Acta Limnologica Brasiliensia (Nov 2024)

Photochemical mineralization of DOM in high humic tropical aquatic ecosystems: ambiguous regulation by watercolor

  • André Megali Amado,
  • Francisco de Assis Esteves,
  • Albert Luiz Suhett,
  • Ana Luiza Rangel Linhares Lima,
  • Layla Mayer Fonseca,
  • Vinicius Fortes Farjalla

DOI
https://doi.org/10.1590/s2179-975x0624
Journal volume & issue
Vol. 36

Abstract

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Abstract: Aim Photochemical mineralization is a significant pathway for the total oxidation of Dissolved Organic Carbon (DOC) in aquatic ecosystems. The concentration of DOC, watercolor, solar radiation intensity, diagenetic state of DOC, and oxygen availability are known regulating factors influencing the DOC photochemical mineralization process. However, these studies have not yet assessed the importance of these regulatory factors under extreme conditions of DOC concentration and watercolor. The aims of this study were: (1) to optimize methodological parameters for investigating the photo-degradation process in tropical humic/super-humic aquatic ecosystems; (2) to evaluate the relative importance of regulatory factors influencing photochemical mineralization in tropical humic/super-humic ecosystems; and (3) to measure photochemical mineralization rates in 20 coastal tropical humic/super-humic ecosystems and comparing them with available data worldwide. Methods Three types of DOC exposure experiments were conducted: (i) exposing water samples to different solar radiation intensities, (ii) exposing water samples of the same origin but with different DOC concentrations (dilutions) to sunlight and (iii) exposing water samples from a gradient of 20 environments with distinct characteristics to sunlight. Results Our results revealed that oxygen concentration became limiting for the photochemical mineralization process in experiments investigating super-humic ecosystems. Watercolor exhibited ambiguous effects on photochemical mineralization; in environments with colored-DOC, increased DOC watercolor favored higher potential photochemical mineralization rates, whereas in super-humic environments, increased DOC watercolor reduced the photochemical mineralization potential due to DOC self-shading. Conclusions We emphasize that the measured results in this study represent the highest values of photochemical mineralization ever recorded in the literature.

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