Predicting Daily Water Table Fluctuations in Karstic Aquifers from GIS-Based Modelling, Climatic Settings and Extraction Wells

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Predicting Daily Water Table Fluctuations in Karstic Aquifers from GIS-Based Modelling, Climatic Settings and Extraction Wells

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作者：Concepcion Pla ; Javier Valdes-Abellan…
关键词：Karstic aquifer ; Recharge ; Effective porosity ; Semiarid regions ; Simple model
刊名：Water Resources Management
出版年：2016
出版时间：May 2016
年：2016
卷：30
期：7
页码：2531-2545
全文大小：747 KB
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作者单位：Concepcion Pla (1) (2)
Javier Valdes-Abellan (3)
Antonio Jose Tenza-Abril (3)
David Benavente (1) (2)

1. Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Alicante, Spain
2. Laboratorio de Petrología Aplicada, Unidad Asociada UA-CSIC, Universidad de Alicante, Alicante, Spain
3. Departamento de Ingeniería Civil, Universidad de Alicante, Alicante, Spain
刊物类别：Earth and Environmental Science
刊物主题：Earth sciences
Hydrogeology
Geotechnical Engineering
Meteorology and Climatology
Civil Engineering
Environment
出版者：Springer Netherlands
ISSN：1573-1650

文摘

In semiarid regions, karstic aquifers are in some cases essential since they often constitute the only source of water supply. The increasing demand for water in these regions is responsible for the decreasing water table levels. As a consequence, groundwater management becomes indispensable. A robust black-box model of the Solana aquifer, a large karstic aquifer in Alicante province, is developed considering GIS-based modelling of the studied area, climatic settings and anthropic disturbances (water extractions and irrigation returns). The proposed model accurately predicts water table levels evolution (with EF index of 0.97 and RMSE of 0.09) and assesses the recharge rates. The model aims to become a useful tool in order to better understand the characteristics of karstic aquifers. A distinctive feature of the model is that it estimates the heterogeneous effective porosities along the depth profiles of the aquifer, which provides an advantage related to detect changes in the hydraulic transmissivity within karstic formations.