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The key estuarine zone practiced episodic low DO and sporadic hypoxia after 2000. The ecosystem buffering capability ended up being characterized by turbidity, really vertical mixing and short residence time which diluted the stress when it comes to development of hypoxia. The eastern rack appeared to be more vulnerable to hypoxia because of its deeper geography, plume front side position, and stratification of the liquid line in contrast to the western rack. Its bottom seas practiced reg
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