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GPR imaging strategies for subsurface object detection from coherent radiometry data

机译:利用GPR成像策略从相干辐射数据中检测地下物体

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摘要

Two different interferometric methodologies are described that allow for extracting Green's functions between two or many receivers from noise recordings. One is the cross correlation method and the other is the deconvolution method. The cross correlation method works well with noise sources on a boundary for non-dissipative media. There is an exception, when all sources enclose a non-dissipative medium and the dissipative part of the medium occurs only on one side of all the sources. Then the Green's function can be extracted when at least on of the receivers is enclosed by all sources, while the other is free to be located in the dissipative part of the medium. The second extracts a Green's function in the form of a reflection response for many receivers simultaneously and requires multi component and multi offset data that is recorded in a plane located on one side of all sources. The advantage of this second method is that is robust for dissipation anywhere in the medium and that the medium on the source side of the receivers is homogenized.
机译:描述了两种不同的干涉测量方法,这些方法允许从噪声记录中提取两个或多个接收机之间的格林函数。一种是互相关方法,另一种是去卷积方法。互相关方法可以很好地处理非耗散介质边界上的噪声源。有一个例外,当所有源封闭一个非耗散介质,并且介质的耗散部分仅出现在所有源的一侧时。然后,当至少一个接收器被所有信号源包围,而另一个接收器自由地位于介质的耗散部分时,可以提取格林函数。第二个方法同时针对许多接收器提取反射响应形式的格林函数,并且需要记录在位于所有源一侧的平面上的多分量和多偏移量数据。第二种方法的优点是对于介质中的任何位置的散布都是健壮的,并且接收器源侧的介质是均匀的。

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