parameter dispersion
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2021 ◽  
Vol 18 (5) ◽  
pp. 664-680
Author(s):  
Xilin Qin ◽  
Zhixian Gui ◽  
Fei Yang ◽  
Yuanyuan Liu ◽  
Wei Jin ◽  
...  

Abstract The frequency-dependent amplitude-versus-offset (FAVO) method has become a practical method for fluid detection in sand reservoirs. At present, most FAVO inversions are based on the assumption that reservoirs are isotropy, but the application effect is not satisfactory for fractured reservoirs. Hence, we analyse the frequency variation characteristics of anisotropy parameters in tight sandstone reservoirs based on a new petrophysical model, and propose a stepwise anisotropic FAVO inversion method to extract frequency-dependent attributes from prestack seismic field data. First, we combine the improved Brie's law with the fine-fracture model to analyse frequency-dependent characteristics of velocities and Thomsen anisotropy parameters at different gas saturations and fracture densities. Then, we derive an anisotropic FAVO inversion algorithm based on Rüger's approximation formula and propose a stepwise anisotropic FAVO inversion method to obtain the dispersions of anisotropy parameters. Finally, we propose a method that combines the inversion spectral decomposition with the stepwise anisotropy FAVO inversion and apply it to tight sand reservoirs in the Xinchang area. We use P-wave velocity dispersion and anisotropy parameter ε dispersion to optimise favourable areas. Numerical analysis results show that velocity dispersion of the P-wave is sensitive to fracture density, which can be used for fracture prediction in fractured reservoirs. In contrast, anisotropic parameter dispersion is sensitive to gas saturation and can be used for fluid detection. The seismic data inversion results show that velocity dispersion of the P-wave and anisotropic parameter dispersion are sensitive to fractured reservoirs in the second member of Xujiahe Group, which is consistent with logging interpretation results.


2018 ◽  
Vol 28 (7) ◽  
pp. 1-6 ◽  
Author(s):  
Denis Crete ◽  
Amacoumba Sene ◽  
Aime Labbe ◽  
Eliana Recoba Pawlowski ◽  
Julien Kermorvant ◽  
...  

Author(s):  
Jiang Fan ◽  
Gaoxiang Chen ◽  
Xiuli Shen ◽  
Tianyi Fan

For the deviation of replacing the actual physical model with the surrogate model in the probability analysis of the turbine disk life, an uncertainty evaluation method of reliability calculation of turbine disk life considering the geometric parameter dispersion and surrogate model error is developed. The main approach of this method is to quantify the maximum fluctuation range of the prediction life of the surrogate model and the maximum fluctuation range of the prediction life deviation between the surrogate model and the life model. The safety margin of turbine disc life is calculated and evaluated. Finally, the quantitative evaluation of uncertainty of the low cycle fatigue life of the engine GH720Li turbine disk is completed by this method.


2009 ◽  
Vol 57 (6) ◽  
pp. 1027-1033 ◽  
Author(s):  
Zhanshan Xiao ◽  
Shengwen Zhang ◽  
Tiexuan Zhang ◽  
Shihe Zhu ◽  
Jing Ma

2008 ◽  
Vol 617 ◽  
pp. 187-205 ◽  
Author(s):  
JOHN P. BOYD ◽  
CHENG ZHOU

The Kelvin wave is the lowest eigenmode of Laplace's tidal equation and is widely observed in both the ocean and the atmosphere. In this work, we neglect mean currents and instead include the full effects of the Earth's sphericity and the wave dispersion it induces. Through a mix of perturbation theory and numerical computations using a Fourier/Newton iteration/continuation method, we show that for sufficiently small amplitude, there are Kelvin travelling waves (cnoidal waves). As the amplitude increases, the branch of travelling waves terminates in a so-called corner wave with a discontinuous first derivative. All waves larger than the corner wave evolve to fronts and break. The singularity is a point singularity in which only the longitudinal derivative is discontinuous. As we solve the nonlinear shallow water equations on the sphere, with increasing ε (‘Lamb's parameter’), dispersion weakens, the amplitude of the corner wave decreases rapidly, and the longitudinal profile of the corner wave narrows dramatically.


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