Thesis. 1977. Elec.E.--Massachusetts Institute of Technology. Dept. of Electrical Engineering and Computer Science. / MICROFICHE COPY AVAILABLE IN ARCHIVES AND ENGINEERING. / Includes bibliographical references. / Elec.E.

Thesis. 1975. Ph.D.--Massachusetts Institute of Technology. Dept. of Electrical Engineering and Computer Science. / Vita. / Includes bibliographical references. / Ph.D.

O método da análise multicanal de ondas superficiais foi empregado em um estudo de caso no sítio controlado do Instituto de Astronomia, Geofísica e Ciências Atmosféricas da Universidade de São Paulo - IAG-USP, localizado no campus Butantã, São Paulo, em terrenos da bacia sedimentar de São Paulo. O estudo visou à investigação geológica rasa, ou seja, ao mapeamento dos estratos sedimentares presentes e do contato sedimentos-embasamento. Além disso, procurou-se, através de testes de diversos parâmetros de aquisição, chegar-se a uma rotina para a aquisição e tratamento dos dados provenientes de fontes ativas (marreta e queda de peso) e passivas (tráfego de veículos) que possa ser indicada para ensaios em outras áreas da cidade de São Paulo que apresentem condições semelhantes às da área estudada. Na aquisição com fontes ativas foram registrados dados com diversos offsets mínimos e na passiva foi aplicada a técnica Passive Roadside com o arranjo de geofones disposto próximo e paralelamente à via de tráfego. Foram realizadas as etapas de pré-processamento dos dados, geração das imagens de dispersão, extração das curvas de dispersão e inversão. A combinação de imagens geradas a partir de dados adquiridos com diferentes fontes resultou numa imagem com melhor razão sinal-ruído, e consequentemente na produção de melhores curvas que foram invertidas para a geração dos perfis 1D das velocidades da onda S. De modo geral, os perfis de velocidades obtidos a partir dos dados obtidos com o emprego de uma marreta para geração da onda mapearam as interfaces geológicas mais superficiais, já os perfis resultantes dos dados adquiridos com o uso de uma fonte tipo queda de peso alcançaram profundidades maiores, por vezes amostrando o embasamento. No caso das fontes passivas, as principais interfaces de contato foram imageadas, conseguindo-se com sucesso o mapeamento do embasamento, que na área está a mais de 50 metros de profundidade. Correlações com o perfil litológico e de dados de ensaios SPT de um furo de sondagem localizado no centro do arranjo revelaram que as diferenças na determinação da profundidade das interfaces foram menores do que 10%. Desta forma, o método mostrou ser uma ferramenta prática e eficiente nas aplicações geotécnicas, principalmente em ix áreas urbanas onde o ruído é elevado, o que muitas vezes inviabiliza o uso da investigação sísmica convencional (refração ou reflexão). / The multichannel analysis of surface waves (MASW) method was employed in a case study on the controlled site in the Institute of Astronomy, Geophysics and Atmospheric Sciences (IAG), University of São Paulo (USP), located on the campus Butantã, São Paulo, in the grounds of the sedimentary basin São Paulo. The study aimed to shallow geological investigation, in other words, mapping of sedimentary strata present and the sediment-basement contact. In addition, It is sought to, by testing with different acquisition parameters, to get a routine for the acquisition and processing of data from active sources (sledgehammer and drop weight) and passive (vehicle traffic) that can be suitable for testing in other areas of the city of São Paulo who have similar conditions of the study area. In the acquisition with active sources were registered data with many different offsets and passive acquisition has been applied to the Passive Roadside MASW technique with the conventional linear receiver array disposed near and parallel to the traffic lane. Were performed, pre-processing of the data, generation of images of dispersion, extraction of dispersion curves and inversion. The combination of images generated based on data acquired from various sources resulted in image with improved signal to noise ratio and consequently in the production of finest curves that have been inverted to generate the 1D shear-wave velocities profiles. In general, the velocity profiles obtained from the data were acquired with the use of a sledgehammer to the wave generation mapped shallowest geological interfaces, but the resulting profiles of the acquired data using a font type \"drop weight\" reached greater depths, sometimes sampling the basement. In the case of passive sources, the main contact interfaces were imaged, achieving successful mapping of the basement, which in this area is over 50 meters deep. Correlations with the lithological profile and SPT data from a borehole located in the center of the array revealed that the differences in the depth determination of the interfaces was less than 10%. Thus, the method showed to be an efficient and practical tool in geotechnical applications, especially in urban areas where the noise is high, which often prevents the use of conventional seismic survey (reflection or refraction).

