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Wave equation receiver deghosting: a provocative example

机译:波浪方程式接收机脱毛:一个挑衅的例子

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The problem of counteracting the effects of the receiver ghost in marine data has generally been addressed either by making complementary measurements such as hydrophone pairs or hydrophone and particle velocity sensors or by estimation of the effect through the so-called ghost model. Here, we discuss a technique based on the wave equation that accomplishes up/down wavefield separation based on a single measurement that does not rely on the spectral ghost model and does not rely on statistical or other means of estimating missing frequencies. While it is a distinct advantage to record multiple measurements, such systems are limited in availability and, moreover, significant legacy data exist that could benefit from deghosting. We briefly review the theory for wave equation receiver deghosting - first presented by Beasley et al., (2013) - and then present examples that confirm the accuracy of the approach. We illustrate a significant difference between this approach and many other approaches that use single measurements. Using the notch frequency in a mono-frequency plane wave example, -we show that our approach accurately reconstructs the -upgoing wavefield without benefit of information from other frequencies; a task that we expect would pose challenges to other single-measurement approaches.
机译:抵消在海洋数据接收机幽灵的效果的问题已普遍通过使互补的测量,例如水听器对或水听器和粒子速度传感器或通过的通过所谓的重影模型的效果的估计处理任一。这里,我们讨论基于在完成向上/向下基于不依赖于频谱鬼模型和不依赖于估计丢失频率的统计或其它方法的单次测量波场分离的波动方程的技术。虽然这是一个明显的优势,以记录多次测量,这样的系统在可用性的限制,而且,存在显著遗留数据,可以去鬼影受益。我们简要地回顾了波动方程接收机的去重影的理论 - 首先由比斯利等人提出,(2013年) - 然后是确认方法的准确性目前例子。我们举例说明这种方法,并使用单次测量其他许多方法之间的差异显著。在单频平面波例如使用陷波频率, - 我们表明,我们的方法准确地重建而没有从其它频率信息利益-upgoing波场;一个任务,我们预期会对其他单测量方法的挑战。

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