unit 3 lesson 1-4 study guide Flashcards
explain Earth as an Open System vs Earth as a Closed System
(Energy): Energy flows from the sun to Earth but can leave the atmosphere. (Matter): Matter cycles within Earth’s system, rarely escaping to space.
Law of Conservation:
Energy and matter cannot be created or destroyed, only transformed.
Matter Transfer
Matter transfers within and between ecosystems, cycling through trophic levels (e.g., food webs). It changes form but is not lost.
The Water Cycle
Water evaporates, condenses, precipitates, and flows back into reservoirs, repeating the cycle.
list some Reservoirs
Water is stored in oceans, lakes, glaciers, clouds.
Key Processes: Evaporation, transpiration, condensation, precipitation, and runoff.
Biogeochemical Cycles
Key Elements: Oxygen, hydrogen, carbon, nitrogen, and phosphorus cycle through biotic (living) and abiotic (non-living) systems.
Energy: The sun and Earth’s internal heat power these cycles.
what dose biotic, abiotic
biotic (living)
abiotic (non-living)
Oxygen Cycle
Oxygen is produced by plants during photosynthesis and used by organisms for respiration. The cycle connects closely with the carbon and water cycles.
Cycle Interaction: Water is required for photosynthesis, connecting the oxygen cycle to the water cycle.
Photosynthesis:
is the process where plants, algae, and some bacteria use sunlight to convert carbon dioxide and water into glucose (a form of sugar) for energy, while releasing oxygen as a byproduct. It’s essential for producing food and oxygen for life on Earth.
Respiration:
Organisms take in oxygen and release carbon dioxide.
Carbon Cycle
Carbon moves between the atmosphere, living organisms, oceans, soil, and fossil fuels. Photosynthesis, respiration, decomposition, and combustion are key processes in this cycle.
Carbon Reservoirs:
Stored in living organisms, the atmosphere (as CO2), oceans, soil, fossil fuels, and rocks.
Key Processes of carbon
Photosynthesis: Plants remove CO2 from the atmosphere.
Respiration and Decomposition: Return CO2 to the atmosphere.
Fossilization: Dead organisms can become fossil fuels over millions of years.
Human Impact: Combustion of fossil fuels releases stored carbon back into the atmosphere.
Nitrogen Cycle
Nitrogen is fixed by bacteria into usable forms like ammonia and nitrates, which plants absorb. It is returned to the atmosphere through denitrification. Lightning also contributes to nitrogen fixation.
Nitrogen Gas:
78% of Earth’s atmosphere is nitrogen (N2), but most organisms cannot use it directly. 78% of Earth’s atmosphere is nitrogen (N2), but most organisms cannot use it directly.