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Water Quality and Microclimate Gradients in the Argentine Andes and Patagonia: Field Measurements of TDS, Conductivity, and Temperature Across Altitudes
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Abstract
This field study reports portable in situ measurements of water temperature, Total Dissolved Solids (TDS), electrical conductivity (EC), air temperature, and humidity across six representative sites in Argentina (March 2025). We sampled 20 points spanning 115 m (Perito Moreno) to 3 383 m (Aconcagua). Mean TDS at high‑altitude sites (Aconcagua: 1172 ± 425 ppm) was up to 50 times higher than at Patagonian lakes (Refugio Frey: 6 ± 1 ppm). A near‑perfect linear relationship (EC = 2.01 × TDS, R² = 0.995) validates field conductivity proxies. These novel baseline data reveal unexpectedly high mineralization in Andean meltwaters and underscore geological controls on freshwater chemistry in remote mountain ecosystems.
DOI
https://doi.org/10.31223/X5643S
Subjects
Physical Sciences and Mathematics
Keywords
Total Dissolved Solids (TDS), Electrical Conductivity, Andes, Patagonia, Microclimate, water quality, Altitudinal Gradient, Glacial Meltwater
Dates
Published: 2025-05-18 01:41
Last Updated: 2025-05-18 01:41
License
CC BY Attribution 4.0 International
Additional Metadata
Conflict of interest statement:
none
Data Availability (Reason not available):
All data underlying this study will be deposited in a public repository (e.g. Zenodo) and made available via a DOI upon acceptance.
There are no comments or no comments have been made public for this article.