Practical Application of Surface-Wave Methods to Estimate a Near-Surface Velocity Model at Spring Coulee
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Practical Application of Surface-Wave Methods to Estimate a Near-Surface Velocity Model at Spring Coulee Khaled Al Dulaijan; Khaled Al Dulaijan Saudi Aramco Search for other works by this author on: This Site Google Scholar Robert R. Stewart Robert R. Stewart Saudi Aramco Search for other works by this author on: This Site Google Scholar Paper presented at the SPE/DGS Saudi Arabia Section Technical Symposium and Exhibition, Al-Khobar, Saudi Arabia, April 2010. Paper Number: SPE-136929-MS https://doi.org/10.2118/136929-MS Published: April 04 2010 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Get Permissions Search Site Citation Al Dulaijan, Khaled , and Robert R. Stewart. "Practical Application of Surface-Wave Methods to Estimate a Near-Surface Velocity Model at Spring Coulee." Paper presented at the SPE/DGS Saudi Arabia Section Technical Symposium and Exhibition, Al-Khobar, Saudi Arabia, April 2010. doi: https://doi.org/10.2118/136929-MS Download citation file: Ris (Zotero) Reference Manager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentAll ProceedingsSociety of Petroleum Engineers (SPE)SPE Kingdom of Saudi Arabia Annual Technical Symposium and Exhibition Search Advanced Search Abstract Variations in the thicknesses and velocities of near-surface layers can cause serious problems for seismic reflection imaging of the deeper subsurface. Static corrections, calculated from near-surface velocity models, are used to remove the effects of the variable near surface. In this paper, near-surface layers are characterized using a method known as Multi-Channel Analysis of Surface Waves (MASW). This method is mainly used for geotechnical engineering applications and is based on the dispersion properties of Rayleigh-waves. Here, it will be used for calculating S-wave statics for a site located at Spring Coulee, Alberta. The results will be compared to those generated by applying Generalized Linear Inversion (GLI) of first arrival times; a widely used and proven method for obtaining near-surface velocity models for both P- and S-waves.In the case of an isotropic homogeneous half space, Rayleigh-waves are non-dispersive with different frequencies traveling at the same velocity. In a real layered earth, Rayleigh-waves are dispersive (the velocity is dependent on frequency) with multiple modes. The phase velocity of surface waves traveling through a layered earth model is a function of the frequency and four earth parameters; P-wave velocity, S-wave velocity, density, and the layer thickness. The Rayleigh-wave phase velocity is most sensitive to the S-wave velocity and the layer thickness. From an initial model, Rayleigh-wave phase velocities of different frequencies (dispersion curves) are calculated, and then compared to the measured dispersion curves. Then the initial model is updated until some acceptable agreement with the measured dispersion curves is reached.In the Spring Coulee analysis area, the S-wave near-surface models, obtained by the GLI method, had different velocity layering and base of weathering from those of the Pwaves. The MASW S-wave velocity model correlated well to the GLI model. For converted wave PS sections, the improvement in the quality of reflection events after applying S-wave statics from the MASW model is similar to the event quality after application of the S-wave statics from the GLI refraction model. Identifying and picking S-wave first arrivals manually is a difficult and time consuming process. Unfortunately, automatic picking programs do not work well for S-wave refractions. Confusing S-waves with Rayleigh-waves is also a problem. Picking fundamental modes dispersion curves of Rayleigh-waves is easy and fast. Therefore, the MASW method is a potential alternative to the GLI method for modeling S-wave velocities of the near surface. Keywords: spring coulee, society of petroleum engineers, s-wave velocity, s-wave velocity model, dispersion curve, near-surface velocity model, upstream oil & gas, geophysics, thickness, surface-wave method Subjects: Reservoir Characterization, Seismic processing and interpretation Copyright 2010, Society of Petroleum Engineers You can access this article if you purchase or spend a download.
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| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,001 | 0,002 |
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| Méta-épidémiologie (sens large) | 0,000 | 0,001 |
| Bibliométrie | 0,001 | 0,001 |
| Études des sciences et des technologies | 0,001 | 0,000 |
| Communication savante | 0,001 | 0,001 |
| Science ouverte | 0,001 | 0,001 |
| Intégrité de la recherche | 0,001 | 0,001 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,003 | 0,001 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
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