大地电场变化的频谱特征  

SPECTRUM CHARACTERISTICS OF GEOELE-CTRIC FIELD VARIATION

作　　者：叶青[1] 杜学彬[2] 周克昌[1] 李宁[2] 马占虎[2] 

机构地区：[1]中国地震台网中心,中国北京100036 [2]中国地震局兰州地震研究所,中国兰州730000

出　　处：《地震学报》2007年第4期382-390,共9页Acta Seismologica Sinica

基　　金：国家自然科学基金(40474027)资助.

摘　　要：处理了中国大陆地区嘉峪关、昌黎、崇明、蒙城、兴济、宝坻和阳原等7个台的地电场观测数据，应用最大熵谱方法研究了大地电场日变化、地电暴等谱成分的特征．结果表明，大地电场日变化主要是12h的半日波成分最强，24-25h的全日波和8h周期成分次之；地电暴是在大尺度空间同步发生的，其谱值高于日变化谱值约2～3个数量级，主要以较长周期成分为主．这一结果初步解释了大地电场变化的主要谱成分的生成机制．The spectrum characteristics of geoelectric diurnal variation and geoelectric storm have been identified by maximum entropy method, based on geoelectric data from seven stations in the Chinese mainland, including Jiayuguan, Changli and Chongming. The study shows that, in geoelectric diurnal variation, the amplitude of the 12 h semidiurnal wave is the largest, followed in turn by the 24-25 h diurnal wave and the 8 h periodic wave; Geoelectric storm usually occurs in a large-scale space, whose spectrum values are higher than those of geoelectric diurnal variation by 2-3 orders of magnitude. A preliminary interpretation is presented for the generative mechanism of predominant waves in geoelectric field variation.

关 键 词：大地电场 周期 最大熵谱 日变 地电暴 

分 类 号：P319.1[天文地球—固体地球物理学]