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Common Misinterpretations of Gas Condensate Reservoirs

机译:气体凝结水库的常见误解

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Geopressured gas reservoirs materialize as a result of a variety of factors, some of which include the rapid compaction of sand/shale sequences and the uplift of sediment layers by a salt intrusion. These gas reservoirs are commonly characterized by a significant drop in formation compressibility owing to the collapse of the rock matrix, and are notorious in the drilling and production industries for the various problems they cause. This paper reviews the retrograde gas condensate production data presented in SPE-2938 (Duggan, 1972) with modern analysis tools to show that gas condensate banking can cause classic material balance analysis to mimic the shape of a geopressured gas reservoir. The condensation of liquid hydrocarbons below the dew-point in a gas reservoir, and the onset of water influx from a leaky fault can complicate the material balance analysis of these reservoirs and may lead to engineers mistakenly classifying them for what they are not. Failure to properly classify a gas reservoir may lead to an incorrect estimation of original gas in place (OGIP). Accurate determination of initial gas in place is of utmost importance in the process of estimating gas reserves. A lower estimation of OGIP or not accounting for condensate banking in low permeability zones may lead to early abandonment of a gas well or significant loss of reserves for an operating company. Results show that proper consideration of the two-phase Z-factor in the material balance calculations calculated via the constant volume depletion test (CVD) leads to a more accurate determination of gas reserves, in addition, the change in formation compressibility is shown to be consolidated sandstone as opposed to geopressured rock matrix. This paper aims to demonstrate a simplified procedure for the flow-after-flow well test of determining the effect of condensate drop- out within the vicinity of the wellbore as the flowing bottom-hole pressure (BHP) drops below the dew-point pressure. Two-phase pseudo pressure was calculated from a constant composition expansion (CCE) using Whitson’s Method (Whitson, 1983) for condensate banking and measured gas composition. The classical Anderson “L” gas reservoir of the Mobil-David field in South Texas (Duggan, 1972) was chosen as a case study. Implementation of the proposed procedure will serve as an aid to gas reservoir engineers in properly classifying potential gas condensate reservoirs.
机译:地理储气储层因各种因素而言,其中一些因素包括砂/页岩序列的快速压实,并通过盐侵入沉积层的隆起。这些气体储层通常是由于岩石矩阵的崩溃而显着的形成压缩性,并且在钻井和生产行业中是臭名昭着的它们导致的各种问题。本文综述了SPE-2938(Duggan,1972)中介绍的逆行气体冷凝水生产数据,具有现代分析工具,以表明气体冷凝水库可能导致经典的材料平衡分析模仿地理储气储层的形状。液体储层中露点下方的液体烃的缩合,以及泄漏过滤的水涌入的发作可以使这些水库的材料平衡分析复杂化,可能导致工程师错误地将它们分类为他们而不是。未正确分类气体储层可能导致原始气体的估计不正确(OGIP)。在估算天然气储备过程中,准确确定初始气体的最大程度至关重要。较低估计OGIP或未核算低渗透区的冷凝银行可能会导致早期放弃运营公司的气体井或大量储备损失。结果表明,通过恒定体积耗尽试验(CVD)计算的材料平衡计算中的两相Z因子的适当考虑导致气体储备的更准确测定,此外,形成压缩性的变化显示为合并砂岩与地形岩石矩阵相反。本文旨在证明一种简化的过程,用于在井筒的附近确定冷凝水滴的效果的流动性井的简化程序,因为流动的底部孔压力(BHP)下降低于露点压力。使用WHITSON的方法(WHITSON,1983)来计算两相伪压力,用于冷凝器银行和测量的气体组合物。选择了南德克萨斯州南部(Duggan,1972年)的Mobil-David领域的古典安德森“L”气体藏作为案例研究。拟议程序的实施将有助于燃气储层工程师适当分类潜在的气体冷凝水库。

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