the analysis of these systems. First, theglobal observability in the absence of noise in these systems is determined by the higherorder phase modulations induced by the array geometry and source motion. Second,for a given signal-to-noise ratio, the local estimation accuracy as specified by Cramer-Rao bounds and the global anomalies as determined by the signal ambiguity need to beexamined. Both are strong functions of the geometry and exhibit individual criticalpoints. Figure XIV-1 illustrates typical behavior.Sources usually radiate signals with some modulation and the transmission mediuminduces its own fluctuations. In any event, the signals are not pure sinusoids. Louis S.Metzger investigated the problems of tracking the bearing and estimating the signal of amoving source with finite bandwidth.2 Using these representatives, he devised repre-sentations for the signals which reflected the space/time structure of the signal andestimator structures.2. DETECTION AND ESTIMATION THEORY METHODSJoint Services Electronics Program (Contract DAAB07-75-C-1346)Arthur B. Baggeroer, Leroy C. Pusey, Thomas Marzetta,Kenneth B. TheriaultA generalization of procedures in spectral analysis and wave propagation by usingoptimal filtering concepts has been described in a doctoral thesis by Leroy C. Pusey. 3He has specified necessary and sufficient conditions for going between an observedcontinuous-time response and a reflection coefficient profile, or equivalently between acovariance function and h(t,O), the impulse response of the optimal filter. This has gen-eralized the concept of covariance extension. Some results are indicated in Fig. XIV-2.-(XIV. DETECTION, ESTIMATION, AND MODULATION THEORY)In related work, Thomas Marzetta is attempting to generalize Pusey' s results totwo-dimensional processes, and Kenneth B. Theriault is formulating the problem ofreflection-coefficient estimation in the presence of noise and finite bandwidth excitation.Their results will be reported in forthcoming theses.3. MULTICHANNEL SEISMIC DATA ACQUISITION AND PROCESSINGWoods Hole Oceanographic Institution Purchase Order 4554Arthur B. Baggeroer, J. Bruce Gallemore, Richard B. Kline,Steven J. Leverette, Kenneth B. TheriaultIn a cruise aboard the R/V Atlantis II on Georges Bank, a six-channel, 1-km, seis-mic array was successfully tested during July and August, 1975. Aside from somenavigation hazards and routine failures of electronic components, we encountered noproblems in the array deployment and the data acquisition. Onboard processing,including deconvolution, and velocity analysis with common shot-point stacking wereimplemented. The throughput rate, however, continues to be a difficulty because of theextensive interpretation that is needed in the velocity analysis of the seismic modeling.Figure XIV-3 is a section of a processed multichannel record indicating reflectionsobserved in up to 3. 8 seconds of two-way travel time.2.0-Uj3.0400500 053090d o6oo0600 030 0700 0o30 0800 08'30TIME12O06 1400SHOT POINT09001600Fig. XIV-3. Seismic profile on Georges Bank.Velocity analysis is an important step in seismic data processing in which we attemptto devise a model of the seismic section which is parametrized by the travel time to areflector and the velocity to it. We attempt to estimate these parameters by the timedelays observed across a multichannel array. Experiments involving the application ofhigh-resolution spectral analysis procedures, e.g., the maximum-likelihood method,have been conducted this year. Figure XIV-4a illustrates the results of applying theseprocedures to synthetic seismograms, while Fig. XIV-4b indicates results using realPR No. 117JSEPJSEP~I ~ C - C~- ~L I- --1 r I I I I Irll I I r I r -I -DETECTION, ESTIMATION, AND MODULATION THEORY)1.0 1.4 1.8TWO-WAY TRAVEL TIME (s)(a).4 .6 .8 1.0 1.2 1.4 1.6 1.8 2.0TWO-WAY TRAVEL TIME (s)Fig. XIV-4. Maximum-likelihood method velocity spectra estimates.(a) Georges Bank data (16 Hz).(b) Synthetic multichannel data (broadband 16-36 Hz).data from reflections observed in Georges Bank. These results were presented at the1975 Society of Exploration Geophysicists Conference.4 Steven J. Leverette is pursuingthis topic in his thesis research.In other work on seismic data processing, J. Bruce Gallemore is comparing theperformance of tapped delay-line and homomorphic filters for removing deep watermultiples.5, 6 Richard B. Kline is analyzing the theoretical resolution capabilities of aseismic array for velocity analysis.PR No. 117-- I --= __ -- -- --(XIV.(XIV. DETECTION, ESTIMATION, AND MODULATION THEORY)4. DESIGN OF A SEISMIC SIGNAL SOURCE USING PARAMETRICSONARArthur B. Baggeroer, Steven W. ZavadilSeismic source signals are typically nonideal impulses. Moreover, they cannot beeffectively modulated in order to take advantage of available signal-processing tech-niques. In a design project for the Department of Ocean Engineering, Steven W. Zavadilis using parametric sonar techniques to design a modulated seismic source. The para-metric models have been designed in conjunction with the U. S. Navy Underwater Sys-tems Center.References1. J. M. F. Moura, "Passive Systems Theory with Applications to Positioning andNavigation," Ph.D. Thesis, Department of Electrical Engineering and ComputerScience, M. I. T. , April 15, 1975; to be published as Technical Report 490 in theResearch Laboratory of Electronics series.2. L. S. Metzger, "Nonlinear Estimation of Target Bearing and Signal," Ph.D. Thesis,Department of Electrical Engineering and Computer Science, M. I. T., October 1,1975.3. L. C. Pusey, "An Innovation Approach to Spectral Estimation and Wave Propagation,"Ph.D. Thesis, Department of Electrical Engineering and Computer Science, M. I. T.,May 2, 1975.4. A. B. Baggeroer and S. J. Leverette, "Estimation of Velocity/Depth Spectra Usingthe Maximum-Likelihood Method," Society of Exploration Geophysicists 45th AnnualMeeting, Denver, Colorado, October 12-16, 1975.5. A. B. Baggeroer, " Trapped Delay Line Models for the Dereverberation of DeepWater Multiples," IEEE Trans. , Vol. GE-12, No. 2, pp. 33-54, April 1974.6. P. Buhl, P. Stoffa, and G. Bryan, "The Application of Homomorphic Deconvolutionto Shallow Water Marine Seismology - Models," Geophys. 39, 401-416 (1974); "TheApplication of Homomorphic Deconvolution to Shallow Water Marine Seismology -Real Data," Geophys. 39, 416-426 (1974).PR No. 117

Detection, Estimation, and Modulation Theory

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Detection, Estimation, and Modulation Theory

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