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استفاده از الگوریتم POCS برای بازسازی داده‌های لرزه‌ای سه‌مؤلفه‌ای در حوزه فوریه کواترنیون | ||
| فیزیک زمین و فضا | ||
| مقاله 2، دوره 45، شماره 2، مرداد 1398، صفحه 269-281 اصل مقاله (1.12 M) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/jesphys.2019.257996.1007006 | ||
| نویسندگان | ||
| امین افتخاری1؛ حمیدرضا سیاهکوهی* 2 | ||
| 1دانش‌آموخته کارشناسی ارشد، گروه ژئوفیزیک، واحد علوم و تحقیقات، دانشگاه آزاد اسلامی، تهران، ایران | ||
| 2استاد، گروه فیزیک زمین، مؤسسه ژئوفیزیک، دانشگاه تهران، تهران، ایران | ||
| چکیده | ||
| لرزه‌نگاری سه‌مؤلفه‌ای از امواج لرزه‌ای در هر ایستگاه در سه راستا نمونه‌برداری کرده و اطلاعات امواج P و S را به‌صورت همزمان برداشت می‌کند. در برخی کاربردها استفاده از اطلاعات موج S به همراه اطلاعات موج P برآورد درستی از خصوصیات مخزن به‌دست می‌دهد. چون در برداشت‌های لرزه‌ای گاهی به‌علت شرایط منطقه یا خرابی دستگاه‌ها، نمونه‌برداری مکانی یکنواخت از امواج لرزه‌ای میسر نیست، باید از روش‌های درون‌یابی استفاده کرد تا ردلرزه‌های برداشت نشده بازسازی شوند. روش‌های مرسوم بازسازی ردلرزه‌های گم‌شده در لرزه‌نگاری سه‌مؤلفه‌ای، معمولاً با اجرای روش روی هر مؤلفه به‌طور جداگانه انجام می‌شود، که می‌تواند به ویژگی‌های ظریف در رکورد صدمه بزند. در این تحقیق روشی برای بازسازی همزمان هرسه مؤلفه به یک‌باره ارائه می‌شود (برگرفته از ایده استنتون و ساشی) که با استفاده از تبدیل فوریه کواترنیون و الگوریتم تصویر بر روی مجموعه‌های محدب (QPOCS)، انجام می‌شود. نمایش برداری داده مختلط در حوزه فرکانس می‌تواند به‌وسیله قراردادن بخش‌های حقیقی و موهومی هر مؤلفه در آرگومان‌های یک کواترنیون، به‌دست آید. این روش اجازه می‌دهد تا عملگرها بر روی هر دو مؤلفه به‌طور همزمان اعمال شوند. مزیت این روش به‌خاطر همپوشانی طیفی مؤلفه‌ها در حوزه فرکانس-عددموج می‌باشد. نتیجه حاصل از کاربرد این روش بر داده‌های سه‌مؤلفه‌ای مصنوعی و واقعی، با نتیجه حاصل از کاربرد الگوریتم POCS بر روی هر مؤلفه به‌تنهایی، مقایسه شده که نتایج بازسازی با استفاده از الگوریتم QPOCS دارای کیفیت بازسازی بهتری می‌باشند. | ||
| کلیدواژه‌ها | ||
| درون‌یابی سه‌بعدی؛ لرزه‌نگاری سه‌مؤلفه‌ای؛ تبدیل فوریه؛ کواترنیون؛ مجموعه محدب | ||
| عنوان مقاله [English] | ||
| Application of POCS algorithm for the reconstruction of three-component seismic data in quaternion Fourier domain | ||
| نویسندگان [English] | ||
| Amin Eftekhari1؛ Hamid Reza Siahkoohi2 | ||
| 1M.Sc. Graduated, Department of Geophysics, Research and Science Branch, Islamic Azad University, Tehran, Iran | ||
| 2Professor, Department of Earth Physics, Institute of Geophysics, University of Tehran, Tehran, Iran | ||
| چکیده [English] | ||
| Three-component (3C) seismic data acquisition method samples seismic wave field at each station along three Cartesian coordinates, simultaneously. Many reservoirs have been discovered and determined by the generation and recording of P waves only, but the P wave alone cannot provide a comprehensive description of the reservoir characteristics. In some studies, S-wave information is required in addition to P-wave information to get a correct estimation from reservoir properties. By the three component seismic acquisition, P and S waves’ information can be recorded simultaneously. More often in seismic surveys, one cannot sample seismic wave field uniformly the along spatial direction due to environment limitations or instrument malfunctions; inevitably we have to use interpolation methods for reconstruction of missing traces. Reconstruction of missing or noisy traces is done using the projection onto convex sets (POCS). The POCS algorithm is a simple algorithm which is suitable for reconstruction of irregularly lost traces in a regular grid using multiple repetitive Fourier transforms. Conventional methods for reconstruction of missing traces in three component acquisition is usually done by implementation of POCS on each component separately, which could damage any subtle features in the record. This research introduces a method to reconstruct all three components at once using the quaternion Fourier transform and Projection onto Convex Sets (QPOCS).Quaternions in mathematics are a commutative numbers system that extend the complex numbers system. As the ordinary complex numbers can be displayed on two dimensions, these numbers can also be displayed on four dimensions. Quaternions were first introduced by William Rowan Hamilton when looking for a way to extend complex numbers to three dimensions. He knew how to sum and multiply three-dimensional numbers, but he was looking for a way to divide these numbers into each other. In 1843, Hamilton discovered that the division of quaternions requires a fourth dimension. Quaternion Algebra is often shown with H (in honor of Hamilton). The two-component data vector representation in the frequency domain can be obtained by putting the real and imaginary parts of each component in the arguments of a quaternion. This method allows operators to apply both components simultaneously. Quaternions are converted to Frequency-wavenumber domain by Quaternion Fourier Transform (QFT) and a single domain spectrum for both components is defined using the polar representation of the Quaternions. Quaternions have other applications in seismic data processing such as computing spectral attributes, multi-component velocity analysis and multi-component deconvolution. The advantage of this method is because of the spectral overlapping of the components in the frequency-wavenumber domain, thus the perpendicularity of input components is preserved (signals are not interconnected) and similarities between components are maintained that helps improve the quality of reconstruction. The coding of this method has been done in MATLAB environment and results of applying the proposed method on 3-component synthetic and real seismic data are compared to that of the POCS algorithm when applied on each component separately. The results of reconstruction using QPOCS algorithm indicate a better quality for reconstructed seismic data and in the output data, the percentage of produced artifacts is lower than that of the POCS algorithm on each component alone. | ||
| کلیدواژه‌ها [English] | ||
| Three-dimensional interpolation, Three-component seismic acquisition, Fourier transform, Quaternion, Convex set | ||
| مراجع | ||
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