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Biogeochemical Cycles. Energy Flows Matter Cycles. Matter Cycles. A cycle is a group of processes in which matter repeatedly moves through a series of reservoirs. A reservoir is a place where matter or energy is stored. (atmosphere, hydrosphere, geosphere, biosphere)
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Biogeochemical Cycles Energy Flows Matter Cycles
Matter Cycles • A cycle is a group of processes in which matter repeatedly moves through a series of reservoirs. • A reservoir is a place where matter or energy is stored. (atmosphere, hydrosphere, geosphere, biosphere) • Many elements on Earth move between reservoirs. These cycles rely on energy sources to drive them. • The length of time that energy or matter spends in a reservoir can vary from a few hours to several million years.
Biogeochemical Cycle Click below to watch the Visual Concept.
The Water (Hydrologic) Cycle If there is magic on this planet it is water -Loren Eisley “All the rivers run into the sea, yet the sea is not full…” - Ecclesiastes 1:7
The Water Cycle • The movement of water from the atmosphere to Earth’s surface and back to the atmosphere is called the water cycle. • In the water cycle, water changes from liquid water to water vapor through the energy transfers involved in evaporation and transpiration. During these processes, water absorbs energy and changes state. • When the water loses energy, it condenses to form water droplets, such as those that form clouds. Eventually, water falls back to Earth’s surface as precipitation.
Important Concepts • Oceans – more evaporation than precipitation • Land – more precipitation than evaporation (Runoff). Land is watered by the system.
Water Quantity • The Earth’s water supply • Oceans 97 % • Atmosphere .0010 % • Cryosphere (Ice caps/Glaciers) 2.23 % • Salt Lakes .007 % • Freshwater Lakes .009 % • Rivers/Streams .0001 % • Groundwater & Soil .609 %
Water Quantity cont’d • 99.4% of Earth’s water is in the Oceans or Cryosphere (icecaps and glaciers) Of the remaining .6% only about .3 % is available to humans with current technology. • Freshwater lakes .009 % • Rivers & Streams .0001 % • Shallow Groundwater .303 % • Total .3121 % • This totals approximately 21 billion gallons per person, which may sound like enough. However, the problem is that freshwater is not evenly distributed geographically. • Humans now, as a GEOLOGIC force are able to affect (usually short-circuit) the hydrologic cycle. • It is estimated that 60 % of all water withdrawn worldwide is “consumed” (or diverted from its normal water cycle pathway).
Human interactions with the Water Cycle • Excessive evaporation losses from irrigated land. • Water diverted from one river or watershed to another. • Groundwater pumped faster than it can be recharged into natural aquifers. • Contamination of groundwater, lakes or rivers. (silt, sewage, fertilizers, pesticides, radioactive waste, toxic waste, heavy metals, pathogens, heat.) • Excessive evaporation from reservoirs.
Water Cycle (summary) • Because freshwater on the planet is a renewable resource (as long as the Sun shines) we will never run out. • However Human activity may modify the distribution and storage capacity in certain regions.
The Water Cycle • http://earthguide.ucsd.edu/earthguide/diagrams/watercycle/
Check up • What source of energy drives the water cycle? Explain. • Describe how water moves through the water cycle. • From what sources does water evaporate? • List 3 ways that humans interact with the water cycle.
The Carbon Cycle • Carbon moves through all four spheres through the carbon cycle. • In the short-term carbon cycle, plants convert carbon dioxide, CO2, from the atmosphere into carbohydrates(photosynthesis). • When organisms’ bodies break down the carbohydrates and release some of the carbon back into the air as CO2 or through their organic wastes as CO2 (respiration),or methane CH4 (decomposition). • In the long-term carbon cycle, carbon is stored in the geosphere in a type of rock called a carbonate.
Check up • What source of energy ultimately drives the carbon cycle? Explain • In what form is carbon found in the atmosphere? Where does it come from? • Cellulose, which makes up the walls of plant cells contains carbon. What is the source of this carbon? • How does carbon become part of the body of an animal? • How is carbon released from the body of an animal? • Briefly explain two ways that humans are interacting or impacting the natural carbon cycle.
Nitrogen Cycle • 78% of Earth’s Atmosphere is Nitrogen • Used to build proteins • Most organisms cannot use atmospheric form, it must be changed or “fixed” • N2 NO3-or NH4+
The Nitrogen Cycle • In the nitrogen cycle, nitrogen moves from the air to soil, from soil to plants and animals, and back to air again. • Nitrogen is removed from air mainly by the action of nitrogen-fixing bacteria in the soil. • The nitrogen then is taken up (absorbed) by plants. • Plants are then are eaten by animals. Animals use the Nitrogen for building proteins and amino acids.
Nitrogen Cycle • The nitrogen is returned to the soil by decay and by animal wastes. • Chemical processes that occur in the soil then release the nitrogen back into the air. • Nitrogen in the atmosphere can also be fixed by the occurrence of lightning.
Check up • What source of energy ultimately drives the nitrogen cycle? Explain • How do animals obtain nitrogen? • In what form is nitrogen found in the atmosphere? • What form of nitrogen are most plants able to absorb? How does it get into that form? • List and explain two processes that return nitrogen to the atmosphere.
Human interaction • All natural cycles can be altered by human activities. • The carbon cycle is affected when humans use fossil fuels. • Deforestation removes the Earth’s ability to naturally “metabolize” CO2. • The nitrogen and phosphorus cycles are affected by agriculture.
What is meant by the phrase: Humans have become a Geologic Force
Credits • Fred Montague, Environment Notebook, pp 108-112, Mountain Bear Ink, 2003 • Holt Earth Science 2010 edition