Ocean Chemistry, Carbon & Acidification — Practice · Grade 12 Science
Chapter: Pollution, Carbon & Climate EvidenceWhat this practice covers
By the end of Ocean Chemistry, Carbon & Acidification you should be able to:
- I can explain how dissolved CO₂ changes carbonate chemistry.
- I can calculate logarithmic pH factors and distinguish acidification from becoming acidic.
8 questions, numeric and written answer, each with a worked explanation.
Vocabulary used: acidification, alkalinity, dissolved inorganic carbon.
Problem 1
Hints
Write the relationship first; substitute with consistent units.
Answer and explanation
10 times
10¹=10.
Problem 2
Answer and explanation
Yes; its pH has declined even though it remains basic.
Response criteria
- State a scientifically accurate conclusion.
- Show the calculation or mechanism that supports it.
- Include units, conditions, or limits where relevant.
Problem 3
Hints
List the given quantities, select a relationship, and check units before substituting.
Answer and explanation
1.585 times
10^.20≈1.585.
Problem 4
Answer and explanation
They are distinct processes: acidification changes chemistry; warming changes temperature, though they can interact.
Response criteria
- State a scientifically accurate conclusion.
- Show the calculation or mechanism that supports it.
- Include units, conditions, or limits where relevant.
Problem 5
Hints
Acidification names a shift, not necessarily crossing neutral pH.
Answer and explanation
10^0.3≈2.0, about a doubling.
Problem 6
Hints
State what the supplied observations or conditions establish, and separate that from any assumption.
Answer and explanation
Carbonate-system equilibria shift, often lowering carbonate ion availability and affecting saturation, depending on conditions.
Problem 7
Answer and explanation
The 26% calculation concerns[H⁺]; carbonate requires additional coupled-equilibrium information.
A known pH difference supports a hydrogen-ion ratio under the stated convention. It does not by itself determine carbonate concentration or a shell-dissolution rate. Alkalinity summarizes seawater’s acid-neutralizing charge account and helps constrain carbonate chemistry alongside dissolved inorganic carbon and conditions. Saturation state compares chemical conditions with mineral equilibrium. Keep these distinct quantities rather than converting a 26% hydrogen-ion increase directly into 26% carbonate loss or 26% biological harm.
The 26% calculation concerns[H⁺]; carbonate requires additional coupled-equilibrium information.
Response criteria
- Interpret labels, structures, axes, units and directions correctly.
- Explain the physical or environmental relationship or mechanism.
- Respect stated assumptions and distinguish observation from inference.
Problem 8
Answer and explanation
[H⁺] increases by 10^0.2≈1.585, about 58.5%. It does not prove the same carbonate decrease; alkalinity, dissolved carbon and coupled-equilibrium conditions are also required.
[H⁺] increases by 10^0.2≈1.585, about 58.5%.
It does not prove the same carbonate decrease; alkalinity, dissolved carbon and coupled-equilibrium conditions are also required.
Response criteria
- Use the stated measurements or conditions, with correct units.
- Connect the result to the physical or environmental mechanism or evidence relationship.
- Identify the assumption, model limit or further evidence requested.