This study presents two new seismic testing methods for engineering application, a new shallow seismic reflection method and Time Filtered Analysis of Surface Waves (TFASW). Both methods are described in this dissertation. The new shallow seismic reflection was developed to measure reflection at a single point using two to four receivers, assuming homogeneous, horizontal layering. It uses one or more shakers driven by a swept sine function as a source, and the cross-correlation technique to identify wave arrivals. The phase difference between the source forcing function and the ground motion due to the dynamic response of the shaker-ground interface was corrected by using a reference geophone. Attenuated high frequency energy was also recovered using the whitening in frequency domain. The new shallow seismic reflection testing was performed at the crest of Porcupine Dam in Paradise, Utah. The testing used two horizontal Vibroseis sources and four receivers for spacings between 6 and 300 ft. Unfortunately, the results showed no clear evidence of the reflectors despite correction of the magnitude and phase of the signals. However, an improvement in the shape of the cross-correlations was noticed after the corrections. The results showed distinct primary lobes in the corrected cross-correlated signals up to 150 ft offset. More consistent maximum peaks were observed in the corrected waveforms. TFASW is a new surface (Rayleigh) wave method to determine the shear wave velocity profile at a site. It is a time domain method as opposed to the Spectral Analysis of Surface Waves (SASW) method, which is a frequency domain method. This method uses digital filtering to optimize bandwidth used to determine the dispersion curve. Results from testings at three different sites in Utah indicated good agreement with the dispersion curves measured using both TFASW and SASW methods. The advantage of TFASW method is that the dispersion curves had less scatter at long wavelengths as a result from wider bandwidth used in those tests.

Ocean-continent convergence and subsequent continental collision are responsible for continental growth, mountain building, and severe tectonic events including volcanic eruptions and earthquake activity. They are also key driving forces behind the extensive thermal and compositional heterogeneities at crustal and mantle depths. Active subduction along the Calabrian Arc in southern Italy and the Hellenic Arc are examples of such collisional tectonics. The first part of this thesis examines the subduction related deformations within the crust beneath the southern Apennines. By modeling regional surface wave recordings of the largest temporary deployment in the southern Apennines, a lower-crustal/upper-mantle low-velocity volume extending down to 50 km beneath the mountain chain is identified. The magnitude (~ 0.4 km/s slower) and anisotropic nature (~ 10%) of the anomaly suggest the presence of hot and partially molten emplacement that may extend into the upper-crust towards Mt. Vulture, a once active volcano. Since the Apulian basement units are deformed during the compressional and consequent extensional events, our observations favor the ``thick-skin'' tectonic growth model for the region. In the deeper mantle, active processes are thermodynamically imprinted on the depth and strength of the phase transitions. This thesis examines more than 15000 SS precursors and provides the present-day reflectivity structure and topography associated with these phase transitions. Through case studies I present ample evidence for both slab penetration into the lower mantle (beneath the Hellenic Arc, Kurile Island and South America) and slab stagnation at the bottom of the Mantle Transition Zone (beneath the Tyrrhenian Sea and eastern China). Key findings include (1) thermal anomalies (~ 200 K) at the base of the MTZ, which represent the deep source for Cenozoic European Rift Zone, Mount Etna and Mount Cameroon volcanism, (2) significant depressions (by 20-40 km) at the bottom of the Mantle Transition Zone beneath subducting slabs, (3) a strong 520-km reflector near subducting slabs, (4) a weak and elevated (15-25 km) 410-km reflector within active deformation zones, (5) strong lower mantle reflectors (~ 900 km) while slabs penetrate into the lower mantle, and (6) consistency between the topography of a 300-km reflector and an exothermic phase transformation. / Geophysics

