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Analyzing Geomechanical Effects While Drilling Sub Salt Wells Through Numerical Modeling

机译:通过数值模拟分析钻井盐井井的地质力学效应

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Santos Basin is one of the most promising basins of Brazil, recently it was discovered light crude oil of 30o API (American Petroleum Institute), this reservoir of high productivity is located below a salt layer of two thousand meters (6561,7 ft) of thickness. Salt also known as an evaporite rock is found in many hydrocarbon basins around the world. Evaporites are sediments formed initially from minerals dissolved in water, the most common are: halite, gypsum, and anhydrite. These minerals are found in areas that passed by a geological time of high evaporation or precipitation. Evaporites in general have the structure of a dome, formed when a thick layer of salt found in the bottom begins to crossover superior layers vertically;this process takes millions of years. The presence of saline structures takes into favorable conditions for creating a trap for hydrocarbons, increasing the success of probability in oil and gas exploration. In salt drilling the main problem is the closing of the well or known as squeeze or salt pinch, this phenomenon provokes the imprisonment of the drillstring also known as stuck pipe. Evaporite rock behavior is defined through a creep model. The creep model is the term used in the bibliography to define the tendency that a material has to move or to deform permanently to relieve stresses. Strains take place due to extended levels of stress;this stress is less than the rupture stress. In this matter it was chosen a numeric tool to simulate the behavior of salt drilling and the effects that this will have due to the overburden stress and drilling fluid pressure. This tool is a commercial program of finite elements in 3D (three dimensions). The objective of this work is to determine the effect of the fluency (creep) in salt during and after the drilling of the well, through numeric simulation. At first it is shown a validation of the commercial finite element program comparing results from literature and then it is shown a simulation of a 3D vertical salt wellbore.
机译:桑托斯盆地是巴西最有前途的盆地之一,最近它被发现的300 API(美国石油研究所)的浅质量原油,这个高生产率的水库位于两千米(6561,7英尺)的盐层下方厚度。在世界各地的许多碳氢化合物盆地中发现了盐也被称为蒸发岩。蒸发素是最初从溶解在水中的矿物质形成的沉积物,最常见的是:宿猪,石膏和空水石。这些矿物质在通过高蒸发或降水的地质时间通过的区域中找到。蒸发晶体通常具有圆顶的结构,当底部发现的厚层盐层开始垂直交叉上层时;这个过程需要数百万年。盐水结构的存在对碳氢化合物产生疏水阀的有利条件,增加了石油和天然气勘探概率的成功。在盐钻的主要问题是井或称为挤压或盐捏的闭合,这种现象引起了钻石的监禁,尚称为卡住管。蒸发岩行为通过蠕变模型定义。蠕变模型是参考书目中使用的术语,以限定材料必须移动或永久地变形以释放应力的趋势。由于延长的应力水平而发生菌株;这种应力小于破裂应力。在此问题中,选择了一个数字工具来模拟盐钻孔的行为以及由于覆盖压力和钻孔流体压力而导致的效果。该工具是3D中有限元的商业程序(三维)。这项工作的目的是通过数值模拟来确定钻井过程中流畅性(蠕变)在盐期间和之后的影响。首先,示出了商业有限元计划的验证比较文献结果,然后显示了3D垂直盐井筒的模拟。

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