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This deck focuses on Ocean Acidification, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study Ocean Acidification in AP Environmental Science with focused flashcards that help you recognize the idea, recall the key rule, and apply it in practice-style prompts.
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What is the chemical formula for a carbonate ion?
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CO32−. Carbonate ions are essential for marine organism calcification.
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This deck focuses on Ocean Acidification, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Work through these flashcards in short sessions. Try to answer each prompt before flipping the card, then revisit any cards you miss until the explanation feels automatic.
Answer: CO32−. Carbonate ions are essential for marine organism calcification.
Answer: CO32−. Carbonate ions are essential for marine organism calcification.
Answer: Major carbon sink, absorbing CO₂. Oceans absorb about 25% of human CO₂ emissions.
Answer: CO2+H2O→H2CO3. CO₂ dissolves in water to form carbonic acid.
Answer: Higher temperature decreases CO₂ solubility. Warmer water holds less dissolved CO₂ than cold water.
Answer: Approximately 8.1 to 8.3. Ocean water is naturally basic, well above neutral pH 7.
Answer: Higher CO₂ leads to lower pH. Inverse relationship: more CO₂ absorption decreases ocean pH.
Answer: HCO3−. Bicarbonate ion is a major component of ocean chemistry.
Answer: Cold water circulation and mixing. Cold water dissolves more CO₂ than warm water.
Answer: Alters sensory perception and behavior. Higher acidity disrupts fish nervous system function.
Answer: Measuring pH and carbonate ion concentrations. These measurements track ocean acidification progress.
Answer: Less than 8.1. Acidified water has lower pH than normal ocean conditions.
Answer: HCO3−. Bicarbonate ion is a major component of ocean chemistry.
Answer: Major carbon sink, absorbing CO₂. Oceans absorb about 25% of human CO₂ emissions.
Answer: Carbon dioxide (CO₂). CO₂ absorption forms acids that lower ocean pH.
Answer: Approximately 8.1 to 8.3. Ocean water is naturally basic, well above neutral pH 7.
Answer: Higher CO₂ leads to lower pH. Inverse relationship: more CO₂ absorption decreases ocean pH.
Answer: Disruption of marine food webs. Loss of calcifying organisms disrupts marine ecosystems.
Answer: Weakens coral skeletons, hindering growth. Lower pH reduces carbonate for coral skeleton formation.
Answer: Ca2++CO32−→CaCO3. Calcium and carbonate combine to form shells and skeletons.
Answer: Coral bleaching. Acidification directly weakens coral structures, causing bleaching.
Answer: Measuring pH and carbonate ion concentrations. These measurements track ocean acidification progress.
Answer: CO2+H2O→H2CO3. CO2 dissolves in water to form carbonic acid.
Answer: Bicarbonate ions (HCO3−). Bicarbonate ions help maintain stable ocean pH levels.
Answer: Weakens coral skeletons, hindering growth. Lower pH reduces carbonate for coral skeleton formation.
Answer: Absorb CO₂ during photosynthesis. Phytoplankton remove CO₂ from water during growth.
Answer: Increased atmospheric CO₂ from human activities. Burning fossil fuels releases CO₂ that dissolves in oceans.
Answer: Reducing CO₂ emissions globally. Reducing the source of excess CO₂ prevents further acidification.
Answer: Damage to coral reefs affects recreational activities. Coral reef degradation reduces diving and snorkeling tourism.
Answer: Potential decline in species diversity. Acidification harms calcifying species, disrupting ecosystems.
Answer: Warmer oceans release more CO₂, lowering pH. Warming reduces CO₂ solubility, creating positive feedback.
Answer: Reducing CO₂ emissions globally. Reducing the source of excess CO₂ prevents further acidification.
Answer: H2CO3. Carbonic acid forms when CO₂ dissolves in seawater.
Answer: Higher temperature decreases CO₂ solubility. Warmer water holds less dissolved CO₂ than cold water.
Answer: Carbon dioxide (CO₂). CO₂ absorption forms acids that lower ocean pH.
Answer: Calcium carbonate (CaCO3). Calcium carbonate dissolves more easily in acidic water.
Answer: Weaker shells and skeletons. Less carbonate means calcifying organisms struggle to build structures.
Answer: Coral reefs, mollusks, and some plankton. These organisms build calcium carbonate shells and skeletons.
Answer: Less than 8.1. Acidified water has lower pH than normal ocean conditions.
Answer: Increased atmospheric CO₂ from human activities. Burning fossil fuels releases CO₂ that dissolves in oceans.
Answer: Lowers pH, making water more acidic. More hydrogen ions decrease pH on the logarithmic scale.
Answer: Threat to fisheries and aquaculture industries. Declining marine ecosystems reduce seafood availability and income.
Answer: Decrease in pH of ocean water due to absorption of CO₂. Ocean water becomes less basic as it absorbs atmospheric CO₂.
Answer: Ca2++CO32−→CaCO3. Calcium and carbonate combine to form shells and skeletons.
Answer: Decreasing pH levels in ocean waters. pH decline is the primary measure of ocean acidification.
Answer: Cold water circulation and mixing. Cold water dissolves more CO₂ than warm water.
Answer: Impacts on food security and livelihoods. Declining fisheries affect coastal communities economically.
Answer: Fossil fuel burning and deforestation. These activities release the most atmospheric CO₂.
Answer: Bicarbonate ions (HCO3−). Bicarbonate ions help maintain stable ocean pH levels.
Answer: Coral reefs, mollusks, and some plankton. These organisms build calcium carbonate shells and skeletons.
Answer: Decreases ocean pH levels. More hydrogen ions make ocean water more acidic.
Answer: Disruption of marine food webs. Loss of calcifying organisms disrupts marine ecosystems.
Answer: Fossil fuel burning and deforestation. These activities release the most atmospheric CO₂.
Answer: Threat to fisheries and aquaculture industries. Declining marine ecosystems reduce seafood availability and income.
Answer: H+. Hydrogen ions determine acidity levels in solutions.
Answer: Impacts on food security and livelihoods. Declining fisheries affect coastal communities economically.
Answer: Lowers pH, making water more acidic. More hydrogen ions decrease pH on the logarithmic scale.
Answer: Alters sensory perception and behavior. Higher acidity disrupts fish nervous system function.
Answer: Damage to coral reefs affects recreational activities. Coral reef degradation reduces diving and snorkeling tourism.
Answer: Decreasing pH levels in ocean waters. pH decline is the primary measure of ocean acidification.
Answer: Coral bleaching. Acidification directly weakens coral structures, causing bleaching.
Answer: It reduces availability of carbonate ions for shell formation. Lower pH decreases carbonate availability for shell-building organisms.