It is well known that direct surface waves of large earthquakes are capable of triggering shallow earthquakes and deep tremor at long-range distances. Recent studies have shown that multiple surface waves circling the earth could also remotely trigger microearthquakes. However, it is still not clear whether multiple surface waves returning back to the main shock epicenters could also trigger/modulate aftershock behavior. Here we conduct a study to search for evidence of such triggering by systematically examining aftershock patterns of earthquakes with magnitude ≥ 8 since 1990 that produce observable surface waves circling the globe repeatedly. We specifically examine the 2011 M9 Tohoku-Oki event using a composite catalog of JMA, HiNet and newly detected events obtained by waveform cross correlation. We compute the magnitude of completeness for each sequence, and stack all the sequences together to compute the seismicity and moment rates by sliding data windows. The sequences are also shuffled randomly and these rates are compared to the actual data as well as synthetic aftershock sequences to estimate the statistical significance of the results. Our results suggest that there is some moderate increase of early aftershock activity after a few hours when the surface waves return to the epicentral region. However, we could not completely rule out the possibility that such an increase is purely due to random fluctuations of aftershocks or caused by missing aftershocks in the first few hours after the mainshock.

Mechanical waves provide information about the stiffness and the condition of a medium; thus, changes in medium conditions can be inferred from changes in wave velocity and attenuation. Non-destructive testing (NDT) methods based on ultrasonic waves are often more economical, practical and faster than destructive testing. Multichannel analysis of surface waves (MASW) is a well-established surface wave method used for determination of the shear-wave profile of layered medium. The MASW test configuration is also applicable to assess the condition of concrete elements using appropriate frequency range. Both attenuation and dispersion of ultrasonic waves can be evaluated by this technique. In ultrasonic testing, the characterization of a medium requires the precise measurement of its response to ultrasonic pulses to infer the presence of defects and boundary conditions. However, any ultrasonic transducer attached to a surface affects the measured response; especially at high frequencies. On the other hand, ultrasonic transducers available for engineering application are mostly used to measure wave velocities (travel time method). Therefore, these transducers do not have a flat response in the required frequency range. Moreover, in the case of full-waveform methods, the recorded signals should be normalized with respect to the transfer functions of the transducers to obtain the real response of the tested specimen. The main objective of this research is to establish a comprehensive methodology based on surface wave characteristics (velocity, attenuation and dispersion) for condition assessment of cemented materials with irregular defects. To achieve the major objective, the MASW test configuration is implemented in the ultrasonic frequency range. The measured signals are subjected to various signal processing techniques to extract accurate information. In addition, a calibration procedure is conducted to determine the frequency response functions (FRF) of the piezoelectric accelerometers outside their nominal frequency range. This calibration is performed using a high-frequency laser vibrometer. This research includes three main studies. The first study introduces the calibration approach to measure the FRFs of the accelerometers outside of their flat frequency range. The calibrated accelerometers are then used to perform MASW tests on a cemented-sand medium. The original signals and the corrected ones by eliminating the effect of the FRFs are used to determine material damping of the medium. Although, the damping ratios obtained from different accelerometers are not same, the values from the corrected signals are found closer to the characteristic damping value compared to those from the uncorrected signals. The second study investigates the sensitivity of Rayleigh wave velocity, attenuation coefficient, material damping and dispersion in phase velocity to evaluate the sensitivity of these characteristics to the damage quantity in a medium. The soft cemented-sand medium is preferred as the test specimen so that well-defined shaped defects could be created in the medium. MASW test configuration is implemented on the medium for different cases of defect depth. The recorded signals are processed using different signal processing techniques including Fourier and wavelet transforms and empirical mode decomposition to determine the surface wave characteristics accurately. A new index, ‘dispersion index’, is introduced which quantifies the defect based on the dispersive behaviour. All surface wave characteristics are found capable of reflecting the damage quantity of the test medium at different sensitivity levels. In the final study, the condition assessment of six lab-scale concrete beams with different void percent is performed. The beam specimens involving Styrofoam pellets with different ratios are tested under ultrasonic and mechanical equipment. The assessment produce established in the second study with well-defined defects is pursed for the beams with irregular defects. Among the characteristics, attenuation, P and R-wave velocities and dispersion index are found as the promising characteristics for quantifying the defect volume.

