Affiliations: Nanjing Institute of Geography and Limnology, Chinese
Academy of Sciences, Nanjing 210008, China. E-mail: cxfan@niglas.ac.cn
Abstract: Intact sediment cores and wet/dried surficial sediments sampled from
the two sublakes in Taihu Lake, Meiliang Bay and Wuli Lake, were incubated in
the laboratory to determine the effects of resuspension on internal phosphorus
loading by simulating different resuspension events. Soluble reactive
phosphorus (SRP) release from undisturbed core sediment sampled in the Meiliang
Bay and Wuli Lake in July 1998 was 1.53 mg/m² and 2.24 mg/m² within 4
days, respectively. However during one hour experimental simulation of
resuspension, SRP increased by 0.041 mg/L and 0.077 mg/L in the above cores,
which indicate that a typical resuspension event in the lake would be
accompanied by the release of 10.77 mgSRP/m² and 23.1 mgSRP/m²,
respectively. The internal phosphorus loading induced by resuspension is
estimated to be 8-10 times greater than the release from undisturbed sediment.
SRP release from the dried sediments during simulation of resuspension was
mainly dependent on the disturbing intensity. Only when the wind strength gets
to certain level, the influence of wind speed on phosphorus release appears
significant, indicating that an exchangeable P pool, capable of altering
equilibrium conditions in the lake areas, isbuilt up under strongly
wind-exposed resuspension events.
Keywords: sediment, Taihu Lake, phosphate release, resuspension simulation