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Laboratory-determined Phosphorus Flux from Lake Sediments as a Measure of Internal Phosphorus Loading
Published on: March 6, 2014
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Ocean acidification: One potential driver of phosphorus eutrophication.
Changzi Ge1, Yanchao Chai1, Haiqing Wang1
1Marine College, Shandong University, Weihai, Weihai 264209, China.
Marine Pollution Bulletin
|December 17, 2016
Summary
Ocean acidification may worsen harmful algal blooms by releasing phosphorus from sediments. This study found that lower pH significantly reduced phosphorus in oxic sediments, facilitating its diffusion into the water.
Area of Science:
- Marine chemistry
- Environmental science
- Eutrophication studies
Background:
- Harmful algal blooms are increasing and may be phosphorus-limited.
- Ocean acidification is a concurrent environmental stressor.
- A potential link exists between ocean acidification and phosphorus eutrophication.
Purpose of the Study:
- To investigate if ocean acidification influences phosphorus release from sediments.
- To test the hypothesis that lower pH can lead to phosphorus eutrophication.
Main Methods:
- Oxic sediments were incubated in seawater under varying pH conditions (pH 8.1 and 7.7) for 30 days.
- Quantified total phosphorus (TP), inorganic phosphorus (IP), and exchangeable phosphorus (Ex-P) in sediments.
- Analyzed the diffusion of reduced phosphorus into the water column.
Main Results:
- Sediments exposed to lower pH (7.7) showed significantly reduced levels of exchangeable phosphorus (Ex-P) and inorganic phosphorus (IP) compared to pH 8.1.
- Specifically, Ex-P decreased from 4.40±0.45 μg/g at pH 8.1 to 2.82±0.15 μg/g at pH 7.7.
- IP content decreased from 1.39±0.10 mg/g at pH 8.1 to 1.06±0.20 mg/g at pH 7.7.
Conclusions:
- Ocean acidification significantly reduces phosphorus content in oxic sediments.
- This reduction facilitates phosphorus diffusion into the water column.
- Ocean acidification is identified as a potential facilitator of phosphorus eutrophication under oxic conditions.
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