Electromagnetic wave scattering from a semi-infinite array of dipoles in free space is described by using asymptotic high frequency methods. An electric field integral expression is obtained and solved with asymptotic high frequency methods. An asymptotic field expression is obtained for a finite &times / infinite array of dipoles in free space. The analytical closed form expression for the array guided surface wave launching coefficient is obtained via a combination of an asymptotic high frequency analysis of a related reciprocal problem and Lorentz reciprocity integral formulation for the semi-infinite planar dipole array in which modified Kirchhoff approximation is used. The accuracy and the validity of the asymptotic analytical solutions are compared with the numerical solutions available in the literature before.

Near-field thermal radiation which can exceed blackbody radiation by several orders of magnitude has potential applications in energy conversion devices, nanofabrication, and near-field imaging. The present dissertation provides a comprehensive and thorough investigation of near-field heat transfer between parallel plates at nanometer distances. The first part of this dissertation focuses on the fundamentals of nanoscale thermal radiation through a systematic study on the near-field heat transfer between doped Si plates. In order to calculate the near-field heat transfer, it is important to accurately predict the dielectric function of doped Si. The dielectric function of doped Si which is described by the Drude model is a function of carrier concentration and mobility. Hence, accurate ionization and carrier mobility models for both p- and n-type Si are identified after a careful review of the available literature. The radiative properties calculated using the improved dielectric function agrees to a good extent with measurements performed using a FTIR. The near-field heat transfer between doped Si plates at varying doping levels is then calculated using the improved dielectric functions. Several important and characteristic features of near-field radiation are revealed in the analysis. An interesting issue regarding the maximum achievable nanoscale thermal radiation arises out of the study on near-field heat transfer in doped Si. The second part of this dissertation investigates the maximum achievable near-field thermal radiation between two plates at finite vacuum gaps. Initially, both the emitter and the receiver are assumed to have identical frequency-independent dielectric functions and a cut off in the order of the lattice spacing is set on the upper limit of the wavevector. The energy transfer is maximum when the real part of dielectric function is around -1 due to surface waves. On the other hand, there is a strong relationship between the imaginary part of the dielectric function and the vacuum gap. While the study using frequency independent dielectric function is not realistic, it lays down the guidelines for the parametric optimization of dielectric functions of real materials for achieving maximum near-field heat transfer. A parametric study of the different adjustable parameters in the Drude and Loretz model is performed in order to analyze their effect on the near-field heat transfer. It is seen that the optimized Drude model always results in greater near-field heat transfer compared to the Lorentz model and the maximum achievable near-field heat transfer is nearly 1 order greater than that between real materials. In the third part of this dissertation, the unusual penetration depth and the energy streamlines in near-field thermal radiation are studied. It is seen that unlike far-field radiation, the penetration depth in near-field heat transfer is dependent on the vacuum gap. This unusual feature results in a 10 nm thick SiC film behaving as completely opaque when the vacuum gap is around 10 nm. The energy streamlines inside the emitter, receiver, and the vacuum gap are calculated using fluctuation electrodynamics and errors generated due to thin film optics are pointed out. It is seen that the lateral shift of the streamlines inside the emitter can be greater than that in the vacuum gap for SiC. However, for doped Si, the lateral shift is comparable in the different media. While the study on the penetration depth determines the thickness of the emitter, the streamlines determine the lateral dimension.

A36 steel is a commonly used material in civil engineering structures where fatigue damage can lead to catastrophic failure. In this research, nonlinear Rayleigh surface waves are used to characterize damage in A36 steel specimens caused by monotonic tension and low cycle fatigue. Fatigue damage produces the increased acoustic nonlinearity that leads to the generation of measurable higher harmonics in an initially monochromatic Rayleigh wave signal. One specimen is subjected to static tension and four specimens are used for low cycle fatigue tests in the tension-tension mode with a constant stress amplitude. The fatigue tests are interrupted at different numbers of cycles for the nonlinear ultrasonic measurements. Tone burst Rayleigh wave signals are generated and detected using a pair of oil coupled wedge transducers. The amplitudes of the first and second harmonic are measured at varying propagation distances to obtain the nonlinearity parameter for a given damage state. The experimental results show an increase of acoustic nonlinearity in the early stages of fatigue life. Furthermore, a close relationship between plastic deformation and the acoustic nonlinearity is found, which indicates that the acoustic nonlinearity is indeed a measure of microplasticity in this material.