From:
Kamatani, A,; Amano, M. 1984. Phosphate and silica regeneration from fecal pellets of benthic animals collected from Tokyo Bay. BULL. JAP. SOC. SCI. FISH./NISSUISHI., vol. 50, no. 6, pp. 999-1003
"The study strongly supports the assumption that phosphate and silica regenerated from the fecal pellets supply a significant fraction of nutrients required by primary producers in the water column during summer months when anoxic conditions are spreading in the water-sediment interface."
In other words, phosphate is regerated your benthic biota when the anoxic band nears the surface of the bed, moves into the bulk water and feeds nuisance algae.
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From:
Ikeda, T; Carleton, JH; Mitchell, AW; Dixon, P. 1982. Ammonia and phosphate excretion by zooplankton from the inshore waters of the Great Barrier Reef. II. Their in situ contributions to nutrient regeneration. AUST. J. MAR. FRESHWAT. RES., vol. 33, no. 4, pp. 683-698.
"Calculations from an empirical equation relating temperature to oxygen consumption by a bottom community indicated a high potential for benthic nutrient regeneration in reef inshore waters (27 multiplied by 1 g m super(-2) per year, as nitrogen). The bottom community therefore appears to be the most important source of nutrient regeneration within the area studied."
Demonstrates importance of regeneration of phosphate by substrate for algal growth.
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From:
Fan, C-X; Zhang, L; Qu, W-C. 2001. Lake sediment resuspension and caused phosphate release--a simulation study. Journal of Environmental Sciences (China). Vol. 13, no. 4, pp. 406-410.
"The internal phosphorus loading induced by resuspension is estimated to be 8 - 10 times greater than the release from undisturbed sediment."
Now do you really want to stir that bed?

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From:
Hasnaoui, M; Kassila, J; Loudiki, M; Droussi, M; Balvay, G; Barroin, G. 2001. Phosphate release at the water-sediment interface in a fisheries pond of the Deroua fish farm (Beni Mellal, Morocco). Revue des Sciences de l'Eau/Journal of Water Science [Rev. Sci. Eau/J. Water Sci.]. Vol. 14, no. 3, pp. 307-322.
"The phosphate (P) released from the sediment is the essential source of P for phytoplankton when the ponds are not fertilised"
Speaks for itself.
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Abstract from:
Gomez, E; Fillit, M; Ximenes, MC; Picot, B. 1998. Phosphate mobility at the sediment-water interface of a Mediterranean lagoon (Etang du Mejean), seasonal phosphate variation. Hydrobiologia [Hydrobiologia]. Vol. 373-374, no. 1-3, pp. 203-216.
"The Mejean Lagoon (Herault, France) is a confined, shallow system, 0.7 m in depth, with a surface area of 747 ha. Its sediments have a fine granulometry and are evenly distributed. The bathymetry and hydrodynamic behaviour of the basin create two zones with restricted exchanges between them. The western part (60% of the total surface area) is rich in dissolved phosphate (> 1 mg l super(-1) in summer) and receives the majority of the phosphate (P) inputs from the watershed. The heavy macroalgal population consists of Gracilaria throughout the year and Ulva in summer and autumn. Phytoplankton levels sometimes reach 100 mu g l super(-1) of chlorophyll a. The sediment-water phosphate exchange varies with environmental conditions and macroalgal growth. P mobility was studied on the basis of these characteristics. Algal biomass and water characteristics were measured at 15-day intervals throughout 1993. A seasonal study was conducted in 1994 to investigate which P fractions in the sediment were involved in the exchanges. The springtime rise in temperature reactivated decomposition of the macroalgal biomass that had accumulated in autumn. The redox potential (E sub(H)) fell as a result of this biological activity, leading to a decrease in the inorganic P fractions. This P release accounts for the higher P water concentrations observed in the lagoon in summer. The mobility of P fractions shows that the P stored in the sediments plays an active role in the dynamics of the overlying water. Seasonal variations in these fractions explain the patterns of P storage and mobilization."
So, while there are controlling factors as to rate of release (and there a lot more than just the temperature control that this article subscribes to), there is constants flux at the water/sediment interface.
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Abstract from:
Valdes, D; Real, E. 1998. Ammonium, nitrite, nitrate and phosphate fluxes across the sediment-water interface in a tropical lagoon. Ciencias marinas. Ensenada [CIENC. MAR.], vol. 20, no. 1, pp. 65-80.
"The sediments of Chelem Lagoon, on the coast of the Gulf of Mexico, north of the Yucatan Peninsula, were studied measuring the nutrient concentrations in the interstitial water. The average values were: ammonium 459 plus or minus 281 mu M, peaking up to 1,045 mu M; nitrite 1.8 plus or minus 1.8 mu M, with a maximum of 5.3 mu M; nitrate 8.2 plus or minus 10.3 mu M, reaching 34.7 mu M; phosphate 0.4 plus or minus 0.4 mu M, with a maximum of 1.1 mu M. Fluxes were estimated with Fick's first law equation. In all cases, the mean flux of the 14 samples from the lagoon were from the sediment to the water column; these values were 182 mu mol/m super(2)h for ammonium, 0.5 mu mol/m super(2)h for nitrite, 1.9 mu mol/mu2h for nitrate and 0.03 mu mol/m super(2)h for phosphate."
Lots of nutrients in the porewater. What is keeping your sediment's porewater from building up those kinds of concentrations?
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From:
Nakamura, Y. 1994. Effect of flow velocity on phosphate release from sediment. Water Science & Technology [WATER SCI. TECHNOL.], vol. 30, no. 10.
"At very low flow velocities, transport through the diffusive boundary layer is the limiting factor...and phosphate release rate is expressed as a linear decreasing function of the velocity. When flow velocities are increased... phosphate release rate become independent of velocity, since the reactions in the sediment are the rate limiting factor. "
So with the high flows in reef tank, the liberation reactions are firing off as fast as they can.
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Enough for now.