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Multiple Scenario Generation of Subsurface Models:Consistent Integration of Information from Geophysical and Geological Data throuh Combination of Probabilistic Inverse Problem Theory and Geostatistics

机译:地下模型的多场景生成:概率反问题理论与地统计学相结合的地球物理和地质数据信息的一致整合

摘要

In geosciences, as well as in astrophysics, direct observations of a studied physical system and objects are not always accessible. Instead, indirect observations have to be used in order to obtain information about the unknown system, which leads to an inverse problem. Such geoscientific inverse problems face the challenge of determining a set of unknown model parameters based on a set of indirect observations of the subsurface. In a traditional least-squares formulation of the solution to an inverse problem, a subjectively chosen regularization parameter is used to obtain a unique solution to this problem, which leads to a smooth solution with no geological realism. Moreover, such a optimization-based framework does not allow introducing realistic geological prior information (due to a vectorial normed space structure). This thesis focuses on a more sophisticated approach based on a probabilistic formulation of the solution to the inverse problem. In this formulation, different sources of information about the subsurface can be weighted with regard to their relative quality and reliability (i.e., uncertainties) using probability distributions and subsequently integrated intoa posterior probability distribution over the model parameters. The different sources of information are provided in form of a set of observed data, uncertainties related to the data, and geological prior information, which is established from, e.g., expert knowledge and old data sets. The prior information, when being informative and realistic, has a regulating effect on the solution to the inverse problem as geological and geophysical information are orthogonal in some ways, which allows reducing the underdetermination of the inverse problem. At the same time, such prior information also reduces the effective dimension of the inverse problem, which may considerably reduce the computationally cost related to such problems. Moreover, the probabilistic formulation of the inverse problem allows the use of geologically more realistic prior information that leads to solutions to the inverse problem with a higher degree of geological realism. Finally, the probabilistic formulation provides a means of analyzing uncertainties and potential multiple-scenario solutions to be used for risk assessments in relation to, e.g., reservoir characterization and forecasting. Prior models rely on information from old data sets or expert knowledge in form of, e.g., training images that expresses structural, lithological, or textural features. Statistics obtained from these types of observations will be referred to as sample models. Geostatistical sampling algorithms use a sample model as input and produce multiple realizations of the model parameters that, to some degree, honor this information. Such algorithms can be used to define the prior information for probabilistic inverse problems. In this way, very informative and geologically more realistic prior information can be provided. This thesis provides an overview of the scientific developments within the fields of probabilistic inverse problem theory and geostatistics, with emphasis on the combination of these scientific disciplines. In particular, the focus will be on consistent probabilistic formulations of this problem, which means that a correct weighting of the different sources of information is obeyed such that no unknown assumptions and biases influence the solution to the inverse problem. This involves a definition of the probabilistically formulated inverse problem, a discussion about how prior models can be established based on statistical information from sample models, and an analysis of geostatistical algorithms in order to understand the implicit assumptions made by such “black box” algorithms. A description of the posterior distribution can be obtained by drawing a representative sample from this distribution. Methodologies to be used for this purpose are presented. An example of sampling the posterior probability distribution of a computationally hard full waveform inverse problem using prior information based on multiple-point statistics, obtained from a training image, is demonstrated. For some computationally challenging inverse problems, a sample from the posterior distribution might still be too laborious to be obtained. Instead, a set of model parameters with (near) maximum posterior probability can be obtained. In order to do this, a closed form mathematical formulation of the prior probability distribution has to be established, such that the posterior probability distribution can be evaluated. Different solutions to