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Mass-transfer rates between water and benthos are derived based on the dissipation of energy by the benthic communities of coral reefs. Roughness of the benthic communities causes currents and waves to dissipate energy on reef flats at rates which far exceed ocean values of energy dissipation. The derivation here shows that first-order rate constants for nutrient uptake are (1) proportional to energy...
The Biosphere 2 coral reef biome is a large, fully enclosed, self-sustaining mesocosm. Water is moved throughout the mesocosm by waves. Inorganic and organic nutrients were monitored weekly from 1995 to 2000. Eight nutrient-uptake experiments were conducted to measure uptake-rate constants (S, m s–1) for NH4, PO4, and NO3. Nutrient concentrations were low, except for DON, and typical of coral-reef...
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