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Organisationseinheit der BAM
The Alpine Fault zone in New Zealand marks a major transpressional plate boundary that is late in its typical earthquake cycle. Understanding the subsurface structures is crucial to understand the tectonic processes taking place. A unique seismic survey including 2D lines, a 3D array, and borehole recordings, has been performed in the Whataroa Valley and provides new insights into the Alpine Fault zone down to ∼2 km depth at the location of the Deep Fault Drilling Project (DFDP)-2 drill site. Seismic images are obtained by focusing prestack depth migration approaches. Despite the challenging conditions for seismic imaging within a sediment filled glacial valley and steeply dipping valley flanks, several structures related to the valley itself as well as the tectonic fault system are imaged. A set of several reflectors dipping 40°–56° to the southeast are identified in a ∼600 m wide zone that is interpreted to be the minimum extent of the damage zone. Different approaches image one distinct reflector dipping at ∼40°, which is interpreted to be the main Alpine Fault reflector located only ∼100 m beneath the maximum drilled depth of the DFDP-2B borehole. At shallower depths (z < 0.5 km), additional reflectors are identified as fault segments with generally steeper dips up to 56°. Additionally, a glacially over-deepened trough with nearly horizontally layered sediments and a major fault (z < 0.5 km) are identified 0.5–1 km south of the DFDP-2B borehole. Thus, a complex structural environment is seismically imaged and shows the complexity of the Alpine Fault at Whataroa.
The ultrasonic echo technique is a frequently used method in non destructive testing for geometry Determination of concrete building elements. Important tasks are thickness measurements as well as the localization and characterization of built-in components and inhomogeneities.
Currently mainly the synthetic aperture focusing family of techniques (SAFT) is used for imaging. These algorithms have difficulties in imaging steeply dipping interfaces and complicated structures such as steps and lower boundaries of voids. As an alternative two geophysical migration methods, pre-stack Kirchhoff depth migration and pre-stack Reversetimemigration (RTM)were tested in this paper at a reinforced concrete foundation slab. The slab consists of various reinforcement contents, different thicknesses and two pile heads.
In a first step, both methods were evaluated with synthetic 2D data. In the second step, ultrasonic measurement data recorded with shear wave transducers on a line profile on the foundation slab were processed. The use of an automatic scanner simplified the measurements. A comparison of the geophysical migration results with those of SAFT shows, in particular for RTM, a significant improvement in the Imaging of the geometry of the foundation slab. Vertical borders were reconstructed and the location and structure of the lower boundary of the foundation slab were reproduced better. Limitations still exist in imaging the piles below the slab.
Das Ultraschall-Echo-Verfahren ist ein klassisches Verfahren in der zerstörungsfreien Prüfung zur Bestimmung der Geometrie von Bauteilen. Die Prüfaufgaben beinhalten unter anderem die korrekte Dickenbestimmung der Baukörper sowie die Lokalisierung von Einbauteilen und Fehlstellen. Stand der Technik bei den Abbildungsverfahren ist die SAFT–Rekonstruktion (Synthetic Aperture Focusing Technique). Diese Verfahrensfamilie hat Schwierigkeiten bei der Darstellung von steilen Grenzflächen und komplizierten Strukturen, wie beispielsweise Stufen oder Unterkanten von Hohlräumen und Hüllrohren. Als Alternative werden seit einiger Zeit geophysikalische Migrationsmethoden evaluiert. Am Beispiel eines Stahlbetonfundamentes mit verschiedenen Bewehrungsgehalten, unterschiedlichen Dicken sowie zwei Pfahlköpfen wurden die Kirchhoff-Migration und die Reverse-Time Migration (RTM) getestet. Die strahlenbasierte Kirchhoff-Migration arbeitet ähnlich wie die SAFT-Rekonstruktion. Die RTM basiert auf der vollständigen Wellengleichung.
In einem ersten Schritt wurden die Methoden an einem synthetischen, auf der akustischen Wellengleichung basierenden zweidimensionalem Modell getestet. Im zweiten Schritt wurden reale Messdaten, die mit Scherwellenprüfköpfen an der Fundamentplatte aufgenommen wurden, bearbeitet. Der Einsatz eines Scannersystems vereinfachte die Messungen. Die Experimente, die in diesem Manuskript vorgestellt werden, sind von bedeutendem Interesse für die Evaluierung geophysikalischer Migrationsmethoden an analogen Modellen.
Ein Vergleich der Migrationsergebnisse mit den bisherigen SAFT-Ergebnissen zeigt insbesondere für die RTM eine deutliche Verbesserung in der Abbildung der Bauteilgeometrie. Vertikale Kanten konnten dargestellt sowie die Lage und Struktur der Rückwände exakter reproduziert werden. Grenzen bestehen noch bei der Darstellung der Pfahlköpfe, da die von dem zylinderförmigen Pfahl kommenden Signale verrauscht sind. Ursachen dafür sind u.a. die Bewehrung, Randeffekte sowie Mehrfachreflexionen an dem Pfahlschaft.
The ultrasonic echo technique is frequently used in non-destructive testing (NDT) of concrete structures for thickness measurements, geometry determinations as well as localization of built-in components. To improve ultrasonic imaging of complex structures in concrete, we transferred a geophysical imaging technique, the reverse time migration (RTM), to NDT in civil engineering. In contrast to the conventionally used synthetic aperture focusing technique (SAFT) algorithms, RTM is a wavefield continuation method in time and uses the full wave equation. Thus, RTM can handle complicated wave propagations in any direction without dip limitation. In this paper, we focused on the application and evaluation of a two-dimensional (2D) elastic RTM algorithm considering compressional waves, vertically polarized shear waves, and Rayleigh waves. We tested the elastic RTM routine on synthetic ultrasonic echo data generated with a 2D concrete model consisting of several steps and circular air inclusions. As these complex structures can often be found in real-world NDT use cases, their imaging is especially important. By using elastic RTM, we were able to clearly reproduce vertical reflectors and lower edges of circular air voids inside our numerical concrete model. Such structures cannot be imaged with conventional SAFT algorithms. Furthermore, the used elastic RTM approach also yielded a better reconstruction of a horizontal reflector and upper boundaries of circular air inclusions. Our encouraging results demonstrate that elastic RTM has the potential to significantly improve the imaging of complex concrete structures and, thus, is a step forward for detailed, high-quality ultrasonic NDT in civil engineering.
In the framework of non-destructive-testing advanced seismic imaging techniques have been applied to ultrasonic echo data in order to examine the integrity of an engineered test-barrier designed to be used for sealing an underground nuclear waste disposal site. Synthetic data as well as real multi-receiver ultrasonic data acquired at the test site were processed and imaged using Kirchhoff prestack depth migration reverse time migration (RTM). In general, both methods provide a good Image quality as demonstrated by various case studies, however deeper parts within the test barrier containing inclined reflectors were reconstructed more accurately by RTM. In particular, the image quality of a specific target reflector at a depth of 8 m in the test-barrier has been significantly improved compared to previous investigations using synthetic aperture Focusing technique, which justifies the considerable computing time of this method.