摘要
根据电磁场理论,推导了磁偶源和接收点均位于海水中时层状海底模型的频域电磁场响应一般表达式,并通过此式,得到了海水为均匀半空间和有限海水深度两种情况下,垂直磁偶极装置、中心回线和重叠回线分别置于均匀半空间海底表面时的瞬变电磁响应(磁场和感应电压)表达式.这些表达式将瞬变响应和海底的电导率等参数有机联系在一起,为海底瞬变电磁法的正演计算和反演解释提供了理论基础.仿真计算表明,海水的存在不仅使得瞬变响应曲线形态发生变化,而且影响其对海底电导率的分辨能力.
By electromagnetic theory, for the case that the magnetic dipole source and the receiver are set in seawater, the general expressions of frequency-domain electromagnetic responses for a layered benthal model are deduced. From those, the transient response expressions of three common configurations--vertical magnetic dipole-dipole （HZHZ）, central loop, and coincident loop, located on the surface of uniform half-space seafloor, are derived respectively, supposing that seawater is uniform half space, or its depth is finite. These expressions connect transient response with oceanic parameters such as the conductivity of the seafloor, and provide theoretical foundation for forward modeling, and inversion and interpretation in seafloor transient electromagnetic exploration. The modeling indicates that the presence of seawater not only changes the shape of transient response curve, but also reduces the resolution to seafloor conductivity.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2006年第6期1891-1898,共8页
Chinese Journal of Geophysics
基金
国家高技术研究发展计划(863计划)(2002AA615030)资助
关键词
海底
瞬变电磁法
垂直磁偶极装置
中心回线
重叠回线
电磁场
瞬变响应
Seafloor, Transient electromagnetic systems,HZHZ, Central loop, Coincident loop,Electromagnetic field, Transient response
