岩石裂隙网络的多点统计模拟是水文地质和盐度的关键控制——以伊朗西阿扎拜詹省卡拉巴格地区为例

Desert Pub Date : 2020-12-01 DOI:10.22059/JDESERT.2020.79255
M. Mohammadi, E. R. Khojasteh, M. Faridazad
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引用次数: 5

摘要

岩石构造网络(RFN)的几何形状和分布的建模和表征在水文地质或环境评估等应用中至关重要。人们普遍认为,RFN可能与周围环境的水文地质(因此盐度)特征有关。尽管RFN的复杂性和不可访问性,但随机方法提供了一个函数框架来预测其在地下的特征。RFN建模的一个有效工具是离散裂缝网络(DFN),它还包括许多考虑空间变异结构的地质统计学技术。这些技术的优点是:逼真的结果,易于应用,以及不确定性评估。多点地质统计学(MPS)是一种用于真实模拟RFN的现代有效的地质统计学工具。在本研究中,我们对Urmia湖西部Qarabagh地区附近的RFN进行了建模;在这方面,我们使用了MPS地质统计学方法的单正态方程模拟(SNESIM)算法,使用了训练图像(TI)而不是变差函数。该建模所需的数据集和信息是使用裂缝方向和倾角的现场测量以及露头照片提供的。这些模型的结果可用于预测周围地区的盐度分布。因此,通过SNESIM算法、从露头照片中获得的TI和直接测量,在每个站生成了100个RFN实现。然后对这些实现进行平均,以预测具有较高和较低断裂概率的位置,并评估断裂分布的总体趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multiple-Point Statistical Simulation of rock fracture network as a key control on the hydrogeology and salinity: a case study from the Qarabagh area, West Azarbayjan Province, Iran
Modeling and characterization of the geometry and distribution of Rock Facture Networks (RFNs) are essential in applications such as hydrogeological or environmental evaluations. It is widely accepted that RFNs are potentially associated with the hydrogeological (thus salinity) characteristics of the surrounding environments. Despite the complexity and inaccessibility of RFNs, stochastic methods provide a functional framework to predict their characteristics in the subsurface. An efficient tool for modeling RFNs is the Discrete Fracture Network (DFN) which also includes a number of geostatistical techniques that consider spatial variability structure. The advantages of these techniques are: realistic results, ease of application, and uncertainty assessments. Multiple-point geostatistics/statistics (MPS) is a modern and effective geostatistical tool for realistically simulating RFNs. In the present study, we modeled the RFNs in a location near the Qarabagh area, in the western Urmia Lake; in this regard, we used the Single Normal Equation Simulation (SNESIM) algorithm of the MPS geostatistical method using Training Images (TIs) instead of variograms. The required datasets and information for this modeling was provided using the field measurements of the fracture orientations and dips, as well as the outcrop photographs. The outcomes of these models can be used in predicting the salinity distribution in the surrounding area . Therefore, through the SNESIM algorithm, TIs obtained from the outcrop photographs, and direct measurements, 100 RFN realizations were generated at each station. These realizations were then averaged to predict the locations with higher and lower fracture probabilities and to assess the general trend of the fracture distributions.
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