利用主动式和被动式近场水听器成像阿布扎比近海超浅水近水面

O. Khakimov, Y. Gholami, B. Tertrais, G. Cambois, M. Mahgoub
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引用次数: 1

摘要

地震勘探通常被设计成对深层储层进行成像,这使得近地表的采样严重不足。在阿布扎比近海,这是一个特别的挑战,那里有复杂的近地表,有岩溶塌陷和蜿蜒的河道,会用强烈的足迹污染地震图像。为了减轻这些影响,我们使用了近场水听器数据,主要用于对气枪源进行QC,用于近地表成像。近场水听器(NFH)位于每个气枪上方约一米处,用于记录源近场压力。他们立即捕捉到不正常或不符合规格的枪支,这提醒了录音人员。然而,在浅水环境中,它们无意中记录了近地表的地震反射,我们将使用这些反射来进行地震成像。拖缆船通常使用两个相距50米的源阵列,以触发器模式发射。主动NFH是指射击枪正上方的记录,而被动NFH是指来自非射击阵列的记录。由于被动NFH受源近场污染较少,因此它们通常是近地表成像的首选。阿布扎比近海水域太浅,不能使用拖带船。相反,地震调查涉及海底电缆(OBC)或节点(OBN)和较小的气枪阵列。射击容器可以是单源的,也可以是双源的。单源容器只有主动NFH,而双源容器同时具有主动和被动NFH。然而,即使使用双源船,射源阵列与被动NFH之间50 m的距离也太大,无法捕获水深小于25 m的海底反射。基于这些原因,我们建议将两种测量方法结合起来,在非常浅的部分使用主动NFH,在较深的部分使用被动NFH。我们已将该技术应用于最近在阿布扎比近海获得的节点调查。通过结合主动和被动NFH,可以获得非常高分辨率的浅层图像,从而可以解释位于海底以下的地质层。与高分辨率二维现场调查图像的对比显示出良好的一致性。由于NFH不需要任何额外的采集,并且是作为标准地震调查的副产品提供的,我们已经证明,正确使用NFH可以为现场前调查解释提供高质量的图像,从而减少了对额外且昂贵的岩土工程调查的需求。这是首次在阿布扎比浅水区使用主动式和被动式NFH进行成像。浅层地层图像的分辨率允许进行常规地震数据无法实现的详细解释。从长远来看,这种技术可以减少额外的实地调查。
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Using Active and Passive Near-Field Hydrophones to Image the Near-Surface in Ultra-Shallow Waters Offshore Abu Dhabi
Seismic surveys are generally designed to image deep reservoirs, which leaves the near-surface woefully under-sampled. This is particularly a challenge offshore Abu Dhabi, where a complex near-surface – with karstic collapses and meandering channels – contaminates the seismic image with strong footprints. To mitigate these effects, we use near-field hydrophone data, primarily designed to QC the airgun source, for near-surface imaging. Near-field hydrophones (NFH) are positioned about a meter above each airgun and are designed to record the source near-field pressure. They immediately capture dysfunctional or out-of-spec guns, which alerts the recording crew. Yet, in a shallow water environment, they unintentionally record seismic reflections from the near-surface, which we will use for seismic imaging. Streamer vessels usually use two source arrays, 50 meters apart, which shoot in a flip-flop mode. The active NFH refer to the recordings directly above the shooting guns, while the passive NFH refer to the recordings from the array that is not shooting. Because the passive NFH are less contaminated by the source near-field, they are typically the preferred choice for near-surface imaging. Waters are too shallow in offshore Abu Dhabi to use streamer vessels. Instead, seismic surveys involve ocean-bottom cables (OBC) or nodes (OBN) and smaller airgun arrays. The shooting vessels can be single-source or dual-source. While a single source vessel has only active NFH, a dual source vessel has both active and passive NFH. However, even if a dual-source vessel is used, the 50 m distance between the shooting source array and the passive NFH is too large to capture the water-bottom reflection for water-depths shallower than 25 m. For these reasons, we propose to combine both measurements, using active NFH for the very shallow section and passive NFH for the deeper section. We have applied this technique to a recent node survey acquired offshore Abu Dhabi. By combining the active and passive NFH, a very high-resolution shallow image was obtained, which allows the interpretation of geological layers just below the water bottom. Comparisons with high resolution 2D site survey images show good agreement. Given the NFH do not require any additional acquisition and are delivered as a byproduct of standard seismic surveys, we have demonstrated that proper use of NFH can provide high quality images for pre-site survey interpretation, which reduces the need for additional – and expensive – geotechnical surveys. This is the first published use of combined active and passive NFH in Abu Dhabi shallow waters for the purpose of imaging. The resolution of the shallow formation images allows detailed interpretation not achievable using conventional seismic data. In the long term, this technique may reduce the need for additional site survey acquisitions.
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