4.7 Article

Critical nutrient thresholds needed to control eutrophication and synergistic interactions between phosphorus and different nitrogen sources

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 23, Issue 20, Pages 21008-21019

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-016-7321-x

Keywords

Nutrient threshold; Synergistic interaction; Multiple nutrient limitations; Ammonium; Eutrophication; Bioassays

Funding

  1. Major Science and Technology Program for Water Pollution Control and Treatment in China [2014ZX07203010]
  2. Key Program of the Chinese Academy of Sciences [KZZD-EW-10-02]
  3. Comprehensive Demonstration Construction of Key Technology of Ecological Security in Beijing-Tianjin-Hebei Urban Agglomeration [2016YFC0503007]

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Eutrophication is one of the greatest threats to global freshwater ecosystems. The phytoplankton responses to nutrient inputs vary in different water bodies, so it is particularly important to determine the nutrient thresholds and synergistic interactions between nutrients in different freshwater ecosystems. Field sampling and bioassay experiments were conducted to determine the thresholds of soluble reactive phosphorus (SRP), nitrate-nitrogen (NO3-N), and ammonium-nitrogen (NH4-N) in Miyun Reservoir. A separate nutrient addition bioassay was designed to assess the synergistic interactions between these nutrients. Chlorophyll a (Chl a) concentrations were used to estimate phytoplankton biomass. The results showed the following: (1) nutrient threshold bioassay indicated that eutrophication thresholds of SRP, NO3-N, and NH4-N should be targeted at below 0.04 mg P L-1, 0.5 mg N L-1, and 0.3 mg N L-1, respectively, to limit the growth of phytoplankton. (2) The stimulatory effect of NH4-N plus P on phytoplankton biomass was greater than NO3-N plus P at the same N concentration, and NH4-N plus NO3-N did not show such associated stimulatory effect as NH4-N plus P or NO3-N plus P. (3) The average concentrations of total phosphorus (TP), NO3-N, and NH4-N in Miyun Reservior were 0.017 mg P L-1, 0.620 mg N L-1, and 0.143 mg N L-1, respectively. The reservoir-wide average Chl a is below 20 mu g L-1 on an annual basis. (4) Ammonium was an important factor for the growth of phytoplankton and inputs of both NH4-N and NO3-N should be reduced to control bloom formation. Our findings imply that although P load reduction is important, appropriate reductions of all forms of N in watershed is recommended in the nutrient management strategy for Miyun Reservoir.

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