4.7 Article

Key hydrological processes in the Del Azul Creek basin, sub-humid Pampean Plain

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 754, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2020.142258

关键词

Hydrological-physical processes; Stable isotopes; Rainwater; Surface water; Groundwater; Pampeano Aquifer

资金

  1. Instituto de Hidrologia de Llanuras Dr. Eduardo J. Usunoff (IHLLA, Argentina)
  2. project PICT 2016 [3688]
  3. Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET, Argentina)
  4. Agencia Nacional de Promocion Cientifica y Tecnologica (ANPCyT, Argentina)

向作者/读者索取更多资源

Groundwater in the Chaco-Pampean Plain in Argentina plays a crucial role in economic activities, with a focus on industry, agriculture, and cattle farming. A study analyzing environmental tracers aimed to update the hydrological model of the Del Azul Creek basin in Buenos Aires Province, showcasing seasonal variations in rainfall isotopic compositions. Evaporation was found to be significant in the flatter regions of the basin, impacting the isotopic composition of groundwater.
Groundwater plays an important role in the economic development of the Chaco-Pampean Plain (Argentina), where industry, agriculture and cattle farming are the main economic activities. The 66% of the country's population lives in this area. The low slopes of this region condition the water movement and the occurrence of physical and chemical processes. The aim of this work is to update the hydrological conceptual model of the Del Azul Creek basin (Buenos Aires Province), a sub-humid and continental plain, using environmental tracers. In total, the study was based on the analysis of 201 samples (stable isotopes) and 184 samples (chemical data) including rainwater, surface water and groundwater. The temporal and spatial variation in the isotopic composition of rainfall and the hydrological physical-processes, evaporation, surface water-groundwater interaction and recharge were studied. Isotopic compositions of rainfall revealed a seasonal variation across the basin. Low delta O-18 rainfalls occur during the coldest seasons, while high delta O-18 rainfalls occur during the warmest seasons. The isotopic compositions of rainfall varied only during the cold period in the upper basin. At this time, the lowest delta O-18 rainfall fell in the upper basin, while in the other areas and during the warmer seasons, no differences were observed. Evaporation was a relevant process in the flatter area of the basin, mainly during the warmest seasons. Samples taken from the wetlands and from the lower section of the Del Azul Creek were strongly evaporated. In the first 30 m depth of the aquifer, groundwater reflected the isotopic composition of rainfall from the warmest seasons, thus revealing seasonal preferential recharge and a good hydraulic connection. This study provides direct evidence showing that both evaporation and the surface water-groundwater interaction are processes that play a key role in the control of the isotopic and chemical composition of water. (C) 2020 Elsevier B.V. All rights reserved.

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