凝析气藏三维成分变化

A. Kabir, Mahbub S. Ahmed, Dhaher Elew
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引用次数: 2

摘要

凝析气藏是石油和天然气行业的主要参与者。正确认识储层流体组成及其空间分布有助于确定资源基础和预测油田生产剖面。在具有较大垂直跨度的气体聚集中,预计会出现成分梯度,其中较重的分子向底端倾斜,较轻组分的浓度向塔顶增加。然而,在文献中,一些研究人员报道了凝析油含量和重烃组分随着深度和温度的增加而减少。他们的观察结果似乎与根据热力学平衡所期望的重力驱动的成分梯度相矛盾。本文对某凝析气藏进行了大面积的面向和垂向组成趋势综合分析,即三维趋势分析。绘制了油田宽面积和垂直储层硬石膏含量图。区域成分梯度违背了预期的重力驱动成分梯度,同时尊重垂直热力学平衡。沉积后流体/岩石热化学反应和低面积扩散率导致了这种面积变化。随着储层深度和温度的升高,地层中H2S生成增强,从而克服了活化能峰。根据热化学反应化学计量学,H2S浓度的增加是以碳氢化合物浓度的降低为代价的。结果表明,垂向组分梯度与热力学平衡计算结果一致。利用岩石成分和地质资料解释了一些观测到的趋势异常。因此,具有这种行为的储层的三维成分梯度被破译。本研究的目的是为凝析气田的储量、产量、采收率和成分组合提供更好的预测。
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Three Dimensional Compositional Variation in Gas Condensate Reservoirs
Gas condensate reservoirs are a major player in the oil and gas industry. Proper understanding of reservoir fluid composition and their spatial distribution helps define our resource base and forecast field production profile. In a gas accumulation with substantial vertical span, a composition gradient is expected, where heavier molecules gravitate towards the bottom end and lighter components' concentration increases towards the top of the column. However, in the literature some investigators have reported both condensate content and heavy hydrocarbon components decrease with increasing depth and temperature. Their observations appear to be contradicting the expected gravity driven compositional gradient as per thermodynamic equilibrium. In this paper, we have done an integrated areal and vertical composition trend analysis of some gas condensate reservoirs across a big area i.e. a three-dimensional trend analysis. Field wide areal and vertical reservoir anhydrite content has been mapped. The areal composition gradient that defies expected gravity driven composition gradient, while honoring vertical thermodynamic equilibrium has been reconciled. Post depositional fluid/rock thermochemical reaction and low areal diffusivity has resulted in this areal variation. In-situ H2S generation has been enhanced where reservoir deepens and temperature increases, thus overcoming the activation energy hump. H2S concentration increase has happened at the expense of the hydrocarbon concentration as per the thermochemical reaction stoichiometry. It was found that the vertical compositional gradient is consistent with thermodynamic equilibrium calculations. Some observed trend anomalies have been explained using rock composition and geological information. Thus, a three dimensional compositional gradient was deciphered for reservoirs with such behavior. The aim of this study has been to provide a better quality forecast for reserves, rate, recovery and composition mix for gas condensate fields.
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