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Effects of Potamogeton crispus growth on phosphorus fractions in lake sediments at two nutrient levels
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This study explored the regulatory effects of Potamogeton crispus (P. crispus) on phosphorus fractions in lake sediments under two nutrient conditions, using a rhizosphere–non-rhizosphere partitioning approach. Sediments from Tangxun Lake (mesotrophic) and Nan Lake (eutrophic), Wuhan, China, were used in a controlled microcosm experiment. The dynamics of seven phosphorus fractions (Ca₂-P, Al-P, Org-P, Fe-P, O-Al-P, O-Fe-P, and Ca₁₀-P) were analyzed across different growth stages. Results showed: (1) In mesotrophic sediments, P. crispus significantly reduced labile phosphorus (Ca₂-P and Fe-P) in the rhizosphere, indicating enhanced uptake and stabilization; (2) In eutrophic sediments, phosphorus fractions including Org-P and Ca₁₀-P accumulated in the rhizosphere, reflecting active turnover and long-term retention; (3) O-Fe-P was consistently lower in rhizosphere sediments across both lakes, likely due to rhizosphere-induced redox suppression. These findings highlight the dual role of P. crispus in activating and stabilizing phosphorus in sediments and provide theoretical guidance for plant-based lake restoration strategies.
Title: Effects of Potamogeton crispus growth on phosphorus fractions in lake sediments at two nutrient levels
Description:
This study explored the regulatory effects of Potamogeton crispus (P.
crispus) on phosphorus fractions in lake sediments under two nutrient conditions, using a rhizosphere–non-rhizosphere partitioning approach.
Sediments from Tangxun Lake (mesotrophic) and Nan Lake (eutrophic), Wuhan, China, were used in a controlled microcosm experiment.
The dynamics of seven phosphorus fractions (Ca₂-P, Al-P, Org-P, Fe-P, O-Al-P, O-Fe-P, and Ca₁₀-P) were analyzed across different growth stages.
Results showed: (1) In mesotrophic sediments, P.
crispus significantly reduced labile phosphorus (Ca₂-P and Fe-P) in the rhizosphere, indicating enhanced uptake and stabilization; (2) In eutrophic sediments, phosphorus fractions including Org-P and Ca₁₀-P accumulated in the rhizosphere, reflecting active turnover and long-term retention; (3) O-Fe-P was consistently lower in rhizosphere sediments across both lakes, likely due to rhizosphere-induced redox suppression.
These findings highlight the dual role of P.
crispus in activating and stabilizing phosphorus in sediments and provide theoretical guidance for plant-based lake restoration strategies.
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