Skip to main page content
U.S. flag

An official website of the United States government

Dot gov

The .gov means it’s official.
Federal government websites often end in .gov or .mil. Before sharing sensitive information, make sure you’re on a federal government site.

Https

The site is secure.
The https:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

Access keys NCBI Homepage MyNCBI Homepage Main Content Main Navigation
. 2023 Apr 3;195(5):535.
doi: 10.1007/s10661-023-11067-2.

Hydrochemistry and weathering at Pardo River basin, São Paulo State, Brazil

Affiliations

Hydrochemistry and weathering at Pardo River basin, São Paulo State, Brazil

Daniel Marcos Bonotto. Environ Monit Assess. .

Abstract

This work was conducted at the Pardo River hydrographic basin, which is a federal watershed belonging to the Paranapanema River hydrographic basin (PRHB) in Brazil (São Paulo State and Paraná State). The aim was to realize an integrated hydrochemical and radiometric (U-isotopes and 210Po) approach, highlighting the water/soil-rock and surface water/groundwater interactions, with implications to the weathering processes occurring there. The study area has been often considered one of the best preserved/unpolluted river in São Paulo State, contributing to the water supply of several cities distributed along its banks. However, the results reported here suggest possible lead diffuse pollution caused by the use of phosphate fertilizers in agricultural activities taking place in the basin. The analyzed groundwaters and surface waters tend to be neutral to slightly alkaline (pH of 6.8-7.7), possessing low mineral concentration (total dissolved solids up to 500 mg/L). SiO2 is the major dissolved constituent in the waters, while bicarbonate is the dominant anion, and calcium is the preponderant cation. The effects of the weathering of silicates to control the dissolution of constituents in the liquid phase have been identified from some diagrams often utilized in hydrogeochemical studies. Chemical weathering rates have been estimated from hydrochemical data associated to analytical results of the natural uranium isotopes 238U and 234U concerning to samples of rainwater and Pardo River waters. The fluxes in this watershed are permitted to obtain the following rates: 11.43 t/km2 year (sodium), 2.76 t/km2 year (calcium), 3.17 t/km2 year (magnesium), 0.77 t/km2 year (iron), and 8.64 t/km2 year (uranium). This new dataset constitutes valuable information for people engaged on the management of the Pardo River watershed, as well as to researchers interested on comparative studies considering the available data from other basins worldwide.

Keywords: Chemical weathering rates; Groundwaters; Hydrochemistry; Pardo River watershed; Surface waters.

PubMed Disclaimer

References

    1. Albarelli, D. S. N. A. (2013). Depositional environments and ceramic characterization of Araçatuba Formation (Bauru basin) at Santo Anastácio River valley, São Paulo State. Monograph. Campinas: UNICAMP-University of Campinas. (in Portuguese).
    1. Anjinho, P., Barbosa, M., Costa, C. W., & Mauad, F. F. (2020). Environmental fragility analysis in reservoir drainage basin land use planning: A Brazilian basin case study. Land Use Policy, 100. https://doi.org/10.1016/j.landusepol.2020.104946
    1. Baas Becking, L. G. M., Kaplan, I. R., & Moore, D. (1960). Limits of the natural environment in terms of pH and oxidation-reduction potential. Journal of Geology, 68, 243–284. - DOI
    1. Baskaran, M. (1995). A search for the seasonal variability on the depositional fluxes of 7Be and 210Pb. Journal of Geophysical Research, 100, 2833–2840. - DOI
    1. Baskaran, M. (2012). Handbook of Environmental Isotope Geochemistry. Berlin: Springer. - DOI

LinkOut - more resources