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- W3092811792 abstract "hydrological modeling is commonly crossed by the solution of inverse problems and the estimation for non-linear parameters techniques. Despite this common scenario, the use of these guidelines is limited to the proper sampling of in-field data. This sampling involves a variety of data that generally have little availability, especially in regions where geographical and climatic variability does not allow a constant measurement. In this article, we present the analysis of a regional underground flow model using two techniques: pilot points (PP) and constant zones (CZ). This methodologies allow identifying properly if there are any biased parameters and heterogeneity of hydraulic properties. For this purpose, we developed a numerical variable density model that is limited with reinterpreted data from real measurements. For the CZ technique, the initial parameters are assigned according to its layer, and every layer is considered constant for parameter values; in contrast for PP technique, the initial parameters are assigned according to interpolations using in-situ point measurements. The developed model was applied in an area under the influence of the ITCZ, located in the middle valley of Magdalena (MMV). This area is important on the development of the country due to its contribution to GDP and has been subject to significant changes in land use, as a result of intense economic activities, for example, agriculture, hydroelectric power, and production of oil and gas. The established model shows a scarce link with the observed state variable (hydraulic head -K), this proves the importance of spatial heterogeneity in K. The model is calibrated in order to establish K (as an anisotropic variable that varies spatially), the porosity (η) and the specific storage capacity (Ss) in the PP and CZ, reducing a “mean square” error of state variable dependable on the observation points. The results show that the PP system approach provides a better heterogeneity representation and shows that each parameter is sensitive, and does not depend on other parameters, giving to the parameter evaluation results factual independence and authenticity. This research compiles a methodology to assertively restrict a highly parameterized inverse model with field data to estimate aquifer parameters that vary spatially at a regional scale" @default.
- W3092811792 created "2020-10-22" @default.
- W3092811792 creator A5026212222 @default.
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- W3092811792 creator A5085548743 @default.
- W3092811792 date "2020-10-12" @default.
- W3092811792 modified "2023-09-26" @default.
- W3092811792 title "Hydrogeological Modeling in Tropical Regions via FeFlow" @default.
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- W3092811792 cites W1643465445 @default.
- W3092811792 cites W1651255643 @default.
- W3092811792 cites W1778389879 @default.
- W3092811792 cites W1796344724 @default.
- W3092811792 cites W1814015335 @default.
- W3092811792 cites W1821143250 @default.
- W3092811792 cites W1823825519 @default.
- W3092811792 cites W1913041613 @default.
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- W3092811792 cites W1976146173 @default.
- W3092811792 cites W1979863169 @default.
- W3092811792 cites W1987417598 @default.
- W3092811792 cites W1992644847 @default.
- W3092811792 cites W1996281714 @default.
- W3092811792 cites W1998417503 @default.
- W3092811792 cites W1998931446 @default.
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- W3092811792 cites W2102277009 @default.
- W3092811792 cites W2119352997 @default.
- W3092811792 cites W2133513614 @default.
- W3092811792 cites W2145384211 @default.
- W3092811792 cites W2152312062 @default.
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- W3092811792 cites W2251516244 @default.
- W3092811792 cites W2254391763 @default.
- W3092811792 cites W2338200983 @default.
- W3092811792 cites W2339307340 @default.
- W3092811792 cites W2341474976 @default.
- W3092811792 cites W2403711021 @default.
- W3092811792 cites W2465310577 @default.
- W3092811792 cites W2475999764 @default.
- W3092811792 cites W2485881327 @default.
- W3092811792 cites W2516020927 @default.
- W3092811792 cites W2530423770 @default.
- W3092811792 cites W2567693678 @default.
- W3092811792 cites W2605011992 @default.
- W3092811792 cites W2607164790 @default.
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- W3092811792 cites W2617605364 @default.
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- W3092811792 cites W2746724255 @default.
- W3092811792 cites W2752323820 @default.
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- W3092811792 cites W2782220640 @default.
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- W3092811792 doi "https://doi.org/10.15446/esrj.v24n3.80116" @default.
- W3092811792 hasPublicationYear "2020" @default.
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