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This document summarizes a study estimating the base flow of the Chumpe River in Peru using various hydrological methods. Water and groundwater balances were calculated using inputs like precipitation, evapotranspiration, and recharge. Recharge was estimated using the water table fluctuation method from piezometer data. Groundwater flow was modeled using Modflow software. Base flow was estimated to be between 20-40 liters per second, equivalent to 6-12% of annual rainfall for the 2013-2014 hydrological year

Author

Hans Sierra Lopinta

Language

EN