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Swept impact seismic technique (SIST)

机译:后掠冲击地震技术(SIST)

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A coded seismic technique is developed that can result in a higher signal-to-noise ratio than a conventional single-pulse method does. The technique is cost-effective and time-efficient and therefore well suited for shallow-reflection surveys where high resolution and cost-effectiveness are critical. A low-power impact source transmits a few to several hundred high- frequency broad-band seismic pulses during several seconds of recording time according to a deterministic coding scheme. The coding scheme consists of a time-encoded impact sequence in which the rate of impact (cycles/s) changes linearly with time providing a broad range of impact rates. Impact times used during the decoding process are recorded on one channel of the seismograph. The coding concept combines the vibroseis swept-frequency and the Mini-Sosie random impact concepts. The swept-frequency concept greatly improves the suppression of correlation noise with much fewer impacts than normally used in the Mini-Sosie technique. The impact concept makes the technique simple and efficient in generating high-resolution seismic data especially in the presence of noise. The transfer function of the impact sequence simulates a low-cut filter with the cutoff frequency the same as the lowest impact rate. This property can be used to attenuate low-frequency ground-roll noise without using an analog low-cut filter or a spatial source (or receiver) array as is necessary with a conventional single-pulse method. Because of the discontinuous coding scheme, the decoding process is accomplished by a "shift-and-stacking" method that is much simpler and quicker than cross-correlation. The simplicity of the coding allows the mechanical design of the source to remain simple. Several different types of mechanical systems could be adapted to generate a linear impact sweep. In addition, the simplicity of the coding also allows the technique to be used with conventional acquisition systems, with only minor modifications.
机译:已开发出一种编码地震技术,该技术可比传统的单脉冲方法产生更高的信噪比。该技术具有成本效益和时间效率,因此非常适合于高分辨率和成本效益至关重要的浅反射测量。根据确定性编码方案,低功率冲击源在记录时间的几秒钟内会发送几百到几百个高频宽带地震脉冲。编码方案由时间编码的冲击序列组成,其中冲击速率(周期/秒)随时间线性变化,从而提供了广泛的冲击速率。解码过程中使用的冲击时间记录在地震仪的一个通道上。编码概念结合了震颤频率和Mini-Sosie随机冲击概念。扫频概念大大改善了相关噪声的抑制,其影响比Mini-Sosie技术中通常使用的冲击少得多。冲击概念使该技术在生成高分辨率地震数据时特别简单且有效,特别是在存在噪声的情况下。冲击序列的传递函数模拟了一个低截止滤波器,其截止频率与最低冲击率相同。此属性可用于衰减低频地面噪声,而无需使用常规单脉冲方法所需的模拟低切滤波器或空间源(或接收器)阵列。由于不连续的编码方案,解码过程是通过“移位和堆叠”方法来完成的,该方法比互相关要简单得多,也要快得多。编码的简单性使信号源的机械设计保持简单。几种不同类型的机械系统可以适用于产生线性冲击波。另外,编码的简单性也使得该技术仅需很小的修改就可以与常规的采集系统一起使用。

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