Basic Electromagnetic Experiments¶
In Case Histories we list a number of problems of relevance to today’s society. In most of those problems there is a requirement to determine what is beneath the surface without direct sampling. This is the realm of geophysics. In a generic geophysical survey, energy is input to the ground. This energy propagates through the subsurface and signals are recorded. We briefly discuss each of the elements involved in a generic geophysical survey below.
Physical properties : Earth materials can be characterized in terms of their physical properties. The properties of relevance to electromagnetics are:
The success of a geophysical survey depends upon how the physical properties of a sought target or geologic structure differ from the background host material. If difference exist, then a particular geophysical survey that is sensitive to that physical property can be selected. In Case Histories the reader is invited to view each of the problems and determine which of the above properties, or any, might be useful. Making this connection is the most crucial element in the successful use of geophysics.
Source: A source provides initial energy that will excite the earth. We are interested only in sources for electromagnetic energy. Man-made sources involve electrical currents that are either injected into the earth or flow in a wire-loop. “Natural” sources refer to the energy fields that arise from the earth and its environment. For example, the solar wind and its interation with our magnetosphere, or the generation of magnetic fields due to the geomagnetic dynamo in the Earth’s core. The input signals to the earth can be harmonic or transient. Correspondingly the equations that propagate the energy through the earth are FDEM (Frequency Domain ElectroMagnetic) or TDEM (Time Domain ElectroMagnetic). The way in which this energy propagates depends upon how the physical properties vary inside the earth.
Data: The electromagnetic fields at the earth’s surface are recorded by “electromagnetic sensors” or “receivers”. The receivers can be in the air, on the surface or undergound. The data, which are components of the magnetic or electric fields, contain information about the physical properties through which they travelled.
Although the data contain information about the subsurface, subsequent processing and inversion are required to extract meaningful information. This is conceptualized in Fig. 2. The item “Forward” refers to predicting the electromagnetic responses from the survey when the physical properties are known. The item “Inverse” refers to the procedure for generating a physical property distribution that explains the observations.