ENTROPY AND SPATIAL DISORDER

被引:116
作者
JOURNEL, AG
DEUTSCH, CV
机构
[1] Department of Applied Earth Sciences, Stanford University, Stanford, 94305, California
来源
MATHEMATICAL GEOLOGY | 1993年 / 25卷 / 03期
关键词
SPATIAL ENTROPY; GAUSSIAN MODEL; SIMULATION; FLUID FLOW;
D O I
10.1007/BF00901422
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The majority of geostatistical estimation and simulation algorithms rely on a covariance mode as the sole characteristic of the spatial distribution of the attribute under study. The limitation to a single covariance implicitly calls for a multivariate Gaussian model for either the attribute itself or for its normal scores transform. The Gaussian model could be justified on the basis that it is both analytically simple and it is a maximum entropy model, i.e., a model that minimizes unwarranted structural properties. As a consequence, the Gaussian model also maximizes spatial disorder (beyond the imposed covariance) which can cause flow simulation results performed on multiple stochastic images to be very similar; thus, the space of response uncertainty could be too narrow entailing a misleading sense of safety. The ability of the sole covariance to adequately describe spatial distributions for flow studies, and the assumption that maximum spatial disorder amounts to either no additional information or a safe prior hypothesis are questioned. This paper attempts to clarify the link between entropy and spatial disorder and to provide, through a detailed case study, an appreciation for the impact of entropy of prior random function models on the resulting response distributions.
引用
收藏
页码:329 / 355
页数:27
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