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Dead zones in the world’s oceans and large lakes are characterized by:
High biological oxygen demand
Excessive bloom of algae
Excess nutrients like nitrates and phosphates
All of the above
- High biological oxygen demand: Dead zones occur when oxygen levels drop, often due to decomposing organic matter, which increases oxygen demand.
- Excessive bloom of algae: Algal blooms are common before dead zones form. When algae die, they decompose, reducing oxygen.
- Excess nutrients like nitrates and phosphates: Runoff containing these nutrients can fuel excessive algae growth, starting the process that leads to dead zones.
- All of the above: These factors interplay, creating and exacerbating dead zones.
By: Parvesh Mehta ProfileResourcesReport error
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