基于连续损伤力学的火山岩储层天然裂缝正演模拟

Xinpu Shen
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摘要

利用连续损伤力学模型和有限元数值模拟技术,研究了火山岩储层内天然裂缝的分布,给出了表征目标层内天然裂缝分布的损伤变量等值线的数值解。提出了数值计算的工作流程。应用这些技术研究了中国西部某油田火山岩储层内构造运动形成的天然裂缝分布。采用准脆塑性损伤模型,对该地区给定的火山岩地层内技术运动产生的裂缝进行了模拟。采用初始应变法模拟构造运动引起的靶层加载,而不是采用边界位移加载。对不同的主应变分量的大小和方向进行了测试,以找出它们的合适值。通过将天然裂缝分布的数值结果与地震资料解释得到的数值结果相匹配,标定了损伤模型的参数值。主要结果表明:(1)上三叠统小泉沟组储层和下条湖组储层天然裂缝分布数值解与地震资料解释结果一致。(2)上三叠统小泉沟组损伤变量最大值为0.2678,破碎程度为26.78%。损伤定位区宽度约为10 ~ 300米。下条湖组损伤变量最大值为0.2569,略小于上小泉沟组。(3)目标区块内天然裂缝带主要分布在区块中东部。因此,计划的新井应位于该区块的这一部分。目标区块西侧天然裂缝带呈窄带状,缺乏连通,不利于新井的开发。该案例研究为火山岩储层中天然裂缝的识别提供了最佳实践。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Forward Modeling of Natural Fractures within Volcanic Reservoir by Using Continuum Damage Mechanics
By using the continuum damage mechanics’ model and finite element numerical simulation technology, this paper studies natural fractures’ distribution within volcanic reservoir and presents numerical solution of contour of damage variable which represents distribution of natural fractures within target formations. Workflow of numerical calculation was proposed. These techniques were applied to investigate natural fractures distribution generated by tectonic movement within volcanic reservoir of an oilfield in west China. Quasi-brittle plastic damage model is used to simulate fractures generated by technical movement within volcanic formations given in this region. Initial-strain-method is used to simulate loading applied to target formation caused by tectonic movement instead of using boundary displacement loading. Different values of magnitude and orientations of principal strain components have been tested in order to find their proper values. Values of parameters of damage models are calibrated by matching numerical results of natural fractures’ distribution to those obtained by interpretation of seismic data. Principal results are: (1) in the upper Triassic Xiaoquangou formation reservoir and the lower Tiaohu formation reservoir, numerical solution of natural fractures’ distribution is consistent with those obtained from interpretation of seismic data. (2) The maximum value of damage variable of the upper Triassic Xiaoquangou formation is 0.2678, i.e., the degree of crushing is 26.78%. The width of the zone of damage localization is about 10 meters to 300 meter. The maximum value of damage variable in the lower Tiaohu formation is 0.2569, which is slightly less than that in the upper Xiaoquangou formation. (3) Within the target block, zones of natural fractures are mainly distributed in central-east part of the block. Therefore the planned new wells should be located in this part of the block. Zones of natural fractures in the west part of the target block are in the shape of narrow bands which are lack of connections, and thus this west side of the block is not a good place for new wells. This case study provides a best practice for identification of natural fractures within volcanic reservoir.
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