开阔砂质储层体系次生高岭石分布的多态性

IF 0.6 Q4 ENGINEERING, GEOLOGICAL
Igor A. Melnik
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引用次数: 0

摘要

引用链接:Melnik I.A.。开放砂质储层体系中次生高岭石分布的多模态。托木斯克理工大学公报。岩土工程Аssets, 2023,第334卷,第2期。8日,рр。17 - 29日。在Rus.Relevance。根据开放系统变换结果对所调查环境的登记特征的分布形式进行的大量研究表明,在系统受到外部影响的情况下,变换元素的强度和含量具有统计分布的多模态形式。显然,系统变换的统计多态现象的本质具有普适性。因此,多模态分布地层的通用理论可用于分析开放体系的渗透砂岩储层中次生矿物含量的样品。显然,变换后的元的多模态统计分布的每一个模态都是某个吸引子表现的结果。本文的目的是提出一种普遍的运动学理论,用于解释开放体系中由于砂质储层叠加后成作用而形成的次生粘土矿物高岭石的多模态统计分布的形成。研究对象为亚马尔半岛油气田砂层次生高岭石化强度值样品和斯托尔博沃油气田上侏罗统砂层次生高岭石含量(岩心测定)样品。次生高岭石化是由深部流体的影响引起的。根据得到的变换单元数多模态分布的统一模态方程确定了研究方法。转换元素的数量(强度)与系统转换时间与外部影响系统元素的流动时间之比成正比。从理论上计算了与“黄金”比例有关的七个基本常数(吸引子),使它们符合系统转换过程状态的普遍原则。结果。通过将理论得到的常数与经验数据模态的计算统一值进行比较,确定了系统变换过程相对于每个模态的状态。对二次高岭石强度和高岭石含量多模态分布计算的模态进行了分析,并将模态值(相应的变换原理)与变换过程的经验数据进行了比较,证明了通用运动学理论的有效性。结论。因此,利用普遍的转化原理,根据在研究的渗透层段中确定的次生高岭石的含量,可以分配具有感兴趣的化学和水动力性质和特征的区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
POLYMODALITY OF SECONDARY KAOLINITE DISTRIBUTION IN OPEN SANDY RESERVOIR SYSTEMS
Link for citation: Melnik I.A. Polymodality of secondary kaolinite distribution in open sandy reservoir systems. Bulletin of the Tomsk Polytechnic University. Geo Аssets Engineering, 2023, vol. 334, no. 8, рр. 17-29. In Rus. Relevance. Numerous studies of the forms of distributions of the registered characteristics of the investigated environment according to the results of transformation of open systems have shown that the intensities and contents of transformed elements have a polymodal form of statistical distribution in the case of external impact on the system. Apparently, the essence of the phenomenon of statistical polymodality of transformation of systems is universal. Therefore, the universal theory of polymodal distribution formation can be used to analyze samples of secondary mineral contents in permeable sand reservoirs, which are open systems. Obviously, each mode of the polymodal statistical distribution of the transformed elements will be the result of the manifestation of some attractor. The purpose of this paper is to present a universal kinematic theory of the formation of a polymodal statistical distribution of the number of transformed elements of an open system, where secondary clay minerals – kaolinites, due to superimposed epigenesis in a sandy reservoir are considered as the formed elements. The objects of the study are samples of secondary kaolinitization intensity values in sand intervals of oil and gas fields of the Yamal Peninsula and the contents of secondary kaolinite (determined from the core) in Upper Jurassic sand strata of the Stolbovoe oil and gas field. Secondary kaoliniteization is caused by the influence of deep fluids. The research method was determined on the basis of the obtained equation of unified modes of polymodal distribution of the number of transforming elements (in transformation of systems). The number (intensity) of transformed elements is proportional to the ratio of the system transformation time to the flow time of the external influence on the elements of this system. Seven basic constants (attractors) related to the «golden» proportion were theoretically calculated, bringing them into conformity with universal principles of system transformation processes states. Results. Having compared constants obtained theoretically with calculated unified values of modes of empirical data, the states of system transformation processes with respect to each mode have been determined. Analysis of modes calculated in a polymodal distribution of secondary kaolinite intensities and kaolinite content, as well as comparing mode values (with corresponding transformation principle) with empirical data on transformation processes gave evidence for the validity of the universal kinematic theory. Conclusions. Thus, using universal principles of transformation, on the basis of the determined contents of secondary kaolinite in the studied intervals of permeable strata, it is possible to allocate zones with the chemical and hydrodynamic properties and characteristics of interest.
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1.40
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50.00%
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