2018
DOI: 10.1007/s12665-018-7699-5
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Mobility of trace elements between the river water, the sediments, and the pore water of Las Catonas Stream, Buenos Aires Province, Argentina

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Cited by 6 publications
(18 citation statements)
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“…The identification of point sources of pollutants in these waters is difficult due to the intermittent and irregular discharges [62], but the detection of heavy metal entry is feasible through the analysis of the anaerobic sediments, where the metals are rapidly incorporated and accumulated. In accordance with our previous reports [3,4,6,32,37,63], as shown in Table 1, the level of contamination of the superficial waters at the SF site was much higher than in the DR site. The very low values of DO and ORP, and high values of nitrates and phosphates measured in SF depict the anaerobic state of the waters due to oxygen depletion by microbial activity on reduced compounds.…”
Section: Discussionsupporting
confidence: 92%
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“…The identification of point sources of pollutants in these waters is difficult due to the intermittent and irregular discharges [62], but the detection of heavy metal entry is feasible through the analysis of the anaerobic sediments, where the metals are rapidly incorporated and accumulated. In accordance with our previous reports [3,4,6,32,37,63], as shown in Table 1, the level of contamination of the superficial waters at the SF site was much higher than in the DR site. The very low values of DO and ORP, and high values of nitrates and phosphates measured in SF depict the anaerobic state of the waters due to oxygen depletion by microbial activity on reduced compounds.…”
Section: Discussionsupporting
confidence: 92%
“…In the case of natural clays, the SSA values measured in the DR clay fractions were consistent with the particle size and corresponded to values typically found in clays with a mineral composition characterized by the presence of illite and smectite [7,32] and with a low content of OM [16,66,67]. Concerning the clays extracted from SF, we found that the upper section of the SF core (SF1: 0-5 cm) had particles of a smaller size than the respective sediment particles.…”
Section: Discussionsupporting
confidence: 84%
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