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Quasi-analytical method for frequency-to-time conversion in CSEM applications

机译:CSEM应用中频率到时间转换的准分析方法

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摘要

Frequency-to-time transformations are of interest to controlled-source electromagnetic methods when time-domain data are inverted for a subsurface resistivity model by numerical frequency-domain modeling at a selected, small number of frequencies whereas the data misfit is determined in the time domain. We propose an efficient, Prony-type method using frequency-domain diffusive-field basis functions for which the time-domain equivalents are known. Diffusive fields are characterized by an exponential part whose argument is proportional to the square root of frequency and a part that is polynomial in integer powers of the square root of frequency. Data at a limited number of frequencies suffice for the transformation back to the time. In the exponential part, several diffusion-time values must be chosen. Once a suitable range of diffusion-time values are found, the method is quite robust in the number of values used. The highest power in the polynomial part can be determined from the source and receiver type. When the frequency-domain data are accurately approximated by the basis functions, the time-domain result is also accurate. This method is accurate over a wider time range than other methods and has the correct late-time asymptotic behavior. The method works well for data computed for layered and 3D subsurface models.
机译:当通过在选定的少数几个频率上通过数值频域建模将地下电阻率模型的时域数据反转时,受控源电磁方法会进行频率到时间的转换域。我们提出了一种有效的Prony型方法,使用频域扩散域基函数,其时域等效项是已知的。扩散场的特征在于其指数与频率的平方根成正比的指数部分和在频率的平方根的整数次幂上是多项式的部分。有限数量的频率上的数据足以转换回时间。在指数部分,必须选择几个扩散时间值。一旦找到合适的扩散时间值范围,该方法在使用的值数量上就非常可靠。多项式部分中的最高功率可以根据源和接收器类型确定。当通过基函数准确地近似频域数据时,时域结果也将是准确的。与其他方法相比,该方法在更宽的时间范围内都是准确的,并且具有正确的后期渐近行为。该方法适用于为分层和3D地下模型计算的数据。

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