2013
DOI: 10.1007/s11004-013-9502-1
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Using Multiple-Point Geostatistics for Tracer Test Modeling in a Clay-Drape Environment with Spatially Variable Conductivity and Sorption Coefficient

Abstract: This study investigates the effect of fine-scale clay drapes on tracer transport. A tracer test was performed in a sandbar deposit consisting of cross-bedded sandy units intercalated with many fine-scale clay drapes. The heterogeneous spatial distribution of the clay drapes causes a spatially variable hydraulic conductivity and sorption coefficient. A fluorescent tracer (sodium naphthionate) was injected in two injection wells and ground water was sampled and analyzed from five pumping wells. To determine (1) … Show more

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Cited by 12 publications
(8 citation statements)
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“…Similar algorithms include GROWTHSIM which introduces a random‐neighbor path [ Eskandari and Srinivasan , ] or HOSIM which uses spatial cumulants for pattern extraction [ Mustapha and Dimitrakopoulos , ]. Although training‐image based methods have been used in many hydrogeological applications [ Hermans et al ., ; Hu and Chugunova , ; Huysmans et al ., ; Mahmud et al ., ; Michael et al ., ], they suffer from limitations inherent to the simulation algorithms. Some important points that limit the applicability of these methods are a high computational cost, the difficulty to reproduce certain types of patterns, and most importantly the limited variability that can be recovered from a finite size training image [ Emery and Lantuéjoul , ].…”
Section: Introductionmentioning
confidence: 99%
“…Similar algorithms include GROWTHSIM which introduces a random‐neighbor path [ Eskandari and Srinivasan , ] or HOSIM which uses spatial cumulants for pattern extraction [ Mustapha and Dimitrakopoulos , ]. Although training‐image based methods have been used in many hydrogeological applications [ Hermans et al ., ; Hu and Chugunova , ; Huysmans et al ., ; Mahmud et al ., ; Michael et al ., ], they suffer from limitations inherent to the simulation algorithms. Some important points that limit the applicability of these methods are a high computational cost, the difficulty to reproduce certain types of patterns, and most importantly the limited variability that can be recovered from a finite size training image [ Emery and Lantuéjoul , ].…”
Section: Introductionmentioning
confidence: 99%
“…The existing methods to explore data features with heterogeneous variations are mainly from the perspective of the continuous spatiotemporal field. They can be roughly divided into the geostatistics analysis and statistical regression-based method (Huysmans et al, 2014). In geostatistics analysis, such as the Kriging (Kleijnen, 2009), generalized Kriging (Xu & Shu, 2015), Bayesian Maximum Entropy (Yu & Wang, 2013), etc., the spatiotemporal heterogeneous variation is considered where the temporal variation is a function of time distance and the spatial variation is a function of spatial distance, and the covariance function is used to describe the structure of heterogeneity (de Marsily et al, 2005).…”
Section: Introductionmentioning
confidence: 99%
“…The improved method was primarily used for reservoir phase pattern simulation (WU & FU, 2016;STRAUBHAAR et al, 2016). Simulations were mostly pattern simulations (VRIES et al, 2009;HUYSMANS et al, 2014), comprehensive simulations (LOU et al, 2015;GARDET et al, 2016), parameter optimization (GAO et al 2016), and computational efficiency research (ZUO et al, 2016;ABDOLLAHIFARD & NASIR, 2017). There are few studies on the patterns of continuous variables, and even fewer have been conducted on the calculation of resource reserves using the MPG method.…”
Section: Introductionmentioning
confidence: 99%