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A groundwater flow model for water resources management in the Ismarida plain, North Greece

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This paper presents the development of a regional flow simulation model of the stream–aquifer system of Ismarida plain, northeastern Greece. It quantifies the water budget for this aquifer system and describes the components of groundwater and the characteristics of this system on the basis of results of a 3-year field study. The semiconfined aquifer system of Ismarida Lake plain consists of unconsolidated deltaic clastic sediments, is hydraulically connected with Vosvozis River, and covers an area of 46.75 km2. The annual precipitation ranges in the study area from 270 to 876 mm. Eighty-seven irrigation wells are densely located and have been widely used for agricultural development. Groundwater flow in this aquifer was simulated with MODFLOW. Model calibration was done with observed water levels, and match was excellent. To evaluate the impacts of the current pumping schedule and propose solutions, four management scenarios were formulated and tested with the model. Based on model results, the simulated groundwater budget indicates that there must be approximately 33% decrease of withdrawals to stop the dramatic decline of groundwater levels. The application of these scenarios shows that aquifer discharge to the nearby river would be very low after a 20-year period.

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Authors and Affiliations

  1. Laboratory of Ecological Engineering and Technology, Department of Environmental Engineering, Democritus University of Thrace, Vas. Sofias 12, 67100, Xanthi, Greece

    V. Pisinaras, C. Petalas & V. A. Tsihrintzis

  2. Hellenic Centre for Marine Research (HCMR), Institute of Oceanography, Athens-Sounio Avenue, 19013, Anavyssos, Greece

    E. Zagana

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  1. V. Pisinaras
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  2. C. Petalas
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  3. V. A. Tsihrintzis
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  4. E. Zagana
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Correspondence to C. Petalas.

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Pisinaras, V., Petalas, C., Tsihrintzis, V.A. et al. A groundwater flow model for water resources management in the Ismarida plain, North Greece. Environ Model Assess 12, 75–89 (2007). https://doi.org/10.1007/s10666-006-9040-z

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  • DOI: https://doi.org/10.1007/s10666-006-9040-z

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