🌡️intro to climate science review

key term - PH

Definition

pH is a scale used to specify the acidity or basicity of an aqueous solution, ranging from 0 to 14. It measures the concentration of hydrogen ions (H+) in a solution, with lower values indicating higher acidity and higher values indicating higher alkalinity. In the context of environmental science, pH plays a crucial role in ocean chemistry, affecting marine life and ecosystem health, particularly as it relates to ocean acidification and its impact on sea life.

5 Must Know Facts For Your Next Test

  1. The pH scale is logarithmic, meaning each whole number change on the scale represents a tenfold change in acidity or basicity.
  2. Normal seawater has a pH of around 8.1; however, increased atmospheric CO2 is causing this value to decline, leading to more acidic ocean conditions.
  3. Ocean acidification can hinder the ability of marine organisms like corals and shellfish to form their calcium carbonate structures, threatening biodiversity.
  4. Monitoring pH levels in oceans is critical for understanding the impacts of climate change on marine ecosystems and fish populations.
  5. A decrease in ocean pH can also disrupt nutrient cycling and food webs in marine environments, further affecting aquatic life.

Review Questions

  • How does the pH scale function in determining the acidity or basicity of solutions, and what implications does this have for ocean ecosystems?
    • The pH scale ranges from 0 to 14, where values below 7 indicate acidity and values above 7 indicate alkalinity. Each unit change represents a tenfold difference in hydrogen ion concentration. In ocean ecosystems, fluctuations in pH can affect the health of marine organisms, especially those like corals that rely on stable conditions for growth and reproduction. Understanding how pH changes impact these ecosystems is vital for predicting how climate change will influence marine biodiversity.
  • Discuss the relationship between rising CO2 levels and ocean acidification, focusing on how this affects oceanic pH levels.
    • Rising CO2 levels from human activities are absorbed by the oceans, leading to chemical reactions that produce carbonic acid and lower seawater pH. This process results in ocean acidification, which poses significant threats to marine life. As pH decreases, organisms that rely on calcium carbonate structures struggle to maintain their shells and skeletons. The ongoing decline in ocean pH illustrates the direct impact of climate change on marine ecosystems.
  • Evaluate the potential long-term effects of decreased ocean pH on marine biodiversity and fisheries management strategies.
    • The long-term effects of decreased ocean pH due to acidification could significantly alter marine biodiversity by threatening species that are sensitive to changes in their environment. As key species like corals and shellfish decline, there could be cascading effects throughout the food web. Fisheries management strategies must adapt by incorporating data on pH levels and their impacts on fish populations and habitats to ensure sustainable practices that consider these environmental changes.