Characterization of Type and Maturity of Organic Matter in Source Rock by In-situ Electrical Heating and Temperature Transient Analysis

K. Lee
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引用次数: 3

Abstract

Reliable estimation of organic matter characteristics is essential in drilling decisions, source rock evaluation, and unconventional reservoir production. Their measurement is based on experiments after core sampling, which is time-consuming and economically challenging. In this study, we present a new approach to evaluate the characteristics of organic matter in source and reservoir rocks by in-situ electrical heating and temperature transient analysis under in-situ conditions. The new approach is based on inverse modeling, which monitors in-situ heater temperature during electrical heating and machine learning technologies. Thermal method of electrical heating is applied for the in-situ pyrolysis, to figure out the characteristics of organic matter—kerogen volume fraction and activation energy of decomposition reaction. The heater temperature acts as an indicator of type and maturity of kerogen, since it is affected by the bulk thermal conductivity of formation, which is a function of dynamically changing rock-and-pore composition by kerogen decomposition. A full-physics simulation model of in-situ kerogen pyrolysis is used to generate output data of electrical heater temperature, which is the input data of learning-based models. Minimal simplification of physical and chemical phenomena in the full-physics simulation model, which describes the multicomponent-multiphase-nonisothermal systems involving kinetic reactions, gives the confidence of synthetic output data of heater temperature. Full-physics simulation model computes system responses under unknown and uncertain input parameters, which determine the reactivity of kerogen pyrolysis. The full-physics simulation model generates the sets of heater temperature transient data while heating with constant heat flux, in the 300 different simulated source rocks containing Types 1, 2, and 3 kerogens with various organic matter content and activation energies. Based on the set of heater temperature transient data as input parameters, Artificial Neural Network (ANN) is employed to generate a black box model to estimate the unknown organic matter content and activation energy. Developed ANN data-driven model shows better performance in estimating unknown parameters, in Types 2 and 3 kerogens with wide ranges of activation energies than Type 1 kerogen with a narrow range of activation energy. Support Vector Machines (SVM) method, which categorizes data into multiple classes by using hyperplanes, is applied to classify the heater temperature transient data into different types of kerogens and shows good performance in classification. The new characterization technology of in-situ organic matter in source rocks presented in this study provides reliable information of types and maturity of organic matter, without experiments after core sampling. It is expected to enable the realistic evaluation of source rocks under subsurface conditions, by resolving technical and economic challenges.
利用原位电加热和温度瞬态分析表征烃源岩有机质类型和成熟度
可靠的有机质特征估计对于钻井决策、烃源岩评价和非常规油藏开发至关重要。他们的测量是基于岩心取样后的实验,这既耗时又具有经济挑战性。在本研究中,我们提出了一种利用原位电加热和原位温度瞬变分析来评价烃源岩和储层有机质特征的新方法。新方法基于逆建模,该模型可以监测电加热过程中的原位加热器温度和机器学习技术。采用电加热的热法进行原位热解,求出有机质-干酪根体积分数和分解反应活化能的特征。加热器温度是干酪根类型和成熟度的标志,因为它受地层体积导热系数的影响,而体积导热系数是干酪根分解动态改变岩石和孔隙组成的函数。利用原位干酪根热解全物理模拟模型生成电加热器温度的输出数据,作为基于学习的模型的输入数据。对涉及动力学反应的多组分多相非等温系统的全物理模拟模型中的物理和化学现象进行了最小程度的简化,使加热器温度的合成输出数据具有置信度。全物理模拟模型计算了系统在未知和不确定输入参数下的响应,决定了干酪根热解的反应性。全物理模拟模型生成了300个含不同有机质含量和活化能的1、2、3型干酪根的不同模拟烃源岩在恒热流密度下加热时的加热器温度瞬态数据集。以加热器温度瞬态数据集为输入参数,利用人工神经网络(ANN)生成黑匣子模型,估算未知有机质含量和活化能。在活化能范围较宽的2型和3型干酪根中,所建立的人工神经网络数据驱动模型对未知参数的估计效果优于活化能范围较窄的1型干酪根。将支持向量机(Support Vector Machines, SVM)方法应用于超平面对数据进行多类分类,将加热器温度瞬态数据分类为不同类型的干酪根,取得了良好的分类效果。本研究提出的烃源岩原位有机质表征新技术,无需岩心取样后的实验,提供了可靠的有机质类型和成熟度信息。通过解决技术和经济挑战,有望在地下条件下对烃源岩进行现实评价。
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