Biogeochemical cycles

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22 Terms

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Biogeochemical Cycles

Flow of chemical elements between the atmosphere, biosphere, hydrosphere, and lithosphere.

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Reservoir (in biogeochemical cycles)

A place where an element is stored (e.g., oceans, land, rocks, animals).

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Residence Time

The average time an atom or molecule stays in a reservoir.

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Flux

The rate of transfer of material between reservoirs.

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Photosynthesis

Biochemical reactions by which plants, algae, and cyanobacteria convert light energy into chemical energy, fixing CO₂ into sugars.Equation: 6 CO₂ + 6 H₂O + light → C₆H₁₂O₆ + 6 O₂

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Carbon Cycle

The movement of carbon among the atmosphere, oceans, biosphere, and lithosphere.

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Types of Carbon in the Carbon Cycle

Organic carbon: from respiration

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Anthropogenic carbon:

released from burning fossil fuels and human activities

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Major Reservoirs in the Carbon Cycle

Lithosphere (largest), oceans (deep water), terrestrial biosphere, atmosphere (smallest).

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Human Impact on the Carbon Cycle

Fossil fuel combustion, cement production, deforestation, land

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Nitrogen Cycle

The movement of nitrogen among the atmosphere, biosphere, and soils; conversion between inorganic and organic nitrogen forms.

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Why Nitrogen Is Needed

Essential for amino acids, proteins, plant growth, and nutrients.

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Nitrogen Fixation

Conversion of atmospheric N₂ into bioavailable organic forms. Done by symbiotic + free

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Nitrification

Conversion of ammonia into nitrates by chemoautotrophic bacteria.

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Assimilation

Uptake of nitrogen by plants and animals to build organic molecules.

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Ammonification

Conversion of organic nitrogen back into ammonium by decomposers.

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Denitrification

Conversion of nitrates back into atmospheric N₂ by bacteria.

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Major Reservoirs in the Nitrogen Cycle

Atmosphere (largest for inorganic N₂), terrestrial biosphere (organic + inorganic), others insignificant.

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Human Impact on the Nitrogen Cycle

Synthetic fertilizers, fossil fuel burning → excess reactive nitrogen → pollution, eutrophication, dead zones.

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Environmental Problems from Disturbed Cycles

Climate change, ocean acidification, dead zones, groundwater contamination.

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Long term Consequences of Cycle Disturbance

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Policies to Reduce Human Impact on Cycles

Reduce carbon emissions, manage fertilizers better, improve wastewater treatment, trap/remove nutrients, redesign food systems, use pricing/regulation/incentives, integrated land–water planning.