基于NAD算子的高精度低数值频散地震波模拟方法
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摘要
基于二维声波方程,使用四阶截断的泰勒展开式离散时间偏导数,利用八阶精度的近似解析离散算子离散空间高阶偏导数,发展了一种八阶ONAD方法.通过数值误差、计算效率和复杂介质波场模拟等考察研究,结果均显示该方法在压制数值频散、计算效率和波场模拟精度等方面明显优越于四阶LAX-Wendroff Corrected(LWC)方法和八阶LWC方法.因此,八阶ONAD方法是一种有望在地震波模拟得到应用的十分有效的数值模拟方法.
The eighth-order ONAD method is developed for solving the 2-D acoustic wave equation.The new method uses the fourth-order truncated Taylor expansion to discretize partial derivative of time,and employs the eighth-order nearly analytic discrete operator discretize high-order partial derivatives of space.Through studying the numerical error,computational efficiency and complex medium wave-field simulations,those results show that this method is obviously superior to the fourth-order LAX-Wendroff Corrected(LWC)method and the eighth-order LWC method in suppressing the numerical dispersion,computational efficiency and simulation precision of wave-fields.Therefore,the eighth-order ONAD method is a very effective method of numerical simulation and can be applied in the seismic wave simulation.
引文
Cerveny V,Firbas P.1984.Numerical modelling and inversion of travel times of seismic body waves in inhomogeneous anisotropic media[J].Geophys.J.Int.,76(1):41-51.
    pyChapman C H,Shearer P M.1989.Ray tracing in azimuthally anisotropic media-Ⅱ:quasi-shear wave coupling[J].Geophys.J.Int.,96(1):65-83.
    Chen K H.1984.Propagating numerical model of elastic wave in anisotropic in homogeneous media-finite element method[C].Symposium of 54th SEG,54:631-632.
    Dablain M A.1986.The application of high-order differencing to the scalar wave equation[J].Geophysics,51(1):54-66.
    Dong L G,Ma Z T,Cao J Z,et al.2000.A staggered-grid highorder difference method of one-order elastic wave equation[J].Chinese J.Geophys.(in Chinese),43(3):411-419.
    Fei T,Larner K.1995.Elimination of numerical dispersion in finitedifference modeling and migration by flux-corrected transport[J].Geophysics,60(6):1830-1842.
    Huang B S.1992.A program for two-dimensional seismic wave propagation by the pseudospectrum method[J].Comput.Geosci.,18(2-3):289-307.
    Kelly K R,Ward R W,Treitel S,et al.1976.Synthetic seismograms;a finite-difference approach[J].Geophysics,41(1):2-27.
    Komatitsch D,Vilotte J P.1998.The spectral element method:an efficient tool to simulate the seismic response of 2Dand 3D geological structures[J].Bull.Seism.Soc.Am.,88(2):368-392.
    Lu M,Yang D H.2005.A modified nearly analytic discrete method and wavefield simulations in transversely isotropic media[J].Sci.in China(Ser.D Earth Sci.),48(8):132l-1328.
    Ma X,Yang D H,Zhang J H.2010.Symplectic partitioned RungeKutta method for solving the acoustic wave equation[J].Chinese J.Geophys.(in Chinese),53(8):1993-2003,doi:10.3969/j.issn.0001-5733.2010.08.026.
    Song G J,Yang D H,Chen Y L,et al.2010.Non-uniform grid algorithm based on the WNAD method and elastic wave-field simulations[J].Chinese J.Geophys.(in Chinese),53(8):1985-1992,doi:10.3969/j.issn.00015733.2010.08.025.
    Tong P,Yang D H,Hua B L,et al.2013.A high-order stereomodeling method for solving wave equations[J].Bulletin of the Seismological Society of America,103(2):811-833.
    Virieux J.1984.SH-wave propagation in heterogeneous media:velocity-stress finite-difference method[J].Geophysics,49(11):1933-1957.
    Virieux J.1986.P-SV wave propagation in heterogeneous media:velocity-stress finite-difference method[J].Geophysics,51(4):889-901.
    Wang L,Yang D H,Deng X Y.2009.A WNAD method for seismic stress-field modeling in heterogeneous media[J].Chinese J.Geophys.(in Chinese),52(6):1526-1535.
    Yang D H.2002.Finite element method of the elastic wave equation and wave field simulation in two-phase anisotropic media[J].Chinese J.Geophys.(in Chinese),45(4):575-583.
    Yang D H,Liu E,Zhang Z J,et al.2002.Finite-difference modelling in two-dimensional anisotropic media using a fluxcorrected transport technique[J].Geophys.J.Int.,148(2):320-328.
    Yang D H,Lu M,W u R S,et al.2004.An optimal nearly analytic discrete method for 2Dacoustic and elastic wave equations[J].Bul1.Seism.Sac.Am.,94(5):1982-1992.
    Yang D H,Peng J M,Lu M,et al.2006a.A nearly analytical discrete method for wave-field simulations in 2Dporous media[J].Commun.Cornput.Phys.,1(3):528-547.
    Yang D H,Peng J M,Lu M,et al.2006b.Optimal nearly analytic discrete approximation to the scalar wave equation[J].Bul1.Seisrn.Soc.Am.,96(3):1114-1130.
    Yang D H,Teng J W,Zhang Z J,et al.2003.A nearly analytic discrete method for acoustic and elastic wave equations in anisotropic media[J].Bull.Seism.Soc.Am.,93(2):882-890.
    Zhang Z J,Wang G J,Harris J M.1999.Multi-component wavefield simulation in viscous extensively dilatancy anisotropic media[J].Phys.Earth Planet Inter.,114(1-2):25-38.
    董良国,马在田,曹景忠,等.2000.一阶弹性波方程交错网格高阶差分解法[J].地球物理学报,43(3):411-419.
    卢明,杨顶辉.2005.一种改进的近似解析离散化方法及其横向各向同性波场模拟[J].中国科学(D辑:地球科学),35(1):72-78.
    马啸,杨顶辉,张锦华.2010.求解声波方程的辛可分Runge-Kutta方法[J].地球物理学报,53(8):1993-2003,doi:10.3969/j.issn.0001-5733.2010.08.026.
    宋国杰,杨顶辉,陈亚丽,等.2010.基于WNAD方法的非一致网格算法及其弹性波场模拟[J].地球物理学报,53(8):1985-1992,doi:10.3969/j.issn.00015733.2010.08.025.
    王磊,杨顶辉,邓小英.2009.非均匀介质中地震波应力场的WNAD方法及其数值模拟[J].地球物理学报,52(6):1526-1535.
    杨顶辉.2002.双相各向异性介质中弹性波方程的有限元解法及波场模拟[J].地球物理学报,45(4):575-583.

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