Diurnal characteristics of geoelectric fields and their changes associated with the Alxa Zuoqi M_S5.8 earthquake on 15 April 2015(Inner Mongolia) |
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Authors: | Qing Ye Ye Fan Xuebin Du Tengfa Cui Kechang Zhou Ramesh PSingh |
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Institution: | 1.China Earthquake Network Center, China Earthquake Administration, Beijing 100045, China2.Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 73000, China3.Institute of Geology, China Earthquake Administration, Beijing 100029, China4.School of Life and Environmental Sciences, Schmid College of Science and Technology, Chapman University, One University Drive, Orange, CA 92866, USA |
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Abstract: | In China, efforts are being made to monitor geoelectric fields through a large network of stations deployed and managed by the China Earthquake Administration. The diurnal variations in the geoelectric field waveforms were similar in the quiet magnetic periods when K5(generally, K3 indicates a quiet time). The arrival time points of the maxima in the geoelectric field waveforms exhibited differences in local time related to geographic longitude. The amplitude of diurnal variation was several to 16.6 mV/km and decreased with increasing latitude. Further,the amplitude of diurnal variation, which was related to seasonal changes, was larger in summer and autumn than in spring and winter. The periods of diurnal changes during quiet days were 24, 12, 8, 6, 4 hours and several minutes over large areas. Finally, the observed diurnal variations in geoelectric field prior to the Alxa Zuoqi M_S5.8 earthquake on 15 April 2015 were studied, and pronounced changes in the spectral values of the geoelectric fields were found to be associated with the Alxa Zuoqi earthquake in Inner Mongolia. |
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Keywords: | Geoelectrical field Diurnal variation Period Alxa Zuoqi earthquake |
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