Ocean Acidification (pH) Calculator
This calculator helps scientists and researchers to understand the changes in ocean acidity by calculating the pH levels under various conditions. It is a critical tool for marine biologists and environmental scientists studying the impacts of increased CO2 levels on marine ecosystems.
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Data Source and Methodology
Data and calculations are based on the methodologies published by the International Oceanographic Commission. View Source. All calculations are rigorously based on the formulas and data provided by this source.
The Formula Explained
The calculator uses the following formula to estimate the pH level of ocean water:
\[ pH = \frac{CO_2}{Alkalinity} \times Constant \]
Glossary of Terms
- CO2 Concentration (µatm): The amount of carbon dioxide in the water measured in microatmospheres.
- Alkalinity (µmol/kg): A measure of the water's capacity to neutralize acid.
- pH Level: The acidity or basicity of the water, which affects marine life.
How It Works: A Step-by-Step Example
For a CO2 concentration of 400 µatm and an alkalinity of 2300 µmol/kg, the pH can be calculated using the given formula, resulting in a specific pH level.
Frequently Asked Questions (FAQ)
What is ocean acidification?
Ocean acidification refers to the process by which the ocean becomes more acidic due to increased CO2 levels in the atmosphere.
Why is pH important for marine life?
The pH of ocean water affects the health and survival of marine organisms, particularly those with calcium carbonate shells or skeletons.
How accurate is this calculator?
This calculator provides estimates based on scientific methodologies. For precise measurements, lab analysis is recommended.