2017
DOI: 10.1016/j.petrol.2017.04.016
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Recursive update of channel information for reliable history matching of channel reservoirs using EnKF with DCT

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Cited by 30 publications
(21 citation statements)
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“…In EnKF, all reservoir models, called ensemble, are a group of state vectors y and they are constructed by reservoir variables and predicted data. We update permeability values in this paper, but other properties such as porosity, facies ratio, and aquifer strength can be put into the state vectors (Zhao et al 2008;Jung et al 2017a;Kim et al 2017). In the assimilation step, ensemble Y is updated by Eq.…”
Section: Ensemble Kalman Filtermentioning
confidence: 99%
“…In EnKF, all reservoir models, called ensemble, are a group of state vectors y and they are constructed by reservoir variables and predicted data. We update permeability values in this paper, but other properties such as porosity, facies ratio, and aquifer strength can be put into the state vectors (Zhao et al 2008;Jung et al 2017a;Kim et al 2017). In the assimilation step, ensemble Y is updated by Eq.…”
Section: Ensemble Kalman Filtermentioning
confidence: 99%
“…DCT is also used to extract the main information of a static model in a history matching area [27][28][29][30][31][32][33][34][35]. After original data are transformed to coefficients of discrete cosine functions, the coefficients are arranged in descending order of frequencies of cosine functions.…”
Section: Combined Distancementioning
confidence: 99%
“…The selection of a subset of DCT coefficients depends on the objective of the research. For example, to characterize channel reservoirs, several papers applied DCT to permeability data to extract only the main channel trends in the ensemble models with low frequencies' coefficients [27][28][29][30][31][32]34,35]. The channel trends in reservoirs can be described with only a small number of coefficients.…”
Section: + ( − 3) =mentioning
confidence: 99%
“…These methods typically involve the following steps: (1) estimating a prior ensemble of facies distribution using indicator geostatistical models, (2) translating the ensemble facies distribution to continuous shape parameters that describe the facies boundaries, (3) performing EDA on the shape parameters to improve the match between model predictions and observations, and (4) updating the facies distribution using the updated shape parameters. All of the aforementioned parameterization methods impose no spatial structure constraints on facies (e.g., facies volume proportions, correlation lengths, or juxtapositional tendencies) in the process of data assimilation, which may lead to an unrealistic discontinuity and/or overfitting in resulted facies distribution (Jung et al, 2017;Ma & Jafarpour, 2018;Nejadi et al, 2015;Vo & Durlofsky, 2016;Zhao et al, 2017). Chang and Zhang (2014) proposed to alleviate the facies discontinuity issue by updating facies indicators on a coarse representation of the computational grid and then using interpolation to generate the rest of the facies field.…”
Section: Introductionmentioning
confidence: 99%