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A New Method of Semi-Permanent Reservoir Monitoring in Deep Water Using Ocean Bottom Nodes

机译:利用海底节点监测深水半永久性水库的新方法

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Deep water Ocean Bottom Node (OBN) systems have delivered high quality full azimuth 3D and 4Drnseismic data. In this paper, we discuss the development of a new node technology and a new method ofrnemploying nodes for reservoir monitoring, wherein, a high-speed underwater optical communicationsrnsystem is utilized to extract data from nodes that have a long deployment capability, without recoveringrnthe nodes from the seafloor. This highly repeatable semi-permanent 4D monitoring capability can bernimplemented at considerably lower cost than with cable based Permanent Reservoir Monitor (PRM)rnsystems.rnFull azimuth and long offset seismic data acquired with a sparse array of ocean bottom nodes and arndense patch of shots has proven to be a very successful technique for both 3D and 4D imaging belowrncomplex salt overburden in the deep water Gulf of Mexico, where more than 25 OBN surveys have beenrnconducted in the last ten years. Deep water OBN 3D and 4D surveys have also been successfullyrnconducted in offshore West Africa and Brazil. Autonomous deep water OBN systems are proven to bernvery reliable, with 98u0002% data recovery, and nodes are routinely deployed by a remotely operated vehiclern(ROV), amongst field infrastructure and simultaneous operations. Also, for reservoir monitoring, OBNrnsurveys are proven to be highly repeatable, resulting in low 4D noise, NRMS statistics typically less thanrn10%, which is comparable with that achieved using PRM systems.rnWe are motivated to look for ways to extend current proven node technology to semi-permanentrnreservoir monitoring in deep water (> 500 m), where the cost and technical, logistic and HSE challengesrnfor PRM installation amongst the infrastructure of a working field are high. Installing a group ofrnautonomous nodes, which is routinely done today, is an attractive alternative to the complex integrationrnof a cabled system with existing facilities. By semi-permanent, we mean the nodes are deployed once, andrnthen multiple surveys are acquired over an extended period of time, before recovery. For this purpose, wernhave designed and built a node which has sufficient energy storage for a five year on-the-seabed lifetimernand a 300 day active recording life, enough for 12 surveys (baseline + 11 monitors) – each having arnduration of about 25 days. An enabling technology that makes the semi-permanent Life of Field (LoF)rnnode possible is a proprietary high speed underwater optical communications technology, whereby, datarndownload from the node is performed in situ on the seafloor. Nodes are deployed in "sleep" mode andrnwhen needed they are remotely switched on, "health" checked for operational readiness, synchronized with a reference time signal, and have their recording systems activated. Upon completion of the active sourcernperiod, each node is re-visited to extract the seismic data via the optical communication system and thenrnswitched off until the next monitor survey, all without handling the node, but by closely approaching thernnode with an ROV or an AUV (Autonomous Underwater Vehicle), to effect the optical link.
机译:深水海底节点(OBN)系统已经提供了高质量的全方位3D和4Drn地震数据。在本文中,我们讨论了一种新的节点技术和一种将节点用于水库监控的新方法的开发,其中,利用高速水下光通信系统从部署能力长的节点中提取数据,而无需从节点中恢复节点。海底。与基于电缆的永久性储层监测器(PRM)系统相比,这种可高度重复的半永久性4D监测功能可以以更低的成本实现。rn已经证明,通过稀疏的海底结点阵列和精确的镜头采集可以获得完整的方位角和长偏移地震数据这是一项非常成功的技术,可用于在墨西哥湾深水区的复杂盐覆盖下的3D和4D成像,在过去的十年中,该地区已进行了25多次OBN调查。在西非近海和巴西,深水OBN 3D和4D测量也已成功进行。事实证明,自主的深水OBN系统具有极高的可靠性,数据恢复率为98u0002%,并且节点通常由远程操作的车辆(ROV)进行常规部署,包括现场基础设施和同步运行。同样,对于油藏监测,OBNrnsurveys被证明具有高度可重复性,从而产生低4D噪声,NRMS统计数据通常小于rn10%,这与使用PRM系统所获得的结果相当。rn我们有动力寻找扩展当前已验证节点技术的方法到深水(> 500 m)的半永久性水库监测,在工作现场的基础设施中安装PRM的成本和技术,物流和HSE挑战都很高。安装一组自治节点(今天已常规完成),是对具有现有设施的有线系统进行复杂集成的一种有吸引力的替代方法。半永久性是指将节点部署一次,然后在恢复之前的较长时间内获取多个调查。为此,我们设计并建造了一个节点,该节点具有足够的能量存储能力,可以在五年的海底生命周期内使用,并且具有300天的有效记录寿命,足以进行12个调查(基线+ 11台监视器)–每个调查的有效期约为25天。使半永久性的“现场生命周期”(LoF)节点成为可能的一项启用技术是专有的高速水下光通信技术,其中,从节点下载数据是在海底原位进行的。节点以“睡眠”模式部署,并且在需要时可以远程打开节点,对运行状况进行“运行状况”检查,与参考时间信号同步并激活其记录系统。活动源周期结束后,将重新访问每个节点以通过光通信系统提取地震数据,然后关闭电源直到下一次监测仪测量,所有操作都无需处理该节点,而是使用ROV或AUV紧密接近该节点(自主水下航行器)以实现光链路。

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