Transcript Chapter 2

Chapter 5

The Biogeochemical Cycles

Botkin & Keller Environmental Science 5e

How Chemicals Cycle

Biogeochemical Cycle

– The complete path a chemical takes through the four major components – or reservoirs – of Earth’s systems 1. Atmosphere 2. Hydrosphere 3. Lithosphere 4. Biosphere Botkin & Keller Environmental Science 5e

Chemical Reactions

Chemical reaction:

– The process in which new chemicals are formed from elements and compounds through chemical change Botkin & Keller Environmental Science 5e

Fig 5.3

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Fig 5.4

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Biogeochemical Cycles and Life: Limiting Factors

• • •

Macronutrients

– Elements required in large amounts by all life – Include the “big six” elements that form the fundamental building blocks of life: carbon hydrogen oxygen phosphorus nitrogen sulfur

Micronutrients

– Elements required either in • small amounts by all life or • moderate amounts by some forms of life and not all by others

Limiting factor

– When chemical elements are not available at the right times, in the right amounts, and in the right concentrations relative to each other Botkin & Keller Environmental Science 5e

The Geologic Cycle

The Geologic Cycle:

– The processes responsible for formation and change of Earth materials – Best described as a group of cycles: • Tectonic • Hydrologic • Rock • Biochemical Botkin & Keller Environmental Science 5e

Fig 5.6

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Tectonic Cycle

• •

Tectonic cycle:

– Involves creation and destruction of the solid outer layer of Earth, the lithosphere

Plate tectonics:

– The slow movement of these large segments of Earth’s outermost rock shell – Boundaries between plates are geologically active areas Botkin & Keller Environmental Science 5e

Fig 5.7

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Tectonic Cycle: Plate Boundaries

• • •

Divergent plate boundary:

– Occurs at a spreading ocean ridge, where plates are moving away from one another – New lithosphere is produced (seafloor spreading)

Convergent plate boundary

– Occurs when plates collide • Produces linear coastal mountain ranges or continental mountain ranges

Transform fault boundary

– Occurs where one plate slides past another • San Andreas Fault in California Botkin & Keller Environmental Science 5e

The Hydrologic Cycle

The Hydrologic Cycle:

– The transfer of water from the oceans to the atmosphere to the land and back to the oceans. Includes: • Evaporation of water from the oceans • Precipitation on land • Evaporation from land • Runoff from streams, rivers, and sub-surface groundwater Botkin & Keller Environmental Science 5e

Fig 5.8

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

The Rock Cycle

The rock cycle:

– Numerous processes that produce rocks and soils – Depends on other cycles: • tectonic cycle for energy • Hydrologic cycle for water – Rock is classified as • Igneous • Sedimentary • Metamorphic Botkin & Keller Environmental Science 5e

Fig 5.9

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Fig 5.12

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Fig 5.13

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

The Carbon Cycle

• •

Carbon is the element that anchors all organic substances The carbon cycle:

– Carbon combines with and is chemically and biologically linked with the cycles of oxygen and hydrogen that form the major compounds of life Botkin & Keller Environmental Science 5e

Fig 5.14

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Fig 5.15

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

Fig 5.16

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

The Carbon Cycle: Unanswered Issues

The Missing Carbon Sink

– Substantial amounts of carbon dioxide released into the atmosphere but apparently not reabsorbed and thus remaining unaccounted for Botkin & Keller Environmental Science 5e

Fig 5.17

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

The Carbon-Silicate Cycle

The carbon-silicate cycle:

– A complex biogeochemical cycle over time scales as long as one-half billion years.

– Includes major geological processes, such as: • Weathering • Transport by ground and surface waters • Erosion • Deposition of crustal rocks – Believed to provide important negative feedback mechanisms that control the temperature of the atmosphere.

Botkin & Keller Environmental Science 5e

Fig 5.18

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

The Nitrogen Cycle

• • •

The nitrogen cycle:

– Cycle responsible for moving important nitrogen components through the biosphere and other Earth systems – Extremely important because nitrogen is required by all living things

Nitrogen fixation:

– The process of converting inorganic, molecular nitrogen in the atmosphere to ammonia or nitrate

Denitrification:

– The process of releasing fixed nitrogen back to molecular nitrogen Botkin & Keller Environmental Science 5e

Fig 5.19

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers

The Phosphorus Cycle

The phosphorus cycle:

– Involves the movement of phosphorus throughout the biosphere and lithosphere – Important because phosphorus is an essential element for life and often is a limiting nutrient for plant growth.

Botkin & Keller Environmental Science 5e

Fig 5.20

Botkin & Keller Environmental Science 5e © 2005 John Wiley and Sons Publishers