Uncertainties in 3-D stochastic geological modeling of fictive grain size distributions in detrital systems

IF 2.6 Q2 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Alberto Albarrán-Ordás , Kai Zosseder
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引用次数: 0

Abstract

Geological 3-D models are very useful tools to predict subsurface properties. However, they are always subject to uncertainties, starting from the primary data. To ensure the reliability of the model outputs and, thus, to support the decision-making process, the incorporation and quantification of uncertainties have to be integrated into the geo-modeling strategies. Among all modeling approaches, the novel Di models method was conceived as a stochastic approach to make predictions of the 3-D lithological composition of detrital systems, based on estimating the fictive grain size distribution of the sediment mixture by using soil observations from drilled materials. Within the present study, we aim to adapt the geo-modeling framework of this method in order to incorporate uncertainties linked to systematic imprecisions in the soil observations used as input data. Following this, uncertainty quantification measures are proposed, based on entropy and joint entropy for the main outcomes of the method, i.e., the partial percentile lithological models, and for the whole sediment mixture. Both the ability of the uncertainty quantification measures and the uncertainty propagation derived from the extension of the method are investigated in the model outcomes in a simulation experiment with real data conducted in a small-scale domain located in Munich (Germany). The results show that this adaptation of the Di models method overcomes potential bias caused by ignoring imprecise input data, thus providing a more realistic assessment of uncertainty. The uncertainty measures provide very useful insight for quantifying local uncertainties, comparing between average uncertainties and for better understanding how the implementation parameters of the geo-modeling process influence the property estimation and the underlying uncertainties. The main findings of the present study have great potential for providing robust uncertainty information about model outputs, which ultimately strengthens the decision-making process for practical applications based on the implementation of the Di models method.

Abstract Image

碎屑系统有效粒度分布三维随机地质建模中的不确定性
地质三维模型是预测地下性质的非常有用的工具。然而,从原始数据开始,它们总是受到不确定性的影响。为了确保模型输出的可靠性,从而支持决策过程,必须将不确定性的纳入和量化纳入地质建模策略。在所有建模方法中,新的Di模型方法被认为是一种随机方法,用于预测碎屑系统的三维岩性组成,其基础是通过使用钻孔材料的土壤观测来估计沉积物混合物的虚拟粒度分布。在本研究中,我们旨在调整该方法的地质建模框架,以便将与系统不精确性相关的不确定性纳入用作输入数据的土壤观测中。随后,基于熵和联合熵,针对该方法的主要结果,即部分百分位岩性模型和整个沉积物混合物,提出了不确定性量化措施。在慕尼黑(德国)的一个小规模领域进行的模拟实验中,利用真实数据,在模型结果中研究了不确定性量化测量的能力和由该方法扩展得出的不确定性传播。结果表明,Di模型方法的这种适应性克服了由于忽略不精确的输入数据而引起的潜在偏差,从而提供了更现实的不确定性评估。不确定性度量为量化局部不确定性、比较平均不确定性以及更好地理解地质建模过程的实施参数如何影响财产估计和潜在不确定性提供了非常有用的见解。本研究的主要发现在提供关于模型输出的稳健不确定性信息方面具有巨大潜力,这最终加强了基于Di模型方法的实际应用决策过程。
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来源期刊
Applied Computing and Geosciences
Applied Computing and Geosciences Computer Science-General Computer Science
CiteScore
5.50
自引率
0.00%
发文量
23
审稿时长
5 weeks
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