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Heterogeneity in the Petrophysical Properties of Carbonate Reservoirs in Tal Block

机译:塔尔区块碳酸盐岩储层岩石物理性质的非均质性

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Exploring for a wide range of hydrocarbon reservoirs, including carbonate systems is increasingly important in times of higher resource demand and progressively dwindling reserves.Exploration for carbonate systems is generally more difficult than siliciclastic reservoir exploration because of intrinsic heterogeneities, which occur at all scales of observation and measurement. Heterogeneity in carbonates can be attributed to variable lithology, chemistry/mineralogy, pore types, pore connectivity, and sedimentary facies. These intrinsic complexities can be related to geological processes controlling carbonate production and deposition, and to changes during their subsequent diagenesis. The term “heterogeneity” is rarely defined and almost never numerically quantified in petrophysical analysis, although it is widely stated that carbonate heterogeneities are poorly understood.This work in carbonates of the Tal block has investigated how heterogeneity can be defined and how we can quantify this term by describing a range of statistical heterogeneity measures (e.g., Lorenz and Dykstra-Parsons coefficients). These measures can be used to interpret variation in wireline log data, allowing for comparison of their heterogeneities within individual and multiple reservoir units. Through this investigation, the Heterogeneity Log has been developed by applying these techniques to wireline log data, over set intervals of 10, 5, 2 and 1m, through a carbonate reservoir.Application to petrophysical rock characterization shows a strong relationship to underlying geological heterogeneities in carbonate facies, mud content and porosity (primary & secondary porosities) in the Tal block. Zones of heterogeneity identified through the successions show strong correlation to fluid-flow zones. By applying the same statistical measures of heterogeneity to established flow zones it is possible to rank these units in terms of their internal heterogeneity. Both increased and decreased heterogeneity are documented with high reservoir quality in different wireline measurements; this can be related to underlying geological heterogeneities. Heterogeneity Logs can be used as a visual indicator of where to focus sampling strategies to ensure intrinsic variabilities are captured.Carbonate lithology and mineralogy can be highly variable, both vertically and horizontally through a succession. Carbonate depositional environments produce a diverse range of sedimentary facies which contain different porosity types with varying degrees of connectivity, producing complex and irregular pore networks. Minerals such as calcite, aragonite, and dolomite may co-exist within a single rock unit in varying proportions. Carbonate minerals have different stabilities and are susceptible to the many post-depositional processes of diagenesis.Porosity-permeability relationships in carbonate reservoirs are notoriously poorly defined, although work by authors such as Lucia (1995; 2000) suggest correlations can be derived from pore type and grain size relationships. The ability to predict porosity and permeability relationships in carbonates continues to be an area of industry research interest. Reservoir zonation is often established using poro-perm features through complex statistical analysis, although traditional placement of flow zone boundaries comes down to visual assessment and an analyst’s experience and expectations.This study therefore focuses on developing these techniques and applying them to carbonate petrophysical and geological data including borehole image and cre data in the Tal block, which can have further application to characterizing poro-perm relationships, fluid flow zone identification and sampling strategies.
机译:在资源需求增加和储量逐渐减少的时代,勘探范围广泛的碳氢化合物储层(包括碳酸盐系统)变得越来越重要。 通常,碳酸盐岩系统的勘探比硅质碎屑岩储层的勘探更为困难,因为其固有的非均质性存在于所有观测和测量规模。碳酸盐岩的非均质性可以归因于可变的岩性,化学/矿物学,孔隙类型,孔隙连通性和沉积相。这些内在的复杂性可能与控制碳酸盐生产和沉积的地质过程有关,并且与它们随后的成岩过程中的变化有关。尽管广泛指出碳酸盐岩的非均质性知之甚少,但在岩石物理分析中,“非均质性”一词很少被定义,也几乎从未用数值来量化。 这项在Tal区块碳酸盐岩中的工作研究了如何定义异质性,以及我们如何通过描述一系列统计异质性度量(例如Lorenz和Dykstra-Parsons系数)来量化该术语。这些措施可用于解释电缆测井数据的变化,从而可以比较它们在单个储层单元和多个储层单元中的非均质性。通过这项调查,通过将这些技术应用于碳酸盐岩储层,以设定的间隔10、5、2和1m将这些技术应用于电缆测井数据,开发了非均质性测井。 在岩石物理岩石表征中的应用表明,它与塔尔区块碳酸盐岩相的潜在地质异质性,泥浆含量和孔隙度(主要和次要孔隙度)有很强的关系。通过演替确定的异质性区域显示出与流体流动区域的强相关性。通过将相同的统计异质性度量应用于已建立的流动区域,可以根据其内部异质性对这些单元进行排名。在不同的电缆测量中,非均质性的增加和减少都被记录为高储层质量。这可能与潜在的地质异质性有关。异质性日志可以用作可视化指示符,指出应将采样策略集中在何处,以确保捕获内在变化。 碳酸盐岩的岩性和矿物学在垂直和水平方向上可能相继变化很大。碳酸盐沉积环境产生各种沉积相,这些沉积相包含具有不同连通度的不同孔隙类型,产生复杂且不规则的孔隙网络。方解石,文石和白云石等矿物可以不同比例共存于单个岩石单元中。碳酸盐矿物具有不同的稳定性,易受成岩作用的许多沉积后过程的影响。 众所周知,碳酸盐岩储层的孔隙度-渗透率关系定义很差,尽管诸如Lucia(1995; 2000)等作者的工作表明,相关性可以从孔隙类型和粒度关系中得出。预测碳酸盐中的孔隙率和渗透率关系的能力仍然是工业研究领域中关注的领域。储层分区通常是通过渗透率特征通过复杂的统计分析来建立的,尽管流域边界的传统布置取决于视觉评估以及分析师的经验和期望。 因此,本研究着重于开发这些技术并将其应用于碳酸盐岩岩石物理和地质数据,包括Tal区块中的井眼图像和cre数据,这些数据可进一步用于表征孔隙-渗透层关系,流体流动带识别和采样策略。

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