复杂构造碳酸盐岩储层过滤、容性及含油饱和度预测(以DDB西北部为例)

O. Oliinyk, S. Vyzhva, V. Antoniuk, I. Bezrodna
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摘要

分析了国内外碳酸盐岩次生孔隙储层的研究成果。以第聂伯-顿涅茨盆地西北部South-Berestivske油田visan地层的储层岩石为例,说明了研究这类储层的综合方法。利用测井资料预测复杂碳酸盐岩储层的滤容特性和含油饱和度特征。为了解决这个问题,采用了一种综合的方法。包括孔隙度平衡方法、电测井曲线和放射性测井曲线(侧向测井-中子伽马测井、脉冲中子中子测井-中子伽马测井)的函数变换(归一化)方法。结果,作者在Visean碳酸盐岩矿床中确定了具有洞穴状空隙和裂缝的层段。每一种地球物理方法都受到空洞空间结构的影响。因此,在计算不同探针的孔隙度系数时,作者确定了以碳酸盐矿床为代表的层段,主要为多孔-洞穴型。而孔隙-洞穴-裂缝型层段为4287.6 ~ 4289.6 m。结果表明,所选地层中不同类型孔隙度系数分别为:次生孔隙度2.5 ~ 6%、海绵孔隙度1.7 ~ 5%、裂缝孔隙度0.2%。生产层厚度在0.8 ~ 2.4 m之间,平均值为2 m,并对复杂构造储层饱和系数计算参数的选择进行了论证。此外,值得注意的是,储层的性质是由次级空隙的存在提供的,即流体通过的空隙,岩石基质被压实,多孔性和低渗透性。
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Prediction of filtration and capacitive properties and oil saturation characteristics of complex structure carbonate reservoirs (on the example of the Northwestern part of DDB)
The world achievements of the study of carbonate reservoir rocks with secondary voids have been analyzed. An integrated approach to the study of this type of reservoir has been demonstrated on the example of reservoir rocks of the Visean strata of the South-Berestivske field in the North-Western part of the Dnipro-Donets Basin. The purpose of this article is to predict the reservoir filtration-capacitive properties, as well as oil saturation characte-ristics of complex carbonate reservoir rocks using well logging data. To solve this problem, an integrat-ed approach is used. It includes the methods of porosities balance and functional transformations (normalization) of the electrical and radioactive well logging curves (lateral logging - neutron gamma ray logging, impulse neu-tron-neutron logging - neutron gamma ray logging). As a result, the authors have identified intervals in the Visean carbonate deposits with cavernous voids and cracks. Each individual geophysical method is influenced by the structure of the void space. Due to this, when calculating the porosity coefficient for different probes, the au-thors identify intervals represented by carbonate deposits, mainly of the porous-cavernous type. However, there is an interval of 4287.6-4289.6 m of porous-cavernous-fractured type. It is established that in the selected layers the coefficients of different types of porosity are: secondary - 2.5-6%, cavernous - 1.7-5% and fracture -0.2%. The thickness of pro-ductive sediments varies within 0.8 - 2.4 m (the average value is 2 m). The authors also substantiated the choice of parameters when calculating the saturation coefficient in complex structural reservoirs. Moreover, it is noted that the reservoir properties are provided by the presence of secondary voids, namely the cavities through which the fluid is filtered, and the rock matrix is compacted, poor-porous and low-permeable.
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