Passive earthquake monitoring data compression method and control system
A technology for monitoring data and passive earthquakes, applied in seismic signal processing, etc., can solve problems such as large amount of transmitted data, difficult to meet real-time transmission, and occupying large disk resources
Patent Information
- Authority / Receiving Office
- CN · China
- Patent Type
- Applications(China)
- Current Assignee / Owner
- Publication Date
- 2013-07-17
- Estimated Expiration
- Not applicable · inactive patent
Smart Images
Figure 1 Figure 2 Figure 3
Abstract
Description
technical field
[0001] The invention relates to the technical field of data collection and processing, in particular to a passive seismic monitoring data compression method and a control system. Background technique
[0002] In the prior art, the transmission of passive seismic monitoring data generally adopts direct transmission or compressed retransmission. However, due to the strong uncertainty and unpredictability of passive seismic events, it is generally necessary to use all-weather real-time monitoring, and the frequency of seismic events Generally, it is 10-1500Hz, and the sampling rate of existing equipment can reach up to 10KHz, so the data generated by monitoring is very large, which causes great difficulties for wireless long-distance real-time data transmission, and takes up a lot of disk storage space. For example, if 20 three-component detectors are deployed on the ground, the sampling rate is 10KHz, and the digital signal precision is 24bit, then 18.31Mb of d...
Examples
Embodiment Construction
[0057] A method for compressing passive seismic monitoring data, comprising the following steps:
[0058] Step 1. Identification of seismic events: see image 3 , under a certain signal-to-noise ratio condition, the energy of the seismic record before and after the earthquake event, that is, the amplitude in the seismic record will have a relatively obvious difference. The average value of the amplitude of seismic signals in the window changes quickly, and the corresponding increase in the ratio R of the two will be more obvious. When the ratio R is greater than a set threshold T, that is, the threshold set by the control system, and continuously greater than this When the number GW of the R value of the threshold T is greater than the critical window TW, it is determined that a seismic event has occurred; when the energy change is not obvious when the event arrives, the event may be missed by directly calculating the amplitude of the original signal, so the introduction a ne...