Accurate determination of seismic velocity of the crust is important for understanding regional tectonics and crustal evolution of the Earth. We propose a stepwise joint linearized inversion method using surface wave ...Accurate determination of seismic velocity of the crust is important for understanding regional tectonics and crustal evolution of the Earth. We propose a stepwise joint linearized inversion method using surface wave dispersion, Rayleigh wave ZH ratio （i.e., ellipticity）, and receiver function data to better resolve 1D crustal shear wave velocity （Vs） structure. Surface wave dispersion and Rayleigh wave ZH ratio data are more sensitive to absolute variations of shear wave speed at depths, but their sensi- tivity kernels to shear wave speeds are different and complimentary. However, receiver function data are more sensitive to sharp velocity contrast （e.g., due to the existence of crustal interfaces） and Vp/Vs ratios. The stepwise inversion method takes advantages of the complementary sensitivities of each dataset to better constrain the Vs model in the crust. We firstly invert surface wave dispersion and ZH ratio data to obtain a 1D smooth absolute vs model and then incorporate receiver function data in the joint inver- sion to obtain a finer Vs model with better constraints on interface structures. Through synthetic tests, Monte Carlo error analyses, and application to real data, we demonstrate that the proposed joint inversion method can resolve robust crustal Vs structures and with little initial model dependency.展开更多
在n-Rayleigh信道下,研究了使用选择合并(SC)接收的移动无线传感器网络系统的平均符号误码率(ASEP)和信道容量。基于矩生成函数(MGF)方法,推导了系统采用相干检测的相移键控调制(PSK),正交幅度调制(QAM),脉冲幅度调制(PAM)等数字调制方...在n-Rayleigh信道下,研究了使用选择合并(SC)接收的移动无线传感器网络系统的平均符号误码率(ASEP)和信道容量。基于矩生成函数(MGF)方法,推导了系统采用相干检测的相移键控调制(PSK),正交幅度调制(QAM),脉冲幅度调制(PAM)等数字调制方式的ASEP的精确表达式。同时,也得到了系统信道容量的精确表达式。然后对不同条件下的ASEP和信道容量性能做了数值仿真,理论分析结果与仿真结果相吻合,验证了理论分析结果的正确性。仿真结果表明:随着分集支路数的增加,系统的ASEP和信道容量性能得到了很好的改善,当使用QPSK调制,信噪比为16 d B时,分集支路数L=1,系统的误码率是6×10-2,信道容量是4(bit/s)/Hz;分集支路数L=2,系统的误码率是1×10-2,信道容量是5.1(bit/s)/Hz;分集支路数L=3,系统的误码率是2×10-3,信道容量是5.8(bit/s)/Hz。展开更多
在n-Rayleigh信道下,研究了MRC(Maximal Ratio Combining)合并接收系统的平均码字错误率(ASEP)性能。基于矩生成函数(MGF)的方法,推导了MRC接收系统在n-Rayleigh衰落信道上采用M进制相移键控(MPSK),M进制正交幅度调制(MQAM)和M进制脉冲...在n-Rayleigh信道下,研究了MRC(Maximal Ratio Combining)合并接收系统的平均码字错误率(ASEP)性能。基于矩生成函数(MGF)的方法,推导了MRC接收系统在n-Rayleigh衰落信道上采用M进制相移键控(MPSK),M进制正交幅度调制(MQAM)和M进制脉冲幅度调制(MPAM)等几种M进制数字调制方式的ASEP的计算式。然后在不同条件下,仿真了系统的ASEP性能,仿真值与理论值相一致,理论分析的正确性得到了证明。分析结果表明:分集支路数和衰弱因子对系统的ASEP性能有重要影响。展开更多
基金supported by the National Earthquake Science Experiment in Sichuan and Yunnan Provinces of China(#2016 CESE 0201)National Natural Science Foundation of China(#41574034)China National Special Fund for Earthquake Scientific Research in Public Interest(#201508008)
文摘Accurate determination of seismic velocity of the crust is important for understanding regional tectonics and crustal evolution of the Earth. We propose a stepwise joint linearized inversion method using surface wave dispersion, Rayleigh wave ZH ratio （i.e., ellipticity）, and receiver function data to better resolve 1D crustal shear wave velocity （Vs） structure. Surface wave dispersion and Rayleigh wave ZH ratio data are more sensitive to absolute variations of shear wave speed at depths, but their sensi- tivity kernels to shear wave speeds are different and complimentary. However, receiver function data are more sensitive to sharp velocity contrast （e.g., due to the existence of crustal interfaces） and Vp/Vs ratios. The stepwise inversion method takes advantages of the complementary sensitivities of each dataset to better constrain the Vs model in the crust. We firstly invert surface wave dispersion and ZH ratio data to obtain a 1D smooth absolute vs model and then incorporate receiver function data in the joint inver- sion to obtain a finer Vs model with better constraints on interface structures. Through synthetic tests, Monte Carlo error analyses, and application to real data, we demonstrate that the proposed joint inversion method can resolve robust crustal Vs structures and with little initial model dependency.
文摘在n-Rayleigh信道下,研究了使用选择合并(SC)接收的移动无线传感器网络系统的平均符号误码率(ASEP)和信道容量。基于矩生成函数(MGF)方法,推导了系统采用相干检测的相移键控调制(PSK),正交幅度调制(QAM),脉冲幅度调制(PAM)等数字调制方式的ASEP的精确表达式。同时,也得到了系统信道容量的精确表达式。然后对不同条件下的ASEP和信道容量性能做了数值仿真,理论分析结果与仿真结果相吻合,验证了理论分析结果的正确性。仿真结果表明:随着分集支路数的增加,系统的ASEP和信道容量性能得到了很好的改善,当使用QPSK调制,信噪比为16 d B时,分集支路数L=1,系统的误码率是6×10-2,信道容量是4(bit/s)/Hz;分集支路数L=2,系统的误码率是1×10-2,信道容量是5.1(bit/s)/Hz;分集支路数L=3,系统的误码率是2×10-3,信道容量是5.8(bit/s)/Hz。
文摘在n-Rayleigh信道下,研究了MRC(Maximal Ratio Combining)合并接收系统的平均码字错误率(ASEP)性能。基于矩生成函数(MGF)的方法,推导了MRC接收系统在n-Rayleigh衰落信道上采用M进制相移键控(MPSK),M进制正交幅度调制(MQAM)和M进制脉冲幅度调制(MPAM)等几种M进制数字调制方式的ASEP的计算式。然后在不同条件下,仿真了系统的ASEP性能,仿真值与理论值相一致,理论分析的正确性得到了证明。分析结果表明:分集支路数和衰弱因子对系统的ASEP性能有重要影响。
