Ocean Acidification

Jack Wilson
7 min read
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Study Guide Overview
This study guide covers ocean acidification, including: the chemical process behind it (CO2 reacting with seawater), its impact on marine life (calcium carbonate availability, shell formation, fish physiology), the specific case of pteropods, and human impact through fossil fuels and deforestation. It also provides practice questions and exam tips.
#Ocean Acidification: A Deep Dive ๐
Hey there, future AP Environmental Science rockstar! Let's break down ocean acidification, a crucial topic that often pops up on the exam. We'll make sure you're not just memorizing facts, but truly understanding the connections. Let's get started!
#What is Ocean Acidification?
Ocean acidification is the ongoing decrease in the pH of the Earth's oceans, caused by the uptake of carbon dioxide (CO2) from the atmosphere. Think of it like this: the ocean is like a giant sponge, soaking up our excess CO2. But this "soaking" has consequences. ๐งช
#The Chemistry Behind It
When CO2 dissolves in seawater, it reacts with water to form carbonic acid (H2CO3). This carbonic acid then releases hydrogen ions (H+), which increases the acidity (lowers the pH) of the ocean. Here's the reaction:
- Key Point: Increased atmospheric CO2 leads to increased ocean acidity.
#Human Impact
- Quick Fact: The burning of fossil fuels and deforestation are major contributors to increased atmospheric CO2.
Over the past 200 years, the ocean's pH has dropped by 0.1 units. While that might not sound like much, remember that the pH scale is logarithmic, meaning a 0.1 change represents about a 30% increase in acidity! ๐
- Memory Aid: Think of the pH scale like the Richter scale for earthquakes. Each whole number represents a tenfold change. A small change in pH means a BIG change in acidity.
#Impacts of Changing pH
So, what does this increased acidity mean for marine life? Let's dive in!
#Calcium Carbonate Crisis
- High-Value Topic: This is a HUGE area for AP questions, so pay close attention!
Increased acidity reduces the availability of calcium carbonate (CaCO3), a crucial building block for many marine organisms. Here's why it mat...

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