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Water coning mechanism in Tarim fractured sandstone gas reservoirs

机译:塔里木裂缝性砂岩气藏水锥化机理

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The problem of water coning into the Tarim fractured sandstone gas reservoirs becomes one of the major concerns in terms of productivity, increased operating costs and environmental effects. Water coning is a phenomenon caused by the imbalance between gravity and viscous forces around the completion interval. There are several controllable and uncontrollable parameters influencing this problem. In order to simulate the key parameters affecting the water coning phenomenon, a model was developed to represent a single well with an underlying aquifer using the fractured sandstone gas reservoir data of the A-Well in Dina gas fields. The parametric study was performed by varying six properties individually over a representative range. The results show that matrix permeability, well penetration (especially fracture permeability), vertical-to-horizontal permeability ratio, aquifer size and gas production rate have considerable effect on water coning in the fractured gas reservoirs. Thus, investigation of the effective parameters is necessary to understand the mechanism of water coning phenomenon. Simulation of the problem helps to optimize the conditions in which the breakthrough of water coning is delayed.
机译:就生产率,增加的运营成本和环境影响而言,进入塔里木(Tarim)裂缝性砂岩气藏的水锥问题已成为主要问题之一。水锥化是由完井时间间隔附近的重力和粘性力之间的不平衡引起的现象。有几个可控和不可控的参数会影响此问题。为了模拟影响水锥现象的关键参数,使用了迪纳气田A-Well裂缝性砂岩气藏数据,开发了一个模型来表示单井和下伏含水层。通过在代表性范围内分别改变六个属性来执行参数研究。结果表明,基质渗透率,井眼渗透率(尤其是裂缝渗透率),垂直水平渗透率,含水层大小和产气率对裂缝性气藏的水锥度有相当大的影响。因此,有必要研究有效参数以了解水锥现象的机理。问题的模拟有助于优化延迟水锥进水的条件。

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