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Fe and Al sedimentation and their importance as carriers for P, N and C in a large humic Lake in Northern Sweden

  • Role of Sediments in Element Cycles
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Abstract

The sedimentation of organic, amorphous oxides, crystalline oxides and crystalline silicate species of Fe and Al was investigated in humic Lake Örträsket. The covariation with C, N and P sedimentation also was studied. The results showed a strong temporal variation in the occurrence of different Fe species. During high discharge, such as in spring. Fe mostly occurred as crystalline Fe-silicate species, while the amorphous form dominated at other times of the year. Al generally sedimented as crystalline AI-silicate species (95%). Amorphous Fe species showed a strong relation with organic C and N, suggesting an association between organic material and amorphous Fe oxides. P was not as strongly related to amorphous Fe, probably as a result of apatite or clay bound-P species sedimentation.

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Jonsson, A. Fe and Al sedimentation and their importance as carriers for P, N and C in a large humic Lake in Northern Sweden. Water Air Soil Pollut 99, 283–295 (1997). https://doi.org/10.1007/BF02406868

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