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This paper deals with the response features of AR(apparent ratio of seismic wave velocities to the changes of TR(true ratio of wave velocities)in the horizontal layered model by mathematical modeling.The results show that:(1)the response features of AR are associated with the parameters of the structure and its dynamic changes,and the relative position between the hypocenters and the monitoring networks,showing complicated patterns strongly related to the concrete paths of propagation of seismic waves from the source to the receiver in the observatories of the network;(2)the depth of the seismic source would have important influence on the response features of AR,especially the capacity to carry the anomalous information in the condition of the earth media,being in the anomalous state would be greater for those earthquakes which occur inside the anomalous layers than those underneath the anomalous layers;(3)the response features of AR are clearly related to the changes of TR(true ratio of wave velocities)instead of changes of wave velocities themselves,i.e.the response could be small as the changes in TR is small even in the case of large changes in the wave velocities.It is suggested that more attention must be paid to all these features in combination with detailed investigation of the velocity structure of the earth media in the study region and best fitting of precise hypocenter locations when one wants to obtain the reliable precursors from the changes in AR.
This paper deals with the response features of AR (apparent ratio of seismic wave velocities to the changes of TR (true ratio of wave velocities) in the horizontal layered model by mathematical modeling. The results show that: (1) the response features of AR are associated with the parameters of the structure and its dynamic changes, and dynamic changes, and the relative positions between the hypocenters and the monitoring networks, showing complicated patterns strongly related to the concrete paths of propagation of seismic waves from the source to the receiver in the observatories of the (2) the depth of the seismic source would have important influence on the response features of AR, especially the capacity to carry the anomalous information in the condition of the earth media, being in the anomalous state would be greater for those earthquakes which occur inside the anomalous layers than those underneath the anomalous layers; (3) the response features of AR are clearly related to the changes of TR (true ratio of wave velocities instead of changes of wave velocities themselves, iethe response could be small as the changes in TR is small even in the case of large changes in the wave velocities. It is suggested that more attention must be paid to all these features in combination with detailed investigation of the velocity structure of the earth media in the study region and best fitting of precise hypocenter locations when one wants to obtain the reliable precursors from the changes in AR.