Lozada Aguilar Miguel Ángel, Khrennikov Andrei, Oleschko Klaudia, de Jesús Correa María
Aseguramiento Tecnológico en Pemex, Exploración y Producción, Blvd. Adolfo Ruiz Cortines No. 1202, Edificio Pirámide Piso 1, Col. Fracc. Oropeza, Centro, CP 86030, Tabasco, Mexico.
International Center for Mathematical Modelling in Physics and Cognitive Sciences, Mathematical Institute, Linnaeus University, Vaxjo 351 95, Sweden
Philos Trans A Math Phys Eng Sci. 2017 Nov 13;375(2106). doi: 10.1098/rsta.2016.0398.
The paper starts with a brief review of the literature about uncertainty in geological, geophysical and petrophysical data. In particular, we present the viewpoints of experts in geophysics on the application of Bayesian inference and subjective probability. Then we present arguments that the use of classical probability theory (CP) does not match completely the structure of geophysical data. We emphasize that such data are characterized by contextuality and non-Kolmogorovness (the impossibility to use the CP model), incompleteness as well as incompatibility of some geophysical measurements. These characteristics of geophysical data are similar to the characteristics of quantum physical data. Notwithstanding all this, contextuality can be seen as a major deviation of quantum theory from classical physics. In particular, the contextual probability viewpoint is the essence of the Växjö interpretation of quantum mechanics. We propose to use quantum probability (QP) for decision-making during the characterization, modelling, exploring and management of the Quantum Bayesianism (QBism), one of the recently developed information interpretations of quantum theory, can be used as the interpretational basis for such QP decision-making in geology, geophysics and petroleum projects design and management.This article is part of the themed issue 'Second quantum revolution: foundational questions'.
本文开篇简要回顾了有关地质、地球物理和岩石物理数据不确定性的文献。特别是,我们阐述了地球物理领域专家对贝叶斯推断和主观概率应用的观点。接着,我们提出论据表明经典概率论(CP)的使用与地球物理数据的结构并不完全匹配。我们强调,此类数据具有情境性和非柯尔莫哥洛夫性(即无法使用CP模型)、不完整性以及某些地球物理测量的不相容性。地球物理数据的这些特征与量子物理数据的特征相似。尽管如此,情境性可被视为量子理论与经典物理学的主要差异。特别是,情境概率观点是韦克舍量子力学诠释的核心。我们建议在地质、地球物理以及石油项目的表征、建模、勘探和管理过程中,利用量子概率(QP)进行决策。量子贝叶斯主义(QBism)是量子理论最近发展起来的信息诠释之一,可作为地质、地球物理和石油项目设计与管理中此类QP决策的解释基础。本文是主题为“第二次量子革命:基础问题”特刊的一部分。