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通过跨维度采样探索数据空间:以四维地震为例

Exploration of Data Space Through Trans-Dimensional Sampling: A Case Study of 4D Seismics.

作者信息

Piana Agostinetti Nicola, Kotsi Maria, Malcolm Alison

机构信息

ZED Depth Exploration Data GmbH Vienna Austria.

PanGeo Subsea Inc. St John's NL Canada.

出版信息

J Geophys Res Solid Earth. 2021 Dec;126(12):e2021JB022343. doi: 10.1029/2021JB022343. Epub 2021 Nov 26.

Abstract

We present a novel methodology for exploring 4D seismic data in the context of monitoring subsurface resources. Data-space exploration is a key activity in scientific research, but it has long been overlooked in favor of model-space investigations. Our methodology performs a data-space exploration that aims to define structures in the covariance matrix of the observational errors. It is based on Bayesian inferences, where the posterior probability distribution is reconstructed through trans-dimensional (trans-D) Markov chain Monte Carlo sampling. The trans-D approach applied to data-structures (termed "partitions") of the covariance matrix allows the number of partitions to freely vary in a fixed range during the McMC sampling. Due to the trans-D approach, our methodology retrieves data-structures that are fully data-driven and not imposed by the user. We applied our methodology to 4D seismic data, generally used to extract information about the variations in the subsurface. In our study, we make use of real data that we collected in the laboratory, which allows us to simulate different acquisition geometries and different reservoir conditions. Our approach is able to define and discriminate different sources of noise in 4D seismic data, enabling a data-driven evaluation of the quality (so-called "repeatability") of the 4D seismic survey. We find that: (a) trans-D sampling can be effective in defining data-driven data-space structures; (b) our methodology can be used to discriminate between different families of data-structures created from different noise sources. Coupling our methodology to standard model-space investigations, we can validate physical hypothesis on the monitored geo-resources.

摘要

我们提出了一种在监测地下资源背景下探索四维地震数据的新方法。数据空间探索是科学研究中的一项关键活动,但长期以来一直被忽视,人们更倾向于模型空间研究。我们的方法进行数据空间探索,旨在定义观测误差协方差矩阵中的结构。它基于贝叶斯推断,通过跨维(trans-D)马尔可夫链蒙特卡罗采样来重建后验概率分布。应用于协方差矩阵数据结构(称为“分区”)的跨维方法允许在蒙特卡罗采样期间分区数量在固定范围内自由变化。由于采用了跨维方法,我们的方法检索到的是完全由数据驱动而非用户强加的数据结构。我们将我们的方法应用于通常用于提取地下变化信息的四维地震数据。在我们的研究中,我们利用在实验室收集的真实数据,这使我们能够模拟不同的采集几何形状和不同的储层条件。我们的方法能够定义和区分四维地震数据中的不同噪声源,从而对四维地震勘探的质量(所谓的“重复性”)进行数据驱动的评估。我们发现:(a)跨维采样在定义由数据驱动的数据空间结构方面可能是有效的;(b)我们的方法可用于区分由不同噪声源产生的不同数据结构族。将我们的方法与标准模型空间研究相结合,我们可以验证关于被监测地质资源的物理假设。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ba3d/9287047/92e7f234e1c0/JGRB-126-0-g009.jpg

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