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ISSN 2096-7780 CN 10-1665/P

基于FY-3E卫星的山东德州Ms5.5地震OLR异常研究

Study on OLR anomalies of Dezhou Ms5.5 earthquake in Shandong province based on FY-3E satellite

  • 摘要: 依据天体引潮力变化周期,利用FY-3E卫星射出长波辐射(OLR)数据,分析了中国大陆大范围(17°~55°N,73°~136°E)内6月30日至8月30日OLR逐日连续变化特征,探讨了引潮力、OLR和2023年8月6日德州平原县发生5.5级地震的关联特征。依据引潮力变化周期同步监测OLR变化图像显示:(1)无震引潮力变化的(震前A和B、震后D)周期,震中附近OLR无明显变化;而发震周期(C周期)同步观测到连续的OLR异常,且伴随引潮力由低谷-高峰-低谷的持续变化,OLR异常在时间上呈现出初始增温-加强-高峰-衰减-逐渐平静的阶段性特征,二者在时间上具有同步性;(2)OLR异常在空间上紧紧围绕聊城-兰考断裂分布,表明地震构造运动是德州平原地震OLR异常变化的主控原因,而地震过程中OLR异常演变特征则是地震构造应力变化的辐射表征;(3)地震发生在C周期的波峰相位点附近,结合同步监测到的OLR异常增强特征,表明当地震构造应力积累到岩石破裂滑动的临界状态时,引潮力大小和方向的突然改变促使聊城-兰考断裂失稳而诱发了地震。以上结果也说明FY-3E卫星OLR产品可较好地应用于地震红外异常研究。

     

    Abstract: Based on the variation cycle of tidal force, the continuous daily variation characteristics of Out Long-wave Radiation (OLR) from June 30 to August 30 in a large area (17°~55°N, 73°~136°E) of the Chinese mainland were analyzed by using the FY-3E satellite OLR data, and the correlation characteristics of tidal force, OLR and the Ms5.5 earthquake in Pingyuan County, Dezhou on August 6, 2023 is discussed. The images of OLR changes monitored synchronously according to the cycle of tidal force changes show that: (1) during the cycle of tidal force changes (A and B cycle before the earthquake and D cycle after the earthquake), OLR near the epicenter shows no significant changes; while the continuous OLR anomalies are observed synchronously during the C cycle of seismogenesis, and accompanied by the continuous change of tidal force from trough to peak to trough, the OLR anomalies show the stage characteristics of initial warming-strengthening-peak-attenuation-gradually calming, which are synchronous in time. (2) OLR anomalies are closely distributed around the Liaocheng-Lankou fault in space, indicating that seismic tectonic movement is the main cause of OLR anomalies of the earthquake, and the evolution characteristics of OLR anomalies during the earthquake is the radiation representation of seismic tectonic stress changes. (3) The earthquake occurred near the peak phase point of the C cycle, combining with the synchronous monitoring of the enhanced characteristics of the OLR anomalies, it is shown that when the seismic tectonic stress accumulates to the critical state of rock fracture and sliding, the sudden change of the size and direction of the tidal force promotes the instability of the Liaocheng-Lankou fault and induces the earthquake. The above results also show that the OLR products of FY-3E satellite can be well applied to the research of seismic infrared anomalies.

     

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