2017
DOI: 10.5194/hess-21-6069-2017
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Multiple-point statistical simulation for hydrogeological models: 3-D training image development and conditioning strategies

Abstract: Abstract. Most studies on the application of geostatistical simulations based on multiple-point statistics (MPS) to hydrogeological modelling focus on relatively fine-scale models and concentrate on the estimation of facies-level structural uncertainty. Much less attention is paid to the use of input data and optimal construction of training images. For instance, even though the training image should capture a set of spatial geological characteristics to guide the simulations, the majority of the research stil… Show more

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Cited by 48 publications
(45 citation statements)
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“…Two-point geostatistics (Pyrcz and Deutsch, 2014;Ritzi, 2000) and object-based methods (Deutsch and Tran, 2002;Maharaja, 2008;Pyrcz et al, 2009) are not effective at reproducing anisotropic features and connectivity patterns properly (Heinz et al, 2003;Klise et al, 2009;Knudby and Carrera, 2005;Vassena et al, 2010) due to the lack of high-order statistics and the difficulty in parameterization. To overcome the abovementioned limitations, multiple-point statistics (MPS) was developed over recent years and has shown prospects in modeling subsurface anisotropic structures, such as porous media, hydrofacies, reservoirs and other sedimentary structures (Dell Arciprete et al, 2012;Hajizadeh et al, 2011;Hu and Chugunova, 2008;Oriani et al, 2014;Pirot et al, 2015;Wu et al, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…Two-point geostatistics (Pyrcz and Deutsch, 2014;Ritzi, 2000) and object-based methods (Deutsch and Tran, 2002;Maharaja, 2008;Pyrcz et al, 2009) are not effective at reproducing anisotropic features and connectivity patterns properly (Heinz et al, 2003;Klise et al, 2009;Knudby and Carrera, 2005;Vassena et al, 2010) due to the lack of high-order statistics and the difficulty in parameterization. To overcome the abovementioned limitations, multiple-point statistics (MPS) was developed over recent years and has shown prospects in modeling subsurface anisotropic structures, such as porous media, hydrofacies, reservoirs and other sedimentary structures (Dell Arciprete et al, 2012;Hajizadeh et al, 2011;Hu and Chugunova, 2008;Oriani et al, 2014;Pirot et al, 2015;Wu et al, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…5 No matter which MPS algorithm is used, a suitable training image is the fundamental requirement. Although such algorithms are gaining popularity in hydrogeological applications (Hermans et al, 2015;He et al, 2014;Høyer et al, 2017;Hu and Chugunova, 2008;Huysmans et al, 2014;Jha et al, 2014;Mahmud et al, 2015), they still suffer from one vital limitation: the lack of training images, especially for 3-D situations. Object-based or process-based techniques are one possibility to build 3-D training images (de Marsily et al, 2005;de Vries et al, 2009;Feyen and Caers, 2004;Maharaja, 10 2008;Pyrcz et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…No matter which MPS algorithm is used, a suitable training image is the fundamental requirement. Although such algorithms are gaining popularity in hydrogeological applications (Hermans et al, 2015;He et al, 2014;Høyer et al, 2017;Hu and Chugunova, 2008;Huysmans et al, 2014;Jha et al, 2014;Mahmud et al, 2015), they still suffer from one vital limitation: the lack of training images, especially for 3-D situations. Object-based or process-based techniques are one possibility to build 3-D training images (de Marsily et al, 2005;de Vries et al, 2009;Feyen and Caers, 2004;Maharaja, 2008;Pyrcz et al, 2009).…”
Section: Introductionmentioning
confidence: 99%