Dissolved concentrations of major elements and water isotopes for water samples 
from the Rio Bermejo mainstem, tributaries, spring-fed channels, and 
groundwater wells

Repasch, Marisa N.; Scheingross, Joel S.; Cook, Kristen; Sachse, D.; Dosch, Sophia Franziska; Orfeo, Oscar

doi:10.1594/PANGAEA.959932

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Dissolved concentrations of major elements and water isotopes for water samples from the Rio Bermejo mainstem, tributaries, spring-fed channels, and groundwater wells

Urheber*innen

Repasch, Marisa N.
External Organizations;

Scheingross, Joel S.
External Organizations;

Cook, Kristen
External Organizations;

/persons/resource/dsachse

Sachse, D.
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/dosch

Dosch, Sophia Franziska
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Orfeo, Oscar
External Organizations;

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Zitation

Repasch, M. N., Scheingross, J. S., Cook, K., Sachse, D., Dosch, S. F., Orfeo, O. (2023): Dissolved concentrations of major elements and water isotopes for water samples from the Rio Bermejo mainstem, tributaries, spring-fed channels, and groundwater wells.
https://doi.org/10.1594/PANGAEA.959932

Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5023313

Zusammenfassung

Water samples were filtered to 0.2 micron prior to measurement. Samples for cation analysis were acidified in the field to pH < 2 using 6N HNO3. Cation concentrations were measured with a Varian 720 inductively coupled plasma optical emission spectrometer (ICP-OES) at the GFZ Helmholtz Laboratory for the Geochemistry of the Earth Surface (HELGES), using SLRS-5 (Saint-Laurent River Surface, National Research Council - Conseil National de Recherches Canada) and USGS M212 and USGS T187 as external standards. We corrected for instrument drift by measuring an internal standard (GFZ-RW1) every 10 samples and we determined measurement uncertainty using calibration curve uncertainty. Anion concentrations were measured with a Dionex ICS1100 Ion Chromatograph, using USGS standards M206 and M212 as external standards for quality control, with uncertainty determined from triplicate analysis. We corrected cation concentrations for cyclic salt inputs following Bickle et al. (2005, doi:10.1016/j.gca.2004.11.019).