In this study, sediment internal
phosphorus (P) and its
supply
ability were studied in the algal-dominated zone of Lake Taihu during
the overwintering and recruitment period of algae. The results indicated
that sediment P fluxes, P mobile fractions, and P supply kinetics
showed dynamic changes from the overwinter to the algal recruitment
period. P flux and the concentration of the diffusive gradient in
thin film (DGT)-measured labile P increased from winter to summer.
However, the highest P supply ability was found in spring sediments,
as indicated by the ratios of DGT-P to porewater P, suggesting that
spring sediments can supply more P for the growth of overwinter algae.
Laboratory incubation experiments show that sediment with a higher
mobile P content could release more soluble P under suitable conditions,
thereby increasing the chlorophyll a (Chla) concentration.
The growth of overwinter algae appeared to be more correlated with
porewater P concentrations and the ratios of nitrogen to phosphorus
than with the solid-phase mobile P fractions, as indicated by the
Pearson correlation analysis. This study strengthens our understanding
of the relationship between the availability of sediment P and algal
recruitment from sediments.