Groundwater Origin and Dynamics on the Eastern Flank of the Colorado River Delta, Mexico

Isotope data and major ion chemistry were used to identify aquifer recharge mechanisms and geochemical evolution of groundwaters along the US–Mexico border. Local recharge originates as precipitation and occurs during winter through preferential infiltration pathways along the base of the Gila Range...

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Bibliographic Details
Main Authors: Hector A. Zamora, Christopher J. Eastoe, Jennifer C. McIntosh, Karl W. Flessa
Format: Article
Language:English
Published: MDPI AG 2021-05-01
Series:Hydrology
Subjects:
Online Access:https://www.mdpi.com/2306-5338/8/2/80