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The Cavendish Field Development, Block 43/19a, UKCS Southern North Sea

机译:卡文迪什油田开发公司,UKCS南北海43 / 19a区块

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The Cavendish Field is located in UKCS Southern North Sea block 43/19a on the Northern margin of the Outer Silverpit Basin some 160 km NE of the Lincolnshire coast. The field was discovered in 1989 by Britoil exploration well 43/19-1 which tested gas from two sandstone intervals within the Namurian (Upper Carboniferous) at rates of 33 and 15 MMSCFD. The field was appraised in 1991 by BP well 43/19-2A which tested gas from Westphalian A sandstones (Upper Carboniferous) at 17 MMSCFD. An additional appraisal well drilled by Amoco (43/19a-4z) in 1996 was located downdip on the NW flank but failed to encounter hydrocarbons and effectively delimits the field. The field is named after the eminent English scientist Henry Cavendish (1731-1810) who was renowned for his experiments on separating gasses from water. The Cavendish structure is a SW dipping rotated fault block bounded to the NE by an inverted extensional fault. The structure is dip closed to the South, West and East and sealed by a combination of an intra Westphalian shale seal and the shales and evaporites of the Permian Silverpit Formation. The effective reservoir consists of NNE-SSW oriented fluvial and distributary channel sandstones of the Millstone Grit (Namurian) and Caister Coal Formations (Westphalian A). The estimated gas-in-place ranges from a minimum of 166 bcf to a maximum of 403 bcf with a most likely case of 311 bcf. Key uncertainties on gas-in-place are definition and distribution of effective reservoir sands and the position of the GWC. Based on numerous stochastic simulation models, a three well development is estimated to recover a most likely case 117 bcf of sales gas with a minimum of 85 bcf and a maximum of 181 bcf over a 10 year production life. Key uncertainties on gas recovery are GIIP, well type, the number of wells and their location(s), fault transmissibility and net sand distribution. Cavendish will be developed by three high angle development wells drilled through a six slot minimum facility, Normally Unattended Installation (NUI), located in 18m of water on the environmentally sensitive Dogger Bank. Production is planned to be routed through a subsea gas cooler and a new 47 km 10” pipeline for gas processing and export via the ConocoPhillips operated CMS host facilities (Murdoch D). Gas will then be exported to the ConocoPhillips Theddlethorpe terminal for blending and onward transmission into the NTS. The Cavendish project will be RWE Dea's first UKCS operated development and could provide a suitable offtake route for additional reserves proven up in the subsequent near field exploration programme. RWE Dea received Secretary of State approval in August 2005 with first gas expected in the second quarter of 2007. RWE Dea hold a 50% WI in the project with the other 50% held by Dana Petroleum plc.
机译:卡文迪许油田位于UKCS南北海43 / 19a区块,位于外银坑盆地北缘,距林肯郡海岸东北约160公里。该油田是由Britoil勘探井43 / 19-1于1989年发现的,该井在Namurian(石炭纪上层)两个砂岩层段以33 MMSCFD和15 MMSCFD的速率测试了天然气。 1991年,该油井由BP井43 / 19-2A进行了评估,该井在17 MMSCFD处测试了来自威斯特伐利亚A砂岩(石炭纪上层)的天然气。阿莫科公司(Amoco)(43 / 19a-4z)在1996年又钻了一口评价井,位于西北侧,但未遇到烃类,因而有效地划定了油田的边界。该领域以著名的英国科学家亨利·卡文迪许(Henry Cavendish(1731-1810))的名字命名,他以将气体与水分离的实验而闻名。卡文迪许结构是一个SW倾转的旋转断层块,由反向伸展断层与NE相连。该结构向南,西和东倾斜关闭,并通过威斯特伐利亚内部页岩密封和二叠纪Silverpit组的页岩和蒸发岩的组合来密封。有效储层由取向为NNE-SSW的河床和分流河道砂岩组成,分别为磨石砾石(Namurian)和凯斯特煤层(Westphalian A)。估计的就地气体范围从最小166 bcf到最大403 bcf,最可能的情况是311 bcf。现场天然气的主要不确定性是有效储层砂的定义和分布以及GWC的位置。基于众多的随机模拟模型,估计三口井的开发将在10年的生产寿命中以最少量的85 bcf和最大的181 bcf的回收率回收117 bcf的销售气体。天然气采收率的主要不确定性是GIIP,井的类型,井的数量及其位置,断层传输率和净砂分布。卡文迪许将通过三个高角度开发井进行开发,这些井将钻探到至少六个槽的设施(通常为无人值守安装(NUI)),该设施位于对环境敏感的Dogger银行18m水深处。计划通过海底气体冷却器和一条新的47 km 10“管道输送生产,以通过ConocoPhillips经营的CMS主机设施(默多克D)进行天然气加工和出口。然后,天然气将被出口到ConocoPhillips Theddlethorpe终端,以进行混合并进一步传输到NTS中。卡文迪许项目将是RWE Dea在UKCS运营的首个开发项目,并可能为随后的近场勘探计划中探明的额外储量提供一条合适的承购路线。 RWE Dea于2005年8月获得国务卿批准,预计第一批天然气将于2007年第二季度投入使用。RWEDea持有该项目50%的WI,其余50%由Dana Petroleum plc持有。

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