Factors influencing release of phosphorus from sediments in a high productive polymictic lake system

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Abstract

Phosphorus (P) release rates from bottom sediments are high (20.6mg/m 2/day) in Dal Lake (India), a polymictic hyper-eutrophic lake. These gross release rates occur over a period of 72 days during summer only. Likewise, a net internal load of 11.3 tons was obtained from mass balance estimates, Significant proportion i.e. ∼ 80% of 287.3 tons/yr of nitrate nitrogen (NO3-N) load is either eliminated by denitrification or gets entrapped for a short period in high macrophyte biomass of 3.2kg/m2 f.w., which eventually get decomposed and nitrogen (N) is released back. These processes result in low lake water NO3-N concentrations which potentially influence sediment phosphorus (P) release. Especially, nitrate nitrogen (NO3-N) <500μg/L in the lake waters were associated with high P concentrations. Phosphorus was also observed to increase significantly in relation to temperature and pH, and it seems likely that release of phosphorus and ammonical nitrogen (NH4-N) depend on decomposition of rich reserves of organic matter (893 tons d.w. in superficial 10-cm bottom sediment layer). Lake P concentrations were significantly predicted by a multivariate regression model developed for the lake. This study describes significance of various lake water variables in relation to P-release from bottom sediments. © IWA Publishing 2009.

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Solim, S. U., & Wanganeo, A. (2009). Factors influencing release of phosphorus from sediments in a high productive polymictic lake system. Water Science and Technology, 60(4), 1013–1023. https://doi.org/10.2166/wst.2009.445

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