this problem are presented and discussed. The prior probability distribution that is sampled by geostatistical sampling algorithms is typically unknown or sometime only a part of or an approximation to the distribution is known. This thesis provides an analysis and a discussion of how these prior probability distributions can be established, such that it is consistent with information provided by a known sample model. It is described how assumptions about the distribution, in addition to the information provided by the sample model, have to be made in order to end up with a unique solution to this problem. It is shown that these sampling algorithms typically provide samples from a prior probability distribution that is not consistent with the sample model. However, examples of consistent algorithms are also provided. A likelihood function is part of the probabilistic formulation of the inverse problem. This function is based on an uncertainty model that describes the uncertainties related to the observed data. In a similar way, a formulation of the prior probability distribution that takes into account uncertainties related to the sample model statistics is formulated. Prior models that are consistent with the statistics from a training image do not necessarily produce realizations with the same spatial patterns as seen in the training image because the local Markov properties that is satisfied in this way does not lead to a global reproduction of the pattern distribution from the training image. A prior probability distribution, with realizations that resemble the patterns as seen in the training image, is described and an efficient sampling algorithm that samples this distribution is provided. Moreover, an example of using this prior model for an inverse problem is demonstrated. The theoretical forward problem that describes the relation between data and model parameters is often associated with some degree of approximation. This approximation may have a great impact on the solution to the inverse problem because such approximatecalculations of the data have an impact similar to observation uncertainties. We refer to the effect of these approximations as modeling errors. Examples that show how the modeling error is estimated are provided. Moreover, it is shown how these effects can be taken into account in the formulation of the posterior probability distribution. Common to the methods and strategies presented in this thesis is that they strive for a solution to the inverse problem that is consistent with the available information and to a less degree based on unconscious or subjective choices and implicit assumptions. Future studies related to theoretical developments of these strategies have to be provided. Moreover, applications of these strategies will reveal the practical implications of these consistent formulations. This will in particular be of great importance when it comes to assessments related cases of high risk such as human health or resources of high economical potentials.
机译:在地球科学和天体物理学中,对被研究的物理系统和物体的直接观测并不总是可访问的。相反,必须使用间接观测来获得有关未知系统的信息,这会导致反问题。这样的地球科学反问题面临着基于对地下的间接观测来确定一组未知模型参数的挑战。在反问题的解决方案的传统最小二乘公式中,使用主观选择的正则化参数来获得该问题的唯一解,这导致没有地质现实性的平滑解。而且,这种基于优化的框架不允许引入现实的地质先验信息(由于矢量规范的空间结构)。本文着重于基于反问题解决方案的概率表述的更复杂的方法。在这种表述中,关于地下的信息的不同来源可以使用概率分布对其相对质量和可靠性(即不确定性)进行加权,然后整合到模型参数上的后验概率分布中。以一组观测数据,与数据有关的不确定性以及地质先验信息的形式提供不同的信息源,这些信息是从例如专家知识和旧数据集中建立的。当地质信息和地球物理信息以某种方式正交时,先验信息在提供信息和现实时,会对反问题的解决产生调节作用,这可以减少反问题的不确定性。同时,这种先验信息还减小了反问题的有效维度,这可以大大减少与此类问题相关的计算成本。此外,反问题的概率表述允许使用地质上更现实的先验信息,从而导致以更高的地质现实主义程度解决反问题。最后,概率公式提供了一种分析不确定性和潜在多方案解决方案的方法,这些方案可用于与例如储层表征和预测有关的风险评估。现有模型依赖于来自旧数据集的信息或专家知识,例如以表示结构,岩性或纹理特征的训练图像的形式。从这些类型的观察中获得的统计信息将被称为样本模型。地统计采样算法将样本模型用作输入,并产生模型参数的多种实现,这些实现在某种程度上尊重了此信息。此类算法可用于定义概率反问题的先验信息。以这种方式,可以提供非常有用且地质上更现实的先验信息。本文概述了概率反问题理论和地统计学领域内的科学发展,重点是这些学科的结合。特别地,重点将放在该问题的一致概率表述上,这意味着要服从不同信息源的正确加权,这样就不会有未知的假设和偏见影响反问题的解决方案。这涉及到概率公式化的反问题的定义,关于如何基于样本模型的统计信息如何建立先验模型的讨论,以及对地统计学算法的分析,以便理解此类“黑匣子”算法所做的隐含假设。后验分布的描述可以通过从该分布中抽取代表性样本来获得。提出了用于此目的的方法。说明了一个示例,该示例使用从训练图像中获取的基于多点统计的先验信息对计算困难的全波形逆问题的后验概率分布进行采样。对于某些计算上具有挑战性的反问题,来自后验分布的样本可能仍然太费力而无法获得。相反,可以获得具有(接近)最大后验概率的一组模型参数。为此,必须建立先验概率分布的封闭形式数学公式,以便可以评估后验概率分布。提出并讨论了该问题的不同解决方案。通常,由地统计采样算法采样的先验概率分布是未知的,或者有时只知道该分布的一部分或近似值。本文对如何建立这些先验概率分布进行了分析和讨论。,以便与已知样本模型提供的信息一致。描述了除了样本模型提供的信息之外,还必须对分布进行假设,以最终解决该问题。结果表明,这些采样算法通常从与样本模型不一致的先验概率分布中提供样本。但是,还提供了一致算法的示例。似然函数是反问题概率公式的一部分。此功能基于不确定性模型,该模型描述了与观测数据相关的不确定性。以类似的方式,制定了考虑与样本模型统计相关的不确定性的先验概率分布。与训练图像中的统计数据一致的现有模型不一定会产生与训练图像中所见具有相同空间模式的实现,因为以此方式满足的局部马尔可夫特性不会导致模式分布的全局再现从训练图像。描述了一种先验概率分布,其实现类似于在训练图像中看到的模式,并提供了对这种分布进行采样的有效采样算法。此外,还说明了使用该现有模型求解反问题的示例。描述数据与模型参数之间关系的理论正向问题通常与某种程度的近似有关。这种近似可能会对反问题的解决方案产生重大影响,因为数据的这种近似计算具有类似于观测不确定性的影响。我们将这些近似的影响称为建模误差。提供了显示如何估计建模误差的示例。此外,显示了在后验概率分布的公式化中如何考虑这些影响。本文提出的方法和策略的共同点是,他们努力寻求一种解决方案,该方案应基于无意识或主观选择和隐含假设,以与现有信息一致的方式解决反问题。必须提供与这些策略的理论发展有关的未来研究。此外,这些策略的应用将揭示这些一致的配方的实际含义。在评估与人类健康或具有高经济潜力的资源等高风险相关案例时,这一点尤其重要。

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