This note presents a model calibration experience on a complex groundwater system located in central Italy, in the subsiding Acque Albule Plain near Rome (Italy).There are two main aquifers in this system. The first one, partially confined by Pliocene-Pleistocene deposits, is constituted by the limestone fractured bedrock, while the second one, unconfined, is within the fractured travertine. These two aquifers are connected in correspondence of the center of the plain, where deep hydrothermal water, starting from the limestone bedrock, upwells through the Plio-Pleistocene deposits in to the travertine.A.A. ground water model is applied to a 55km2 and is developed using Modflow-2005, discretized by 100x100 meters cells and three layers. Calibration process applied to this model consisted in several steps using estimation methods along with sensitivity analysis and geology information.The final model fitting shows clearly the importance of applying not only automatic estimation methods for calibration processes but also the need to be prepared to change own conceptual model starting from sensitivity analysis and from collecting new data to better understand the system.

LA VIGNA, F., Rossetto, R., Mazza, R. (2009). Ground water model calibration using geology information along with sensitivity analysis and estimation methods (UCODE-2005), the Acque Albule model, Rome, (Italy). In Calibration and Reliability in Groundwater Modeling “Managing Groundwater and the Environment" (pp.79-82). WUHAN : China University of Geosciences Press.

Ground water model calibration using geology information along with sensitivity analysis and estimation methods (UCODE-2005), the Acque Albule model, Rome, (Italy)

MAZZA, Roberto
2009-01-01

Abstract

This note presents a model calibration experience on a complex groundwater system located in central Italy, in the subsiding Acque Albule Plain near Rome (Italy).There are two main aquifers in this system. The first one, partially confined by Pliocene-Pleistocene deposits, is constituted by the limestone fractured bedrock, while the second one, unconfined, is within the fractured travertine. These two aquifers are connected in correspondence of the center of the plain, where deep hydrothermal water, starting from the limestone bedrock, upwells through the Plio-Pleistocene deposits in to the travertine.A.A. ground water model is applied to a 55km2 and is developed using Modflow-2005, discretized by 100x100 meters cells and three layers. Calibration process applied to this model consisted in several steps using estimation methods along with sensitivity analysis and geology information.The final model fitting shows clearly the importance of applying not only automatic estimation methods for calibration processes but also the need to be prepared to change own conceptual model starting from sensitivity analysis and from collecting new data to better understand the system.
2009
978-7-5625-2417-5
LA VIGNA, F., Rossetto, R., Mazza, R. (2009). Ground water model calibration using geology information along with sensitivity analysis and estimation methods (UCODE-2005), the Acque Albule model, Rome, (Italy). In Calibration and Reliability in Groundwater Modeling “Managing Groundwater and the Environment" (pp.79-82). WUHAN : China University of Geosciences Press.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/175327
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